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	<title>ISTerre - Institut des Sciences de la Terre</title>
	<link>https://www.isterre.fr/</link>
	<description>Site web de l'Institut des Sciences de la Terre (ISTerre), unit&#233; mixte de recherche du CNRS, de l'Universit&#233; Grenoble Alpes, de l'Universit&#233; Savoie Mont Blanc, de l'IRD et de l'IFSTTAR</description>
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		<title>ISTerre - Institut des Sciences de la Terre</title>
		<url>https://www.isterre.fr/sites/www.isterre.fr/local/cache-vignettes/L60xH59/siteon0-1e5f7.png?1789475664</url>
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<item xml:lang="fr">
		<title>Presentation of some PhD topics proposed in ISTerre</title>
		<link>https://www.isterre.fr/english/research/phds-at-isterre-laboratory/sujets-de-these/article/presentation-of-some-phd-topics-proposed-in-isterre.html</link>
		<guid isPermaLink="true">https://www.isterre.fr/english/research/phds-at-isterre-laboratory/sujets-de-these/article/presentation-of-some-phd-topics-proposed-in-isterre.html</guid>
		<dc:date>2024-03-26T09:24:24Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>fr</dc:language>
		<dc:creator>Mai-Linh DOAN</dc:creator>



		<description>&lt;p&gt;A series of flash presentations of open PhD proposal at ISTerre&lt;/p&gt;

-
&lt;a href="https://www.isterre.fr/english/research/phds-at-isterre-laboratory/sujets-de-these/" rel="directory"&gt;PhD Thesis proposals&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;p&gt;On April 3rd, a series of PhD topics will be presented at ISTerre at Kilian Amphitheater at ISTerre Grenoble (&lt;a href=&#034;https://www.openstreetmap.org/way/495692657&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;location&lt;/a&gt;)&lt;/p&gt;
&lt;p&gt;Presentation are also accessible on Zoom : &lt;br class='autobr' /&gt;
&lt;a href=&#034;https://univ-grenoble-alpes-fr.zoom.us/j/95751333912?pwd=bC9qWWd5dDdVT3piOUV2ODN4Mjd1UT09&#034; class=&#034;spip_url spip_out auto&#034; rel=&#034;nofollow external&#034;&gt;https://univ-grenoble-alpes-fr.zoom.us/j/95751333912?pwd=bC9qWWd5dDdVT3piOUV2ODN4Mjd1UT09&lt;/a&gt;&lt;br class='autobr' /&gt; Meeting ID : 957 5133 3912. Passcode : 918743&lt;/p&gt;
&lt;h3 class=&#034;spip&#034;&gt;&lt;i&gt;Open PhD proposals at ISTerre&lt;/h3&gt;&lt;table&gt; &lt;tr&gt; &lt;th width=&#034;10%&#034;&gt; Time (CET) &lt;/th&gt;&lt;th&gt; Title &lt;/th&gt;&lt;th width=&#034;15%&#034;&gt; Presenter &lt;/th&gt;&lt;th width=&#034;15%&#034;&gt; Comment &lt;/th&gt; &lt;/tr&gt; &lt;tr&gt; &lt;td&gt;17:00&lt;/td&gt;&lt;td&gt;ISTerre laboratory in a nutshell&lt;/td&gt;&lt;td&gt;Mai-Linh Doan&lt;/td&gt;&lt;td&gt;&lt;/td&gt; &lt;/tr&gt; &lt;tr&gt; &lt;td&gt;17:05&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;https://adum.fr/as/ed/voirproposition.pl?langue=&amp;site=edtue&amp;matricule_prop=53614&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Large scale slope deformations in Upper Mustang, Nepal &#8211; controls and impacts&lt;/a&gt;
&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;#&#034; title=&#034;kristen.cook..&#229;t..univ-grenoble-alpes.fr&#034; onclick=&#034;location.href=lancerlien('kristen.cook,6aaa3781a5226,univ-grenoble-alpes.fr',',6aaa3781a5226,'); return false;&#034; class=&#034;spip_mail&#034;&gt;Kristen Cook&lt;/a&gt;&lt;/td&gt;&lt;td&gt;Lab priority for Doctoral grant competition&lt;/td&gt; &lt;/tr&gt; &lt;tr&gt; &lt;td&gt;17:10&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;https://adum.fr/as/ed/voirproposition.pl?langue=&amp;site=edstep&amp;matricule_prop=53669&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Paleoseismicity of large active strike-slip faults in the Western Alps : Implications for geodynamics and seismic hazard&lt;/a&gt;
&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;#&#034; title=&#034;rvass..&#229;t..univ-smb.fr&#034; onclick=&#034;location.href=lancerlien('rvass,6aaa3781a525b,univ-smb.fr',',6aaa3781a525b,'); return false;&#034; class=&#034;spip_mail&#034;&gt;Riccardo Vassallo&lt;/a&gt;&lt;/td&gt;&lt;td&gt;Lab priority for Doctoral grant competition&lt;/td&gt; &lt;/tr&gt; &lt;tr&gt; &lt;td&gt;17:15&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;https://adum.fr/as/ed/voirproposition.pl?langue=&amp;site=edstep&amp;matricule_prop=53697&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Monitoring rock slope mechanical properties with environmental seismology&lt;/a&gt;
&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;#&#034; title=&#034;eric.larose..&#229;t..univ-grenoble-alpes.fr&#034; onclick=&#034;location.href=lancerlien('eric.larose,6aaa3781a5270,univ-grenoble-alpes.fr',',6aaa3781a5270,'); return false;&#034; class=&#034;spip_mail&#034;&gt;&#201;ric Larose&lt;/a&gt;&lt;/td&gt;&lt;td&gt;Lab priority for Doctoral grant competition&lt;/td&gt; &lt;/tr&gt; &lt;tr&gt; &lt;td&gt;17:20&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;https://adum.fr/as/ed/voirproposition.pl?langue=&amp;site=edtue&amp;matricule_prop=55531&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Faster alteration of rocks in active faults ? Insight from experiments and numerical simulations, with application to geothermal energy&lt;/a&gt;&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;#&#034; title=&#034;mai-linh.doan..&#229;t..univ-grenoble-alpes.fr&#034; onclick=&#034;location.href=lancerlien('mai-linh.doan,6aaa3781a5281,univ-grenoble-alpes.fr',',6aaa3781a5281,'); return false;&#034; class=&#034;spip_mail&#034;&gt;Mai-Linh Doan&lt;/a&gt;&lt;/td&gt;&lt;td&gt;Funded&lt;/td&gt; &lt;/tr&gt; &lt;td&gt;17:25&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;https://emploi.cnrs.fr/Offres/Doctorant/UMR5275-FABCAR-088/Default.aspx-&gt;https://emploi.cnrs.fr/Offres/Doctorant/UMR5275-FABCAR-089/Default.aspx&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Physicochemical fingerprints and quantification of microbially-mediated mineral weathering&lt;/a&gt;&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;#&#034; title=&#034;damien.daval..&#229;t..univ-grenoble-alpes.fr&#034; onclick=&#034;location.href=lancerlien('damien.daval,6aaa3781a5292,univ-grenoble-alpes.fr',',6aaa3781a5292,'); return false;&#034; class=&#034;spip_mail&#034;&gt;Damien Daval&lt;/a&gt;&lt;/td&gt;&lt;td&gt;Funded&lt;/td&gt; &lt;/tr&gt; &lt;td&gt;17:30&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;https://emploi.cnrs.fr/Offres/Doctorant/UMR5275-FABCAR-089/Default.aspx&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Modeling the morphological evolution of mineral surface upon (bio)alteration : Implications for the concept of biosignatures&lt;/a&gt;&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;#&#034; title=&#034;damien.daval..&#229;t..univ-grenoble-alpes.fr&#034; onclick=&#034;location.href=lancerlien('damien.daval,6aaa3781a52a1,univ-grenoble-alpes.fr',',6aaa3781a52a1,'); return false;&#034; class=&#034;spip_mail&#034;&gt;Damien Daval&lt;/a&gt;&lt;/td&gt;&lt;td&gt;Funded&lt;/td&gt; &lt;/tr&gt;
&lt;tr&gt;
&lt;td&gt;17:35&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;https://adum.fr/as/ed/voirproposition.pl?site=adumR&amp;matricule_prop=55990&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Exploring and simulating earthquakes interactions&lt;/a&gt;&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;#&#034; title=&#034;david.marsan..&#229;t..univ-smb.fr&#034; onclick=&#034;location.href=lancerlien('david.marsan,6aaa3781a52b1,univ-smb.fr',',6aaa3781a52b1,'); return false;&#034; class=&#034;spip_mail&#034;&gt;David Marsan&lt;/a&gt;&lt;/td&gt;&lt;td&gt;Funded&lt;/td&gt; &lt;/tr&gt;
&lt;tr&gt;
&lt;td&gt;17:40&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;https://adum.fr/as/ed/voirproposition.pl?site=adumR&amp;matricule_prop=53595&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;The role of the past subductions on the location of the intracontinental transform faults&lt;/a&gt;&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;#&#034; title=&#034;julia.de-sigoyer..&#229;t..univ-grenoble-alpes.fr&#034; onclick=&#034;location.href=lancerlien('julia.de-sigoyer,6aaa3781a52c1,univ-grenoble-alpes.fr',',6aaa3781a52c1,'); return false;&#034; class=&#034;spip_mail&#034;&gt;Julia de Sigoyer&lt;/a&gt;&lt;/td&gt;&lt;td&gt;Doctoral grant competition&lt;/td&gt; &lt;/tr&gt;&lt;tr&gt;
&lt;td&gt;17:45&lt;/td&gt;&lt;td&gt;
&lt;a href=&#034;https://adum.fr/as/ed/voirproposition.pl?langue=&amp;site=edtue&amp;matricule_prop=53319&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Contribution of dense seismological networks to the characterization of fluid seepage monitoring (water, gas) in the critical zone&lt;/a&gt;&lt;/td&gt;&lt;td&gt;&lt;a href=&#034;#&#034; title=&#034;philippe.roux..&#229;t..univ-grenoble-alpes.fr&#034; onclick=&#034;location.href=lancerlien('philippe.roux,6aaa3781a52d1,univ-grenoble-alpes.fr',',6aaa3781a52d1,'); return false;&#034; class=&#034;spip_mail&#034;&gt;Philippe Roux&lt;/a&gt;&lt;/td&gt;&lt;td&gt;Lab priority for Doctoral grant competition&lt;/td&gt; &lt;/tr&gt;
&lt;/table&gt;&lt;/div&gt;
		
		</content:encoded>


		

	</item>
<item xml:lang="fr">
		<title>ANR AlterAction</title>
		<link>https://www.isterre.fr/french/recherche/projets-de-recherche/projets-anr/projets-en-cours/article/anr-alteraction.html</link>
		<guid isPermaLink="true">https://www.isterre.fr/french/recherche/projets-de-recherche/projets-anr/projets-en-cours/article/anr-alteraction.html</guid>
		<dc:date>2023-07-19T08:13:22Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>fr</dc:language>
		<dc:creator>Mai-Linh DOAN</dc:creator>



		<description>&lt;div class=&#034;encartgris&#034;&gt;
&lt;strong&gt;Dur&#233;e : &lt;/strong&gt; 2024-2028
&lt;/br&gt;
&lt;strong&gt;Contact &#224; ISTerre :&lt;/strong&gt; &lt;a href=&#034;https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/&#034;&gt;Mai-Linh Doan&lt;/a&gt;&lt;/div&gt;

-
&lt;a href="https://www.isterre.fr/french/recherche/projets-de-recherche/projets-anr/projets-en-cours/" rel="directory"&gt;Projets en cours&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;div class=&#034;encartgris&#034;&gt;
&lt;strong&gt;Dur&#233;e : &lt;/strong&gt; 2024-2028
&lt;/br&gt;
&lt;strong&gt;Contact &#224; ISTerre :&lt;/strong&gt; &lt;a href=&#034;https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/&#034;&gt;Mai-Linh Doan&lt;/a&gt;&lt;/div&gt;
&lt;p&gt;This ANR project will focus on the process of maturation of active faults in the upper crust by chemical alteration of their fault walls, and on the feedback between alteration and tectonic activity.&lt;/p&gt;
&lt;p&gt;The main research hypothesis is that the fault activity induces new fractures that enhance fluid-rock interactions and associated fault zone alteration. This feedback forcing would accelerate the maturation of active faults, by creating clay gouges that weakens the fault and decreases its core permeability over time.&lt;/p&gt;
&lt;p&gt;Our focus is on granitoid rocks, which is the lithology of both the Rhine Valley geothermal reservoirs and that of the wall rocks of the Nojima fault responsible for the 1995 Nanbu-Kobe earthquake in Japan. Dynamic loading pulverizes granitoid rocks, which enhances their permeability. That facilitates laboratory alteration of centimetric samples, as shown by preliminary experiments.&lt;/p&gt;
&lt;p&gt;We will use core samples from the GSJ-Hirabayashi scientific borehole intersecting the Nojima fault to (1) obtain a continuous alteration profile through the fault by combining core and downhole geophysical data and (2) perform laboratory alteration experiments at various differential stresses to assess the intertwined effects of tectonic loading and fault alteration.&lt;/p&gt;
&lt;div class=&#034;col-un-un-un&#034;&gt;&lt;div&gt;
&lt;/div&gt;&lt;div&gt;&lt;div class=&#034;encartbleu&#034;&gt;&lt;center&gt;&lt;a href=&#034;https://anr-alteraction.osug.fr/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;&lt;strong&gt;Site web du projet&lt;/strong&gt;&lt;/a&gt;&lt;/center&gt;&lt;/div&gt;&lt;/div&gt;&lt;div&gt;
&lt;/div&gt;&lt;/div&gt;&lt;/div&gt;
		
		</content:encoded>


		

	</item>
<item xml:lang="en">
		<title>ANR AlterAction</title>
		<link>https://www.isterre.fr/english/research/research-projects/national-research-agency-anr-projects/ongoing-projects/article/anr-alteraction.html</link>
		<guid isPermaLink="true">https://www.isterre.fr/english/research/research-projects/national-research-agency-anr-projects/ongoing-projects/article/anr-alteraction.html</guid>
		<dc:date>2023-07-19T08:13:22Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>en</dc:language>
		<dc:creator>Mai-Linh DOAN</dc:creator>



		<description>&lt;div class=&#034;encartgris&#034;&gt;
&lt;strong&gt;Duration : &lt;/strong&gt; 2024-2028
&lt;/br&gt;
&lt;strong&gt;ISTerre contact :&lt;/strong&gt; &lt;a href=&#034;https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/&#034;&gt;Mai-Linh Doan&lt;/a&gt;&lt;/div&gt;

-
&lt;a href="https://www.isterre.fr/english/research/research-projects/national-research-agency-anr-projects/ongoing-projects/" rel="directory"&gt;Ongoing projects&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;div class=&#034;encartgris&#034;&gt;&lt;strong&gt;Duration : 2024-2028
&lt;/br&gt;
ISTerre contact : &lt;a href=&#034;https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/&#034;&gt;Mai-Linh Doan&lt;/a&gt;&lt;/strong&gt;&lt;/div&gt;
&lt;p&gt;This &lt;a href=&#034;https://anr-alteraction.osug.fr/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;ANR project&lt;/a&gt; will focus on the process of maturation of active faults in the upper crust by chemical alteration of their fault walls, and on the feedback between alteration and tectonic activity.&lt;/p&gt;
&lt;p&gt;The main research hypothesis is that the fault activity induces new fractures that enhance fluid-rock interactions and associated fault zone alteration. This feedback forcing would accelerate the maturation of active faults, by creating clay gouges that weakens the fault and decreases its core permeability over time.&lt;/p&gt;
&lt;p&gt;Our focus is on granitoid rocks, which is the lithology of both the Rhine Valley geothermal reservoirs and that of the wall rocks of the Nojima fault responsible for the 1995 Nanbu-Kobe earthquake in Japan. Dynamic loading pulverizes granitoid rocks, which enhances their permeability. That facilitates laboratory alteration of centimetric samples, as shown by preliminary experiments.&lt;/p&gt;
&lt;p&gt;We will use core samples from the GSJ-Hirabayashi scientific borehole intersecting the Nojima fault to (1) obtain a continuous alteration profile through the fault by combining core and downhole geophysical data and (2) perform laboratory alteration experiments at various differential stresses to assess the intertwined effects of tectonic loading and fault alteration.&lt;/p&gt;&lt;/div&gt;
		&lt;div class="hyperlien"&gt;View online : &lt;a href="https://anr-alteraction.osug.fr/" class="spip_out"&gt;https://anr-alteraction.osug.fr/&lt;/a&gt;&lt;/div&gt;
		
		</content:encoded>


		

	</item>
<item xml:lang="fr">
		<title>Accueil</title>
		<link>https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/accueil.html</link>
		<guid isPermaLink="true">https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/accueil.html</guid>
		<dc:date>2011-10-06T09:48:08Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>fr</dc:language>
		<dc:creator>Mai-Linh DOAN</dc:creator>



		<description>&lt;p&gt;Page d'accueil&lt;/p&gt;

-
&lt;a href="https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/" rel="directory"&gt;Mai-Linh DOAN&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;table class=&#034;table spip&#034;&gt;
&lt;tbody&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td rowspan='4'&gt;&lt;div class='spip_document_2257 spip_document spip_documents spip_document_image spip_documents_center spip_document_center'&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;img src='https://www.isterre.fr/sites/www.isterre.fr/local/cache-vignettes/L3xH5/me_tcdp-2-a5b49-c4cd2.jpg?1789540225' width='3' height='5' alt='' /&gt;
&lt;/figure&gt;
&lt;/div&gt;&lt;/td&gt;
&lt;td&gt;Adresse postale&lt;/td&gt;
&lt;td&gt;Adresse physique&lt;/td&gt;
&lt;td&gt;T&#233;l&#233;phone&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;CS 40700&lt;/td&gt;
&lt;td&gt;1381, rue de la Piscine&lt;/td&gt;
&lt;td&gt;Tel : (+33) 4 76 63 52 09&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td&gt;38058 Grenoble CEDEX 9&lt;/td&gt;
&lt;td&gt;38400 Saint-Martin d'H&#232;res&lt;/td&gt;
&lt;td&gt;Fax : (+33) 4 76 63 52 52&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;FRANCE&lt;/td&gt;
&lt;td&gt;FRANCE&lt;/td&gt;
&lt;td&gt;Mail&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;&lt;h4 class=&#034;spip&#034;&gt; CV&lt;/h4&gt;&lt;table class=&#034;table spip&#034;&gt;
&lt;tbody&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td&gt;1997&lt;/td&gt;
&lt;td&gt;El&#232;ve fonctionnaire stagiare &#224; l'&lt;a href=&#034;http://www.ens.fr/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;&#201;cole normale sup&#233;rieure of Paris&lt;/a&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;2000&lt;/td&gt;
&lt;td&gt;DEA de physique des liquides (Paris VI)&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td&gt;2001&lt;/td&gt;
&lt;td&gt;Agr&#233;gation de Physique&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;2005&lt;/td&gt;
&lt;td&gt;Th&#232;se de g&#233;ophysique sous la direction de &lt;a href=&#034;http://eost.u-strasbg.fr/IPGS/perso.php?nom=CORNET&amp;iprenom=F&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Fran&#231;ois Cornet&lt;/a&gt; au Laboratoire de m&#233;canique des roches de l'&lt;a href=&#034;http://www.ipgp.fr/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Institut de Physique du Globe de Paris&lt;/a&gt;&lt;br class='autobr' /&gt;
&#034;&lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/these.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Etude in situ des interactions hydrom&#233;caniques entre fluides et failles actives - Application au Laboratoire du Rift de Corinthe&lt;/a&gt;&#034;&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td&gt;2005-2007&lt;/td&gt;
&lt;td&gt;S&#233;jour postdoctoral avec&lt;a href=&#034;http://www.es.ucsc.edu/personnel/Brodsky/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Emily Brodsky&lt;/a&gt; &#224; &lt;a href=&#034;http://www.ess.ucla.edu/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;UCLA&lt;/a&gt; puis &lt;a href=&#034;http://www.pmc.ucsc.edu/~seisweb/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;UCSC&lt;/a&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;2007-...&lt;/td&gt;
&lt;td&gt;Ma&#238;tre de conf&#233;rences &#224; l'&lt;a href=&#034;http://www.ujf-grenoble.fr/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Universit&#233; Grenoble I&lt;/a&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;&lt;h4 class=&#034;spip&#034;&gt; Recherche&lt;/h4&gt;&lt;h5 class=&#034;spip&#034;&gt; Etude in-situ des propri&#233;t&#233;s m&#233;caniques et hydrologiques des failles
&lt;/h5&gt;
&lt;p&gt;Les s&#233;ismes s'initient sur des failles actives, le plus souvent &#224; plusieurs kilom&#232;tres de profondeur. Pendant longtemps, il a fallu se contenter de donn&#233;es sismiques enregistr&#233;es &#224; plusieurs kilom&#232;tres de la source sismique, ou d'affleurement de failles inactives depuis plusieurs milliers d'ann&#233;es. Les forages profonds apportent des donn&#233;es assez uniques pour comprendre la m&#233;canique des s&#233;ismes.&lt;/p&gt;
&lt;p&gt;Je m'int&#233;resse &#224; la m&#233;canique des failles, en mesurant sur le terrain leurs propri&#233;t&#233;s hydrauliques, thermiques et les contraintes qui les environnent. J'ai notamment particip&#233; &#224; de nombreux projets d'instrumentation de failles actives : (1) la faille d'Aigion dans le Golfe de Corinthe (2) la faille de Chelungpu (3) le projet NantroSEIZE de forage dans la zone de subduction de Nankai au large du Japon.&lt;/p&gt;
&lt;h5 class=&#034;spip&#034;&gt;Etude en laboratoire de la m&#233;canique &#224; haute vitesse de d&#233;formation&lt;/h5&gt;
&lt;p&gt;Lors d'un s&#233;isme, les parois d'une faille glisse l'une contre l'autre avec une vitesse de plusieurs m&#232;tres par seconde. La d&#233;formation autour d'une faille se fait donc &#224; des taux de d&#233;formation tr&#232;s &#233;lev&#233;s. J'effectue deux types d'exp&#233;riences en laboratoire :&lt;/p&gt;
&lt;ul class=&#034;spip&#034; role=&#034;list&#034;&gt;&lt;li&gt; des exp&#233;riences de friction &#224; haute vitesse sur le talc et sur des m&#233;langes de serpentine et de talc. Le but est de comprendre si les faibles concentration de talc observ&#233;es le long de la faille de San Andreas permettent le glissement continu (et donc sans d&#233;gat) de la faille de San Andreas.&lt;/li&gt;&lt;li&gt; des exp&#233;riences d'endommagement &#224; haut taux de d&#233;formation. Ces exp&#233;riences offrent des pistes pour comprendre les roches pulv&#233;ris&#233;es observ&#233;es le long de la faille de San Andreas.&lt;/li&gt;&lt;/ul&gt;&lt;h5 class=&#034;spip&#034;&gt; Publications
&lt;/h5&gt;
&lt;p&gt;Voir la &lt;a href='https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/publications.html' class=&#034;spip_in&#034;&gt;liste des publications&lt;/a&gt;&lt;/p&gt;&lt;/div&gt;
		
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	</item>
<item xml:lang="fr">
		<title>Accueil</title>
		<link>https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/accueil-6246.html</link>
		<guid isPermaLink="true">https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/accueil-6246.html</guid>
		<dc:date>2011-10-06T09:48:08Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>fr</dc:language>
		<dc:creator>Mai-Linh DOAN</dc:creator>



		<description>&lt;p&gt;Page d'accueil&lt;/p&gt;

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&lt;a href="https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/" rel="directory"&gt;Mai-Linh DOAN&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;table class=&#034;table spip&#034;&gt;
&lt;tbody&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td rowspan='4'&gt;&lt;div class='spip_document_2257 spip_document spip_documents spip_document_image spip_documents_center spip_document_center'&gt;
&lt;figure class=&#034;spip_doc_inner&#034;&gt; &lt;img src='https://www.isterre.fr/sites/www.isterre.fr/local/cache-vignettes/L3xH5/me_tcdp-2-a5b49-c4cd2.jpg?1789540225' width='3' height='5' alt='' /&gt;
&lt;/figure&gt;
&lt;/div&gt;&lt;/td&gt;
&lt;td&gt;Adresse postale&lt;/td&gt;
&lt;td&gt;Adresse physique&lt;/td&gt;
&lt;td&gt;T&#233;l&#233;phone&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;CS 40700&lt;/td&gt;
&lt;td&gt;1381, rue de la Piscine&lt;/td&gt;
&lt;td&gt;Tel : (+33) 4 76 63 52 09&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td&gt;38058 Grenoble CEDEX 9&lt;/td&gt;
&lt;td&gt;38400 Saint-Martin d'H&#232;res&lt;/td&gt;
&lt;td&gt;Fax : (+33) 4 76 63 52 52&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;FRANCE&lt;/td&gt;
&lt;td&gt;FRANCE&lt;/td&gt;
&lt;td&gt;Mail&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;&lt;h4 class=&#034;spip&#034;&gt; CV&lt;/h4&gt;&lt;table class=&#034;table spip&#034;&gt;
&lt;tbody&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td&gt;1997&lt;/td&gt;
&lt;td&gt;El&#232;ve fonctionnaire stagiare &#224; l'&lt;a href=&#034;http://www.ens.fr/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;&#201;cole normale sup&#233;rieure of Paris&lt;/a&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;2000&lt;/td&gt;
&lt;td&gt;DEA de physique des liquides (Paris VI)&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td&gt;2001&lt;/td&gt;
&lt;td&gt;Agr&#233;gation de Physique&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;2005&lt;/td&gt;
&lt;td&gt;Th&#232;se de g&#233;ophysique sous la direction de &lt;a href=&#034;http://eost.u-strasbg.fr/IPGS/perso.php?nom=CORNET&amp;iprenom=F&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Fran&#231;ois Cornet&lt;/a&gt; au Laboratoire de m&#233;canique des roches de l'&lt;a href=&#034;http://www.ipgp.fr/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Institut de Physique du Globe de Paris&lt;/a&gt;&lt;br class='autobr' /&gt;
&#034;&lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/these.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Etude in situ des interactions hydrom&#233;caniques entre fluides et failles actives - Application au Laboratoire du Rift de Corinthe&lt;/a&gt;&#034;&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_odd odd'&gt;
&lt;td&gt;2005-2007&lt;/td&gt;
&lt;td&gt;S&#233;jour postdoctoral avec&lt;a href=&#034;http://www.es.ucsc.edu/personnel/Brodsky/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Emily Brodsky&lt;/a&gt; &#224; &lt;a href=&#034;http://www.ess.ucla.edu/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;UCLA&lt;/a&gt; puis &lt;a href=&#034;http://www.pmc.ucsc.edu/~seisweb/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;UCSC&lt;/a&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr class='row_even even'&gt;
&lt;td&gt;2007-...&lt;/td&gt;
&lt;td&gt;Ma&#238;tre de conf&#233;rences &#224; l'&lt;a href=&#034;http://www.ujf-grenoble.fr/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Universit&#233; Grenoble I&lt;/a&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/tbody&gt;
&lt;/table&gt;&lt;h4 class=&#034;spip&#034;&gt; Recherche&lt;/h4&gt;&lt;h5 class=&#034;spip&#034;&gt; Etude in-situ des propri&#233;t&#233;s m&#233;caniques et hydrologiques des failles
&lt;/h5&gt;
&lt;p&gt;Les s&#233;ismes s'initient sur des failles actives, le plus souvent &#224; plusieurs kilom&#232;tres de profondeur. Pendant longtemps, il a fallu se contenter de donn&#233;es sismiques enregistr&#233;es &#224; plusieurs kilom&#232;tres de la source sismique, ou d'affleurement de failles inactives depuis plusieurs milliers d'ann&#233;es. Les forages profonds apportent des donn&#233;es assez uniques pour comprendre la m&#233;canique des s&#233;ismes.&lt;/p&gt;
&lt;p&gt;Je m'int&#233;resse &#224; la m&#233;canique des failles, en mesurant sur le terrain leurs propri&#233;t&#233;s hydrauliques, thermiques et les contraintes qui les environnent. J'ai notamment particip&#233; &#224; de nombreux projets d'instrumentation de failles actives : (1) la faille d'Aigion dans le Golfe de Corinthe (2) la faille de Chelungpu (3) le projet NantroSEIZE de forage dans la zone de subduction de Nankai au large du Japon.&lt;/p&gt;
&lt;h5 class=&#034;spip&#034;&gt;Etude en laboratoire de la m&#233;canique &#224; haute vitesse de d&#233;formation&lt;/h5&gt;
&lt;p&gt;Lors d'un s&#233;isme, les parois d'une faille glisse l'une contre l'autre avec une vitesse de plusieurs m&#232;tres par seconde. La d&#233;formation autour d'une faille se fait donc &#224; des taux de d&#233;formation tr&#232;s &#233;lev&#233;s. J'effectue deux types d'exp&#233;riences en laboratoire :&lt;/p&gt;
&lt;ul class=&#034;spip&#034; role=&#034;list&#034;&gt;&lt;li&gt; des exp&#233;riences de friction &#224; haute vitesse sur le talc et sur des m&#233;langes de serpentine et de talc. Le but est de comprendre si les faibles concentration de talc observ&#233;es le long de la faille de San Andreas permettent le glissement continu (et donc sans d&#233;gat) de la faille de San Andreas.&lt;/li&gt;&lt;li&gt; des exp&#233;riences d'endommagement &#224; haut taux de d&#233;formation. Ces exp&#233;riences offrent des pistes pour comprendre les roches pulv&#233;ris&#233;es observ&#233;es le long de la faille de San Andreas.&lt;/li&gt;&lt;/ul&gt;&lt;h5 class=&#034;spip&#034;&gt; Publications
&lt;/h5&gt;
&lt;p&gt;Voir la &lt;a href='https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/publications.html' class=&#034;spip_in&#034;&gt;liste des publications&lt;/a&gt;&lt;/p&gt;&lt;/div&gt;
		
		</content:encoded>


		
		

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<item xml:lang="fr">
		<title>Publications</title>
		<link>https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/publications.html</link>
		<guid isPermaLink="true">https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/publications.html</guid>
		<dc:date>2011-10-04T13:02:27Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>fr</dc:language>
		<dc:creator>Mai-Linh DOAN</dc:creator>



		<description>
&lt;p&gt;Publications &#224; comit&#233; de lecture J. Pwavodi and Doan, M.L., Direct assessment of the hydraulic structure of the plate boundary at the toe of the Nankai accretionary prism. Geophys. J. Int. 236(2), 1125&#8211;1138, doi : 10.1093/gji/ggad473, 2024. Doan, M.L., J. Dutilleul, and P. Henry, Effective porosity profile at IODP Site C0002 in the heart of the Nankai accretionary prism, and Its use for predicting in situ seismic velocities, Geophys. Res. Lett., 50, e2022GL100209, doi : 10.1029/2022GL100209, (&#8230;)&lt;/p&gt;


-
&lt;a href="https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/" rel="directory"&gt;Mai-Linh DOAN&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;h3 class=&#034;spip&#034;&gt;Publications &#224; comit&#233; de lecture&lt;/h3&gt;&lt;ol class=&#034;spip&#034; role=&#034;list&#034;&gt;&lt;li&gt; J. Pwavodi and &lt;strong&gt;Doan, M.L.&lt;/strong&gt;, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/pwavodi_doan_2024_direct_assessment_of_the_hydraulic_structure_of_the_plate_boundary_at_the_toe.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Direct assessment of the hydraulic structure of the plate boundary at the toe of the Nankai accretionary prism&lt;/a&gt;. Geophys. J. Int. 236(2), 1125&#8211;1138, doi : 10.1093/gji/ggad473, 2024.&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt;, J. Dutilleul, and P. Henry, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/doan23_grl_vp-porosity_nankai.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Effective porosity profile at IODP Site C0002 in the heart of the Nankai accretionary prism, and Its use for predicting in situ seismic velocities&lt;/a&gt;, Geophys. Res. Lett., 50, e2022GL100209, doi : 10.1029/2022GL100209, 2023.&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt;, M.J. Heap, M. Schell and U. Kueppers, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/doan22_jvgr_shpb_andesite.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;High strain rate damage in porous andesite&lt;/a&gt;, J. Volcanol. Geotherm. Res., 427, 107551, doi : 10.1016/j.jvolgeores.2022.107551, 2022&lt;/li&gt;&lt;li&gt; De Gelder, G., &lt;strong&gt;M-L, Doan&lt;/strong&gt;, C. Beck, J. Carlut,, C. Seibert, N. Feuillet, G. Carter, S. Pechlivanidou and R. Gawthorpe, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/degelder22_sedimentology_seismiite_golfecorinthe.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Micro-scale sedimentary signature of paleoearthquakes and paleotsunamis in the Corinth Rift (Greece), Multi-scale and multi-parametric analysis of Late Quaternary event deposits within the active Corinth Rift (Greece)&lt;/a&gt; : Sedimentology, doi:10.1111/sed.12964, 2022&lt;/li&gt;&lt;li&gt; M&#252;ller, B., &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, T. H. Goebel, Y. Liu, P. Mart&#237;nez-Garz&#243;n, T. Mitchell, and I. Zaliapin, &lt;a href=&#034;https://eos.org/editors-vox/understanding-and-anticipating-induced-seismicity&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Understanding and anticipating induced seismicity&lt;/a&gt;, Eos, 102, doi : 10.1029/2021EO161325, 2021.&lt;/li&gt;&lt;li&gt; Aben. F.M, &lt;strong&gt;M.-L. Doan&lt;/strong&gt; and Mitchell, T., &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/aben20_jgr_offfaultdamagelab.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Variation of hydraulic properties due to dynamic fracture damage : Implications for fault zones.&lt;/a&gt; J. Geophys. Res. v125, p. 1&#8211;22, doi:10.1029/2019jb018919., 2020&lt;/li&gt;&lt;li&gt; McNeill L., and the &lt;strong&gt;IODP Expedition 381 Science Team&lt;/strong&gt; &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/mcneill19_scientific_reports_exp381_corinth__article.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;High-resolution record reveals climate-driven environmental and sedimentary changes in an active rift&lt;/a&gt; Scientific Reports, 9(1). doi:10.1038/s41598-019-40022-w, 2019&lt;/li&gt;&lt;li&gt; Weaver, K., &lt;strong&gt;Doan, M.L.&lt;/strong&gt;, Cox, S. C., Townend, J., Holden, C., &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/weaver19_wrr_christchurch_aquifer_changes_tides.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Tidal behavior and water-level changes in gravel aquifers in response to multiple earthquakes : A case study from New Zealand&lt;/a&gt;. Water Resour. Res. 55, &lt;a href=&#034;https://doi.org/10.1029/2018WR022784&#034; class=&#034;spip_url spip_out auto&#034; rel=&#034;nofollow external&#034;&gt;https://doi.org/10.1029/2018WR022784&lt;/a&gt;, 2019&lt;/li&gt;&lt;li&gt; Janku-Capova, L., R. Sutherland, J. Townend, M. L. Doan, C. Massiot, J. Coussens, and B. C&#233;l&#233;rier, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/weaver19_wrr_christchurch_aquifer_changes_tides.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Fluid Flux in Fractured Rock of the Alpine Fault Hanging-Wall Determined from Temperature Logs in the DFDP-2B Borehole, New Zealand&lt;/a&gt;, Geochemistry, Geophys. Geosystems, 19(8), 2631&#8211;2646, doi:10.1029/2017GC007317, 2018&lt;/li&gt;&lt;li&gt; Massiot, C., C&#233;l&#233;rier, B., &lt;strong&gt;Doan, M.L.&lt;/strong&gt;, Little, T.A., Townend, J., McNamara, D.D., Williams, J., Schmitt, D.R., Toy, V.G., Sutherland, R., Janku-Capova, L., Upton, P., Pezard, P.A., &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/massiotdoan18_g3_dfdp2_bhtv.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;The Alpine Fault Hangingwall Viewed From Within : Structural Analysis of Ultrasonic Image Logs in the DFDP-2B Borehole&lt;/a&gt;, New Zealand, Geochemistry, Geophys. Geosystems, 19(8), 2492&#8211;2515, doi:10.1029/2017GC007368, 2018.&lt;/li&gt;&lt;li&gt; Wang, C.-Y., &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, L. Xue, and A. J. Barbour, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/wang18_wrr_tides_oklahoma.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Tidal Response of Groundwater in a Leaky Aquifer - Application to Oklahoma&lt;/a&gt;, Water Resour. Res., 54, doi:10.1029/2018WR022793, 2018&lt;/li&gt;&lt;li&gt; Townend, J., Sutherland, R., Toy, V.G., &lt;strong&gt;M.-L. Doan&lt;/strong&gt; and the DFDP-2B Science Team. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/townend17_g3_dfdp2_geophysics.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Petrophysical, Geochemical, and Hydrological Evidence for Extensive Fracture-Mediated Fluid and Heat Transport in the Alpine Fault's Hanging-Wall Damage Zone&lt;/a&gt;. Geophys. Geosystems Geochem, doi : 10.1002/2017GC007202, 2017&lt;/li&gt;&lt;li&gt; Toy, V.G., Sutherland, R., Townend, J. and the &lt;strong&gt;DFDP-2B Science Team&lt;/strong&gt;. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/toy17_nzjournal_geology_dfdp2.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Bedrock Geology of DFDP-2B, Central Alpine Fault, New Zealand&lt;/a&gt;. New Zealand Journal of Geology and Geophysics, 60(4), 497&#8211;518, doi:10.1080/00288306.2017.1375533, 2017.&lt;/li&gt;&lt;li&gt; Aben. F.M, M.-L. Doan, J-P Gratier, F. Renard. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/aben17_grl_healing_percolation.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Experimental postseismic recovery of fracture rocks assisted by calcite sealing&lt;/a&gt;. Geophys. Res. Lett. 44, doi :10.1002/2017GL073965. 2017&lt;/li&gt;&lt;li&gt; Sutherland, R., Townend, J., Toy, V.G., Upton, P., Coussens, J. and the &lt;strong&gt;DFDP-2B Science Team&lt;/strong&gt;. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/sutherland17_nature_dfdp_thermal.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Extreme hydrothermal conditions at an active plate-bounding fault&lt;/a&gt;, Nature, 546(7656):137-140. doi:10.1038/nature22355. 2017&lt;/li&gt;&lt;li&gt; Aben. F.M, &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, J-P Gratier, F. Renard. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/aben17_epsl_pulverisation_sandstone.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;High strain rate deformation of porous sandstone and the asymmetry of earthquake damage in shallow fault zones&lt;/a&gt;. Earth and Planet. Sci. Lett. 463, 81-91, doi :10.1016/j.epsl.2017.01.016 2017&lt;/li&gt;&lt;li&gt; Fondriest, M., &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, F. Aben, F. Fusseis, T. M. Mitchell, M. Voorn, M. Secco, and G. Di Toro, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/fondriest17_epsl_dolostone_pulverization.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Static versus dynamic fracturing in shallow carbonate fault zones&lt;/a&gt;, Earth Planet. Sci. Lett., 461, 8&#8211;19, doi:10.1016/j.epsl.2016.12.024. 2017&lt;/li&gt;&lt;li&gt; Shalev, E., I. Kurzon, &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, and V. Lyakhovsky, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/fondriest17_epsl_dolostone_pulverization.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Sustained water-level changes caused by damage and compaction induced by teleseismic earthquakes&lt;/a&gt;, J. Geophys. Res. Solid Earth, 1&#8211;12, doi:10.1002/2016JB013304. 2016&lt;/li&gt;&lt;li&gt; Aben. F.M, &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, J-P Gratier, F. 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<item xml:lang="fr">
		<title>Publications</title>
		<link>https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/publications-6247.html</link>
		<guid isPermaLink="true">https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/article/publications-6247.html</guid>
		<dc:date>2011-10-04T13:02:27Z</dc:date>
		<dc:format>text/html</dc:format>
		<dc:language>fr</dc:language>
		<dc:creator>Mai-Linh DOAN</dc:creator>



		<description>
&lt;p&gt;Publications &#224; comit&#233; de lecture Aben. F.M, M.-L. Doan and Mitchell, T., Variation of hydraulic properties due to dynamic fracture damage : Implications for fault zones. . J. Geophys. Res. v125, p. 1&#8211;22, doi:10.1029/2019jb018919., 2020 McNeill L., and the IODP Expedition 381 Science Team High-resolution record reveals climate-driven environmental and sedimentary changes in an active rift&#034;. Scientific Reports, 9(1). doi:10.1038/s41598-019-40022-w, 2019 Weaver, K., Doan, M.L., Cox, S. C., (&#8230;)&lt;/p&gt;


-
&lt;a href="https://www.isterre.fr/annuaire/pages-web-du-personnel/mai-linh-doan/" rel="directory"&gt;Mai-Linh DOAN&lt;/a&gt;


		</description>


 <content:encoded>&lt;div class='rss_texte'&gt;&lt;h3 class=&#034;spip&#034;&gt;Publications &#224; comit&#233; de lecture&lt;/h3&gt;&lt;ol class=&#034;spip&#034; role=&#034;list&#034;&gt;&lt;li&gt; Aben. F.M, M.-L. Doan and Mitchell, T., Variation of hydraulic properties due to dynamic fracture damage : Implications for fault zones. . J. Geophys. Res. v125, p. 1&#8211;22, doi:10.1029/2019jb018919., 2020&lt;/li&gt;&lt;li&gt; McNeill L., and the IODP Expedition 381 Science Team High-resolution record reveals climate-driven environmental and sedimentary changes in an active rift&#034;. Scientific Reports, 9(1). doi:10.1038/s41598-019-40022-w, 2019&lt;/li&gt;&lt;li&gt; Weaver, K., Doan, M.L., Cox, S. C., Townend, J., Holden, C., Tidal behavior and water-level changes in gravel aquifers in response to multiple earthquakes : A case study from New Zealand. Water Resour. Res. 55, &lt;a href=&#034;https://doi.org/10.1029/2018WR022784&#034; class=&#034;spip_url spip_out auto&#034; rel=&#034;nofollow external&#034;&gt;https://doi.org/10.1029/2018WR022784&lt;/a&gt;, 2019&lt;/li&gt;&lt;li&gt; Janku-Capova, L., R. Sutherland, J. Townend, M. L. Doan, C. Massiot, J. Coussens, and B. C&#233;l&#233;rier, Fluid Flux in Fractured Rock of the Alpine Fault Hanging-Wall Determined from Temperature Logs in the DFDP-2B Borehole, New Zealand, Geochemistry, Geophys. Geosystems, 19(8), 2631&#8211;2646, doi:10.1029/2017GC007317, 2018&lt;/li&gt;&lt;li&gt; Massiot, C., C&#233;l&#233;rier, B., Doan, M.L., Little, T.A., Townend, J., McNamara, D.D., Williams, J., Schmitt, D.R., Toy, V.G., Sutherland, R., Janku-Capova, L., Upton, P., Pezard, P.A., The Alpine Fault Hangingwall Viewed From Within : Structural Analysis of Ultrasonic Image Logs in the DFDP-2B Borehole, New Zealand, Geochemistry, Geophys. Geosystems, 19(8), 2492&#8211;2515, doi:10.1029/2017GC007368, 2018.&lt;/li&gt;&lt;li&gt; Wang, C.-Y., M.-L. Doan, L. Xue, and A. J. Barbour, Tidal Response of Groundwater in a Leaky Aquifer - Application to Oklahoma, Water Resour. Res., 54, doi:10.1029/2018WR022793, 2018&lt;/li&gt;&lt;li&gt; Townend, J., Sutherland, R., Toy, V.G., M.-L. Doan and the DFDP-2B Science Team. Petrophysical, Geochemical, and Hydrological Evidence for Extensive Fracture-Mediated Fluid and Heat Transport in the Alpine Fault's Hanging-Wall Damage Zone. Geophys. Geosystems Geochem, doi : 10.1002/2017GC007202, 2017&lt;/li&gt;&lt;li&gt; Toy, V.G., Sutherland, R., Townend, J. and the DFDP-2B Science Team. Bedrock Geology of DFDP-2B, Central Alpine Fault, New Zealand. New Zealand Journal of Geology and Geophysics, 60(4), 497&#8211;518, doi:10.1080/00288306.2017.1375533, 2017.&lt;/li&gt;&lt;li&gt; Aben. F.M, M.-L. Doan, J-P Gratier, F. Renard. Experimental postseismic recovery of fracture rocks assisted by calcite sealing. Geophys. Res. Lett. 44, doi :10.1002/2017GL073965. 2017&lt;/li&gt;&lt;li&gt; Sutherland, R., Townend, J., Toy, V.G., Upton, P., Coussens, J. and the DFDP-2B Science Team. Extreme hydrothermal conditions at an active plate-bounding fault, Nature, 546(7656):137-140. doi:10.1038/nature22355. 2017&lt;/li&gt;&lt;li&gt; Aben. F.M, M.-L. Doan, J-P Gratier, F. Renard. High strain rate deformation of porous sandstone and the asymmetry of earthquake damage in shallow fault zones. Earth and Planet. Sci. Lett. 463, 81-91, doi :10.1016/j.epsl.2017.01.016 2017&lt;/li&gt;&lt;li&gt; Fondriest, M., M.-L. Doan, F. Aben, F. Fusseis, T. M. Mitchell, M. Voorn, M. Secco, and G. Di Toro, Static versus dynamic fracturing in shallow carbonate fault zones, Earth Planet. Sci. Lett., 461, 8&#8211;19, doi:10.1016/j.epsl.2016.12.024. 2017&lt;/li&gt;&lt;li&gt; Shalev, E., I. Kurzon, M.-L. Doan, and V. Lyakhovsky, Sustained water-level changes caused by damage and compaction induced by teleseismic earthquakes, J. Geophys. Res. Solid Earth, 1&#8211;12, doi:10.1002/2016JB013304. 2016&lt;/li&gt;&lt;li&gt; Aben. F.M, M.-L. Doan, J-P Gratier, F. Renard. Coseismic damage generation and pulverization in fault zones : insights from high strain rate experiments. AGU Monograph contribution, 2016&lt;/li&gt;&lt;li&gt; Shalev, E., I. Kurzon, M.-L. Doan, and V. Lyakhovsky Water-level oscillations caused by volumetric and deviatoric dynamic strains, Geophys. J. Int., 204(2), 841&#8211;851, doi:10.1093/gji/ggv483. 2016&lt;/li&gt;&lt;li&gt; Aben, F. M., M. L. Doan, T. M. Mitchell, R. Toussaint, T. Reuschl&#233;, M. Fondriest, J.-P. Gratier, and F. Renard Dynamic fracturing by successive coseismic loadings leads to pulverization in active fault zones, J. Geophys. Res. Solid Earth Res., 121, doi:10.1002/ 2015JB012542. 2016&lt;/li&gt;&lt;li&gt; Wiersberg,T., A.M. Schleicher, K. Horiguchi, &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, N. Eguchi, J. Erzinger. Origin and in situ concentrations of hydrocarbons in the Kumano forearc basin from drilling mud gas monitoring during IODP NanTroSEIZE Exp. 319, Applied Geochemistry, 61, 206-216, 2015&lt;/li&gt;&lt;li&gt; Richard, J., &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, J.-P. Gratier and F. Renard Microstructures induced by dynamic loading and fracture healing in porous limestone : experimental approaches, Pure and Applied Geophysics, 172, 1269-1290, doi : 10.1007/s00024-014-0958-9, 2015&lt;/li&gt;&lt;li&gt; Richard, J., J.-P. Gratier, &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, A.-M. Boullier, and F. Renard. Rock and mineral transformations in a fault zone leading to permanent creep : Interactions between brittle and viscous mechanisms in the San Andreas Fault, J. Geophys. Res. Solid Earth, 119, 8132&#8211;8153, doi:10.1002/ 2014JB011489. 2014.&lt;/li&gt;&lt;li&gt; Gratier, J-P., F. Thouvenot, L., Jenatton, A. Tourette, &lt;strong&gt;M.L. Doan&lt;/strong&gt; and F. Renard. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/gratier13_tectonophysics_clery.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Geological control of the partitioning between seismic and aseismic sliding behaviour in active faults : evidence from the Western Alpes, France&lt;/a&gt;, &lt;i&gt;Tectonophysics&lt;/i&gt; ,600:226-242, doi:10.1016/j.tecto.2013.02.013, 2013&lt;/li&gt;&lt;li&gt; Ito, T., Funato , A., W. Lin , &lt;strong&gt;M.L. Doan&lt;/strong&gt; , D. Boutt , Y. Kano , H. Ito , D. Saffer , L. McNeill , T. Byrne and K. Moe . &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Ito13_JGR_Stress_Kumano_Basin.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Determination of Stress State in Deep Subsea Formation by Combination of Hydraulic Fracturing In-situ Test and Core Analysis - A Case Study in the IODP Expedition 319&lt;/a&gt;, &lt;i&gt;J. Geophys. Res.&lt;/i&gt;, 118, 1&#8211;13, doi:10.1002/jgrb.50086, 2013&lt;/li&gt;&lt;li&gt; Saffer, D., P. Flemings, D. Boutt, &lt;strong&gt;M.L. Doan&lt;/strong&gt; , T. Ito , L. McNeill , T. Byrne , M. Conin , W. Lin , Y. Kano , E. Araki , N. Eguchi and S. Toczko. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/saffer13_g3_kumanopressure.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;In Situ Stress and Pore Pressure in the Kumano Forearc Basin, offshore SW Honshu from Down-hole Measurements During Riser Drilling&lt;/a&gt;, &lt;i&gt;Geochem. Geophys. Geosys.&lt;/i&gt;, 14(5),&lt;br class='autobr' /&gt; doi:10.1002/ggge.20051, 2013&lt;/li&gt;&lt;li&gt; Boutareaud, S. T. Hirose, M. Andr&#233;ani, M. Pec, K. Kunze D.-G. Calugaru, A.-M. Boullier and &lt;strong&gt;M.-L. Doan&lt;/strong&gt;. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Boutareaud12_JGR_Talc_HVR_Friction.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;On the role of phyllosilicates on fault lubrication : Insight from micro- and nanostructural investigations on talc friction experiments&lt;/a&gt;, &lt;i&gt;J. Geophys. Res&lt;/i&gt;, 117 (B8), B08408, doi : 10.1029/2011JB009006, 2012&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt; and V. d'Hour, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Doan12_JSG_Pulverisation_InitialDamage.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Effect of initial damage on rock pulverization along faults&lt;/a&gt;, &lt;i&gt;J. Struct. Geol.&lt;/i&gt;, 45,113-124, 2012&lt;/li&gt;&lt;li&gt; Spencer, J.Q.G., J. Hadizadeh, J.-P. Gratier and &lt;strong&gt;M-L Doan&lt;/strong&gt;, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Spencer12_QG_OSL_SAFOD.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Dating deep ? Luminescence studies of fault gouge from the San Andreas Fault Zone 2.6 km beneath Earth's surface&lt;/a&gt;, &lt;i&gt;Quat. Geochronol.&lt;/i&gt;, 10, 280-284, 2012&lt;/li&gt;&lt;li&gt; Boutt, D., D. Saffer, &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, W. Lin, T. Ito, Y. Kano, P. Flemings, L. McNeil, T. Byrne, K. Moe. Scale Dependence of &lt;i&gt;In-situ&lt;/i&gt; &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Boutt12_GRL_MDT.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Permeability Measurements in the Nankai Accretionary Prism : The Role of Fractures&lt;/a&gt;, &lt;i&gt;Geol. Res. Lett.&lt;/i&gt;, 39, L07302, doi:10.1029/2012GL051216, 2012&lt;/li&gt;&lt;li&gt; 7.	Moe, K.T., T. Ito, W. Lin, &lt;strong&gt;M.-L. Doan&lt;/strong&gt;, D. Boutt, Y. Kawamura, C.K. Khong, L. McNeill, T. Byrne, D. Saffer, E. Araki, N. Eguchi, I. Sawada, P. Flemings, Y. Kano, C. Moore, M. Kinoshita, H. Tobin. Operational Review of the First Wireline in Situ Stress Test in Scientific Ocean Drilling, Scientific Drilling, 13:35-39, 2012&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt;, and A. Billi, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Doan11_GRL_SHPB_Marble.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;High strain rate damage of Carrara marble&lt;/a&gt;, &lt;i&gt;Geophys. Res. Lett.&lt;/i&gt;, 38, L19302, doi:10.1029/2011GL049169, 2011&lt;/li&gt;&lt;li&gt; Gratier, J-P., J. Richard, F. Renard, S. Mittempergher, &lt;strong&gt;M.L. Doan&lt;/strong&gt;, G. Di Toro, J. Hadizadeh and A-M. Boullier. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Gratier11_Geology_PressureSolution_SAFOD.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Aseismic sliding of active faults by pressure solution creep : Evidence from the San Andreas Fault Observatory at Depth (SAFOD)&lt;/a&gt;. &lt;i&gt;Geology&lt;/i&gt;, 39, 1131-1134, 2011&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt;, M. Conin, P. Henry, and IODP expedition 319 scientists, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Doan11_G3_NantroSEIZE_PorosityProfileFromSonic.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Free gas in Kumano basin detected from borehole sonic data in IODP NanTroSEIZE drilling Site&lt;/a&gt;. &lt;i&gt;Geophys. Geosystems Geochem.&lt;/i&gt; 12, Q0AD06, doi:10.1029/2010GC003284, 2011.&lt;/li&gt;&lt;li&gt; Lin, W., &lt;strong&gt;M.L. Doan&lt;/strong&gt;, J.C. Moore and IODP expedition 319 scientists, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/LinDoanetal_GRL_2010.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Present day stress horizontal stress orientations in the Kumano forearc basin of the Southwest Japan subduction zone determined from IODP NantroSEIZE drilling Site C0009&lt;/a&gt;. &lt;i&gt;Geophys. Res. Lett.&lt;/i&gt; 37, L13303, doi:10.1029/2010GL042158, 2010.&lt;/li&gt;&lt;li&gt; Noiriel, C., F. Renard, &lt;strong&gt;M.L. Doan&lt;/strong&gt; and J.P. Gratier, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Noiriel11_ChemGeol_CrystallisationForce.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Intense fracturing and fracture sealing induced by mineral growth in porous rocks&lt;/a&gt;. &lt;i&gt;Chem. Geol.&lt;/i&gt; 269(3-4) : 197-209, 2010&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L&lt;/strong&gt;. and G. Gary, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/DoanGary_NatureGeo_2009.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Rock pulverisation at high strain rate near the San Andreas Fault&lt;/a&gt;, &lt;i&gt;Nature Geoscience.&lt;/i&gt; 2:709-712, 2009. (&lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/DoanGary_NatureGeo_2009_supp.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Suppl&#233;ments&lt;/a&gt;, vid&#233;o en fran&#231;ais)&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt; and F.H. Cornet. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Doan07_EPSL_PressureDrop.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Small pressure drop triggered near a fault by small teleseismic waves&lt;/a&gt;, &lt;i&gt;Earth Planet. Sci. Lett.&lt;/i&gt;, 258 (1-2) : 207-218, 2007&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt; and F.H. Cornet. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Doan07_GRL_Convection_CorinthRift.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Thermal Anomaly near the Aigio Fault, Gulf of Corinth, Greece, maybe due to convection below the fault&lt;/a&gt;. &lt;i&gt;Geophys. Res. Lett.&lt;/i&gt;, 34 (6) doi:10.1016/j.epsl.2007.03.036, 2007&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt;, E.E. Brodsky, Y. Kano, and K.-F. Ma, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/DBKM_GRL_2006.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;In-situ measurement of the hydraulic diffusivity of the active Chelungpu Fault&lt;/a&gt;, Taiwan. &lt;i&gt;Geophys. Res. Lett.&lt;/i&gt;, 33 (16) doi :10.1029/2006GL026889, 2006.&lt;/li&gt;&lt;li&gt; Cornet, F.H., &lt;strong&gt;M.L. Doan&lt;/strong&gt;, I. Moretti and G. Borm. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/CornetDoanGeosciences2004.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Drilling through the active Aigion fault : the AIG10 well observatory&lt;/a&gt;. &lt;i&gt;C.R. G&#233;oscience&lt;/i&gt;, 336 (4-5) : 395-406, 2004.&lt;/li&gt;&lt;li&gt; Cornet, F.H., &lt;strong&gt;M.L. Doan&lt;/strong&gt;, and F. Fontbonne. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/CDF_IJRM_2003.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Electrical imaging and hydraulic testing for a complete stress determination&lt;/a&gt;. &lt;i&gt;Int. J. Rock Mech. Min. Sci.&lt;/i&gt;, 40 :1225-1241, 2003.&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt; and F.H. Cornet.&lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/DoanNarms2003.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;A coupled hydraulic and electrical stress determination technique&lt;/a&gt;. In Hammah R. et al, editor, Mining and Tunneling Innovation and Opportunity, vol. 2, 1413-1417. NARMS-TAC, University of Toronto Press, 2002.&lt;/li&gt;&lt;/ol&gt;&lt;h3 class=&#034;spip&#034;&gt;Autres Publications&lt;/h3&gt;&lt;ol class=&#034;spip&#034; role=&#034;list&#034;&gt;&lt;li&gt; Th&#232;se : Th&#232;se de g&#233;ophysique sous la direction de &lt;a href=&#034;http://eost.unistra.fr/recherche/ipgs/ge/ge-perso/francois-cornet/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Fran&#231;ois Cornet&lt;/a&gt; au Laboratoire de m&#233;canique des roches de l'&lt;a href=&#034;http://www.ipgp.fr/&#034; class=&#034;spip_out&#034; rel=&#034;external&#034;&gt;Institut de Physique du Globe de Paris&lt;/a&gt; &#034;&lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/these.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Etude in situ des interactions hydrom&#233;caniques entre fluides et failles actives - Application au Laboratoire du Rift de Corinthe&lt;/a&gt;&#034;. 2005.&lt;/li&gt;&lt;li&gt; &lt;strong&gt;Doan, M.L.&lt;/strong&gt;, E.E. Brodsky, R. Prioul and C. Signer, &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/tidal_tutorial_SDR.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Tidal analysis of borehole pressure - A tutorial&lt;/a&gt;. Schlumberger Research report. 2006.&lt;/li&gt;&lt;li&gt; Moe Kyaw Thu, Takatoshi Ito, Weiren Lin, &lt;strong&gt;Mai-Linh Doan&lt;/strong&gt;, , and IODP expedition 319 scientists. &lt;a href='https://www.isterre.fr/sites/www.isterre.fr/IMG/pdf/Moe12_ScientificDrilling_MDT.pdf' class=&#034;spip_in&#034; type='application/pdf'&gt;Operational Review of the First Wireline in Situ Stress Test in Scientific Ocean Drilling&lt;/a&gt;. Scientific Drilling, 13 : 35-39, 2012.&lt;/li&gt;&lt;/ol&gt;&lt;/div&gt;
		
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