ISTerre - Institut des Sciences de la Terre

Publications

Marie-Pierre DOIN — 2013-07-16T09:51:05Z

1995

A. Bonneville and R. P. Von Herzen and F. Lucazeau and A. Provost and B. Ollivier and A. Desautez and M. P. Doin and A. Eliason and L. Faynot and M. Godard and P. Gouze and J. Guilbert and J. Kirklin and S. Klarika and L. Lin and B. Malengreau and D. Rousset and C. Wolfteich, Une lithosphere amincie sous le point chaud de la Reunion ? Contraintes apportees
par de nouvelles mesures de flux de chaleur sur la ride des Mascareignes,
Bull. Soc. Geol. France, 32, 909-915, 1995

1996

M. P. Doin and L. Fleitout and D. P. McKenzie, Geoid anomalies and the structure of continental and oceanic lithospheres, J. Geophys. Res., 101, 16119-16135, 1996

M. P. Doin and L. Fleitout, Thermal evolution of the oceanic lithosphere : an alternative view, Earth Planet. Sci. Lett., 142, 121-136, 1996

1997

P. E. van Keken and S. D. King and H. Schmeling and U. R. Christensen and D. Neumeister and M.-P. Doin A comparison of methods for the modeling of thermochemical convection J. Geophys. Res., 102, 22477-22495, 1997

M.-P. Doin and L. Fleitout and U. Christensen, Mantle convection and stability of depleted and undepleted continental lithosphere, J. Geophys. Res., 102, 2771-2787, 1997

1999

C. Dumoulin and M.-P. Doin and L. Fleitout, Heat transport in stagnant lid convection with temperature- and pressure-dependent Newtonian or non-Newtonian rheology, J. Geophys. Res., 104, 12759-12778, 1999

2000

M. P. Doin and L. Fleitout, Flattening of the oceanic topography and geoid : Thermal versus dynamic origin, Geophys. J. Int., 143, 582-594, 2000

C. Prijac and M.P. Doin and J.-M. Gaulier and F. Guillocheau, Subsidence of the Paris Basin and its bearing on the late Variscan lithosphere evolution : a
comparison between Plate and Chablis models, Tectonophysics, 323,1-38, 2000

2001

C. Dumoulin and M.-P. Doin and L. Fleitout, Numerical simulations of the cooling of an oceanic lithosphere above a convective mantle, Phys. Earth Planet. Int., 125, 45-64, 2001

C. Dumoulin and M.-P. Doin and L. Fleitout, On the interpretation of the relationship between seafloor subsidence rate and the height of the ridge,
Geophys. J. Int., 146, 691-698, 2001

M.P. Doin and P. Henry, Subduction initiation and continental crust recycling :
the roles of rheology and eclogitization, Tectonophysics, 342, 163-191, 2001

2002

Morency C, Doin MP, Dumoulin C., Convective destabilization of a thickened continental lithosphere, Earth Planet. Sci. Letter, Earth Planet. Sci. Lett., 202, 303-320, 2002

2003

Robin C., P. Allemand, E. Burov, M.-P. Doin, F. Guillocheau, G. Dromart & J.-P. Garcia, Thermo-mechanical characteristics of the Paris Basin (Triassic-Pleistocene) : from 3D stratigraphic database to numerical models, Special Issue for the Geological Society of London, in " New Insights into Structural Interpretation and Modeling ", Geol. Soc. Sp. Pub. of London, 212, p. 225-250, 2003

2004

Morency C, Doin MP, Numerical simulation of the mantle lithosphere delamination, J. Geophys. Res., 109 (B3) : Art. No. B03410 MAR 20 2004

Le Solleuz A., Doin M.-P., Robin C., and F. Guillocheau, From mountain belt collapse to sedimentary basin development : 2-D thermal model based on inversion of stratigraphic data in the Paris Basin, Tectonophysics, v386, p1-27, 2004

2005

Dumoulin C, Doin MP, Arcay D, et al., Onset of small-scale instabilities at the base of the lithosphere : scaling laws and role of pre-existing lithospheric structures, GEOPHYSICAL JOURNAL INTERNATIONAL 160 (1) : 344-356 JAN 2005

Arcay D., Tric E., and Doin M.-P., Numerical simulations of subduction zones : effect of slab dehydration on the mantle wedge dynamics, Phys. Earth Planet. Int., 149 (1-2) : 133-153 MAR 15 2005

Morency C./ Doin M.-P., Dumoulin C., 3-D numerical simulations of mantle flow beneath mid-ocean ridges, J. Geophys. Res., VOL. 110, B11407, doi:10.1029/2004JB003454, 2005

2006

Thoraval, C., A. Tommasi, and M. Doin (2006), Plume-lithosphere interaction beneath a fast moving plate, Geophys. Res. Lett., 33, L01301, doi:10.1029/2005GL024047.

Arcay, D., M.-P. Doin, E. Tric, R. Bousquet, and C. de Capitani (2006), Overriding plate thinning in subduction zones : Localized convection induced by slab dehydration, Geochem. Geophys. Geosyst., 7, Q02007, doi:10.1029/2005GC001061.

2007

Cavalié O., M.-P. Doin, C. Lasserre, P. Briole (2007), Ground motion measurement in the Lake Mead area, Nevada, by differential synthetic aperture radar interferometry time series analysis : Probing the lithosphere rheological structure, J. Geophys. Res., 112, B03403, doi:10.1029/2006JB004344.

2007- Arcay, D., E. Tric, and M. P. Doin, Slab surface temperature in subduction zones : Influence of the interplate decoupling depth and upper plate thinning processe, Earth and Planetary Science Letters, doi:10.1016/j.epsl.2006.12.027

Arcay D, Doin MP, Tric E, et al. (2007), Influence of the precollisional stage on subduction dynamics and the buried crust thermal state : Insights from numerical simulations TECTONOPHYSICS 441 (1-4) : 27-45 AUG 15

2008

Arcay, D., S. Lallemand, and M.-P. Doin (2008), Back-arc strain in subduction zones : Statistical observations versus numerical modeling, Geochem. Geophys. Geosyst., 9, Q05015, doi:10.1029/2007GC001875.

Cavalié 0., C. Lasserre, M.-P. Doin, G. Peltzer, J. Sun, X. Xu and Z.-K. Shen (2008), Measurement of interseismic strain across the Haiyuan fault (Gansu, China), by InSAR, Earth and Planetary Science Letters, 275, p 246-257, doi:10.1016/j.epsl.2008.07.057

Dumoulin C., G. Choblet, and M.P. Doin (2008), Convective interactions between oceanic lithosphere and asthenosphere : Influence of a transform fault, Earth and Planetary Science Letters, 274, p. 301-309, doi:10.1016/j.epsl.2008.07.017

V. Pinel, A. Hooper , S. De la Cruz-Reyna, G. Reyes-Davila, M. P. Doin, Study of the deformation field of two active Mexican stratovolcanoes (Popocatepetl and Colima Volcano) by time series of InSAR data., Fringe Workshop Proceedings, ESA Special Publication SP-649, 2008

2009

P. Lopez Quiroz, M.-P. Doin, F. Tupin, P. Briole, J.-M. Nicolas, Time series analysis of Mexico city subsidence constrained by radar Interferometry, Journal of Applied Geophysics, Volume : 69 Issue : 1 Special Issue : Sp. Iss. SI Pages : 1-15 Published : SEP 2009, DOI : 10.1016/j.jappgeo.2009.02.006

M.-P. Doin, C. Lasserre, G. Peltzer, 0. Cavalié, C. Doubre, Corrections of stratified tropospheric delays in SAR interferometry : validation with global atmospheric models, Journal of Applied Geophysics, Volume : 69 Issue : 1 Special Issue : Sp. Iss. SI Pages : 35-50 Published : SEP 2009, DOI : 10.1016/j.jappgeo.2009.03.010 PDF

2010

Grandin R, Socquet A, Doin MP, Jacques E, de Chabalier JB, King GCP, Transient rift opening in response to multiple dike injections in the Manda Hararo rift (Afar, Ethiopia) imaged by time-dependent elastic inversion of interferometric synthetic aperture radar data, JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH Volume : 115 Article Number : B11499 Published : NOV 13 2010,DOI : 10.1029/2010JB008020

M.-P. Doin, C. Twardzik, G. Ducret, C. Lasserre, S. Guillaso, and S. Jianbao, Crustal flexure around Siling Co lake in Tibet observed by InSAR, Proc. Dragon 2 Program Mid-Term Results 2008 2010, Guilin City, People's Republic of China 17-21 May 2010 (ESA SP-684, October 2010)

2011

A. Julea, N. Méger, P. Bolon, C. Rigotti, M.-P. Doin, C. Lasserre, E. Trouvé and V. Lazarescu., Unsupervised Spatiotemporal Mining of Satellite Image Time Series using Grouped Frequent Sequential Patterns, IEEE Transactions on Geoscience and Remote Sensing, 1417-1430 DOI : 10.1109/TGRS.2010.2081372, vol. 49, issue 4, 2011.

V. Pinel, A. Hooper , S. De la Cruz-Reyna, G. Reyes-Davila, M. P. Doin, P. Bascou, The challenging retrieval of the displacement field from InSAR data for andesitic stratovolvanoes : Case study of Popocatepetl and Colima Volcano, Mexico, Journal of Volcanology and Geothermal Research, v 200, 49-61 DOI : 10.1016/j.jvolgeores.2010.12.002, 2011

Jolivet, R., R. Grandin, C. Lasserre, M.-P. Doin, and G. Peltzer (2011), Systematic InSAR tropospheric phase delay corrections from global meteorological reanalysis data, Geophys. Res. Lett., 38, L17311, doi:10.1029/2011GL048757

Ducret G., M. P. Doin, R. Grandin , C. Lasserre and S. Guillaso (2011). DEM corrections before unwrapping in a small baseline strategy for InSAR time series analysis. Proc. Igarss., IEEE, p 1353-1356

M.-P. Doin, Felicity Lodge, S. Guillaso, R. Jolivet, C. Lasserre, G. Ducret, R. Grandin, E. Pathier, V. Pinel, Presentation of the small baseline NSBAS processing chain on a case example : the Etna deformation monitoring from 2003 to 2010 using Envisat data, Proc. ESA Fringe 2011 PDF

E. Trouvé, J.-M. Nicolas, L. Ferro-Famil, M. Gay, V. Pinel, M.-P. Doin, N. Méger, C. Lasserre,G. Mauris, F. Vernier, R. Fallourd,Y. Yan,O. Harant, R. Jolivet, Extraction et Fusion d'Informations pour la mesure de Déplacements par Imagerie Radar, Traitement du Signal , Vol. 28, N° 3-4 pp.375-416, 2011

2012

R. Jolivet, C. Lasserre, M.-P. Doin, S. Guillaso, G. Peltzer, R. Dailu, J. Sun, Z.-K. Shen and X. Xu, Shallow creep on the Haiyuan Fault (Gansu, China) observed by SAR Interferometry, J. Geophys. Res., 117, B06401, doi:10.1029/2011JB008732, 2012

Y. Yan, M.-P. Doin, P. Lopez-Quiroz, F. Tupin, B. Fruneau, V. Pinel, E. Trouvé, Mexico City subsidence measured by InSAR time series : Joint analysis using PS and SBAS approaches, accepted, IEEE,J. of Selected Topics in Applied Earth Observations and Remote Sensing, DOI:10.1109/JSTARS.2012.2191146, 2012 PDF

R. Grandin, M.-P. Doin , L. Bollinger , B. Pinel-Puysségur , G. Ducret , R. Jolivet , S. Sapkota , Long-term growth of the Himalaya inferred from interseismic InSAR measurement, Geology, September 18, 2012, doi : 10.1130/G33154.1

R. N. Nof, Ziv A., Doin M.P., Baer G., Fialko Y., Wdowinski S., Eyal Y., Bock Y., 2012, Rising of the lowest place on Earth due to Dead Sea water-level drop : Evidence from SAR Interferometry and GPS, J. Geophys. Res.,117 (B5) doi:10.1029/2011JB008961

M. Cerca, D. Carreón-Freyre, P.López-Quiroz, E. Ovando-Shelley, M.-P. Doin, R. Gutierrez-Calderón, M. González-Hernández, A. Jimenez-Sánchez and D. Blancas-Dominguez, Engineering geology approach to the effects of land subsidence in Mexico City, doi : 10.1130/2012.0025(06), GSA Field Guides 2012, v. 25, p. 115-134

2013

P. S. Agram, R. Jolivet, B. Riel, Y. N. Lin, M. Simons, E. Hetland, M.-P. Doin, and C. Lasserre, New Radar Interferometric Time Series Analysis Toolbox Released", Eos, Vol. 94, No. 7, 12 February 2013 PDF

R. Jolivet, C. Lasserre, M.-P. Doin, G. Peltzer, J.-P. Avouac, R. Dailu, J. Sun, Spatio-temporal evolution of aseismic slip along the Haiyuan fault, China : Implications for fault frictional properties, Earth Planet. Sci. Lett., accepted

Ducret G., M. P. Doin, R. Grandin, S. Guillaso and C. Lasserre, DEM corrections before unwrapping in a small baseline strategy for InSAR time series analysis. GRSL, IEEE, accepted

CV

Marie-Pierre DOIN — 2013-07-16T09:44:12Z

CURSUS

Sept 2012 à actuel : Chargée de recherche à ISTerre, Université Joseph Fourier, Grenoble

Fevrier 97 à Août 2012 : Chargée de recherche au Laboratoire de Géologie, Ecole Normale Supérieure, Paris

Mars 96 à Janvier 97 : Post-doctorat a l'Institut Océanographique de La Jolla, USA, avec D. Sandwell

Aout 95 à Février 96 : Post-doctorat a l'Institut de Géophysique de l'Université de Goettingen, avec U. Christensen (Allemagne)

1991/1995 : Thèse de Doctorat en Géophysique, au Laboratoire de Géologie, ENS, Paris, sous la direction de L. Fleitout, mention très honorable avec félicitations : "Structure thermique et pétrologique de la lithosphère océanique continentale et anomalies du champ de gravité terrestre"

1988-1992 : Elève à l'Ecole Normale Supérieure de Paris

THEMES DE RECHERCHE DÉVELOPPÉS

* Compréhension et modélisation des mécanismes qui régissent la défomation de la lithosphère et l'interaction de type convective entre lithosphère et manteau sous-jacent. Dans ce cadre, j'ai utilisé des modèles de déformation thermo-mécaniques et thermo-chimiques. Le paramètre principal de ce type d'étude est la ductilité du manteau supérieur et de la croûte, dont l'évaluation est un enjeu scientifique majeur.

* Mesure par interférométrie radar le déplacement de surface associé à des chargements ou déchargements lacustres. L'objectif de ces mesures est de connaître les propriétés rhéologiques des premiers 100 km de l'enveloppe terrestre, indispensables pour la compréhension des cycles sismique et volcanique.

* Développement de techniques permettant d'étendre l'applicabilité de l'InSAR, en terme de couverture géographique et de precision (infra-centrimétrique).

* Mesure de la déformation associée au cycle sismique autour des failles.

* Etude de la subsidence dans la vallée de Mexico.

PROJETS (DEPUIS 2008)

.
2008-2011 : Participation au projet EFIDIR de l'ANR 2007 Masses de données et connaissances, “Extraction et Fusion d'Information pour la mesure de Déplacements par Imagerie Radar”, PI : Emmanuel Trouvé, LISTIC, Université de Savoie, Responsable du SP2 sur la mesure du déplacement.

2008-2012 : Participation au programme de coopération Dragon-2 entre l'ESA et NRSCC (China), project ID 5305, PI C. Lasserre

2010-2012 : PI projet TerraSAR-X GEO0728 "Measure of Mexico City subsidence by high resolution TerraSAR-X interferometry", avec B. Puyssegur, V. Pinel, P. Lopez Quiroz

2010-2011 : INSU-PNTS : "Apport de l'interférométrie radar à haute résolution spatiale et temporelle à la mesure des déformations au Tibet". Rôle dans le projet : développement méthodologique et logiciel pour le calcul de série temporelle InSAR, coordination".

2010-2011 : INSU-Risques et catastrophes telluriques :"Etude géodésique et sismologique conjointe de l'accumulation de la déformation intersismique à travers l'Himalaya : apport de l'interférométrie satellitaire SAR". Rôle dans le projet : coll. avec R. Grandin, développements méthodologiques InSAR, interprétation de la déformation

2012-2016 : Participation au programme de coopération Dragon-3 entre l'ESA et NRSCC (China), project ID 5305, PI C. Lasserre

2012-2014 : LONGRIBA : "Faille de Longriba : la clef pour comprendre la tectonique de la marge Est du plateau Tibétain ?", ANR Jeune Chercheur portée par J. De Sigoyer. Rôle dans le projet : Séries temporelles InSAR sur Longriba, modélisation.

2013-2015 : MEGA-CHILI : "Mega-séismes au Chili : Exemple de Maule en 2010 (Mw 8.8) et implications sismo-tectoniques", ANR blanche portée par C. Vigny. Rôle dans le projet : co-encadrement de la thèse de G. Ducret : observation par InSAR de l'accumulation intersismique de la déformation au Chili Central.

LONGRIBA project : Unravel the tectonics of the Eastern Tibetan Margin

Anaïs SCHNEIDER, Marie-Pierre DOIN — 2011-10-17T13:11:00Z

The Longriba fault : the key to unravel the tectonics of the Eastern Tibetan Margin ?

PI : De Sigoyer, Julia, Laboratoire de Géologie, Ecole Normale Supérieure, Paris ISTerre research team involved : Seismic cycle and transient deformations

ABSTRACT
The paradox of a high eastern Tibetan plateau associated with very low convergence rate (Shen et al., 2005 ; Gan et al., 2007) has led to an underestimation of the seismic hazard in the Longmen Shan area (China) prior to the May 12th 2008, Mw 7.9 earthquake. A crucial problem in our understanding of the seismic hazard in Eastern Tibet is the difficulty of reconciling long-term geological studies (several millions years), which suggest strong thickening of the Tibetan margin and the Longmen Shan belt, and short-term geophysical studies (seconds to decades) that show low convergence rate across this area. Compounding this difficulty is the complex structural geology of the margin, which comprises a large number of poorly-understood faults that interact in as-yet-unknown ways. In this project we will investigate this paradox directly, focusing our study on the Longriba fault system located 150 km west of the Longmen Shan front. This fault is a key structure that is rarely taken into account in conceptual frameworks for the geodynamics and seismo-tectonics of this area, although it seams to accommodate a large part of the present-day relative movement (6-8 mm/yr) between the Songpan block (Bayan Har block) and the south China block (Thatcher, 2007, Shen et al 2005). It seems also to partition the movement between dextral strike-slip movement along the fault itself and residual E-W convergence that is taken on the Longmen Shan. The interaction between the Longriba fault and the faults in the Longmen Shan is critical, because its estimated Quaternary slip rate is an order of magnitude higher than that of the Longmen Shan faults ; it may thus account for a large part of the present-day deformation, and must be accounted for in any regional assessment of seismic hazard.
The first aim of this proposal (Task 2) is to characterize and quantify the recent activity of the Longriba fault system by geodetic, neotectonic, and strain rate modelling analyses. The potential interactions between the Longriba system and the southern Xianshui He and East Kunlun faults will be also studied, to understand its role in a regional context.

The second aim of this proposal (Task 3) is to estimate the activation age of the Longriba fault with geomorphic analyses and dating (cosmogenic, OSL), and to use low-temperature thermochronology to understand the potential role of Longriba fault in accommodating uplift of the eastern Tibetan plateau in this area,. We expect that the uplift of the Tibetan plateau occurred before the (very recent) activation of the Longriba fault, implying that the pre-Longriba tectonic framework could was very different from that at present, allowing more convergence across the eastern Tibetan margin and Longmen Shan belt than today.
Recent geochemical studies on the eastern Songpan Garze Triassic granitoids suggest that the Longriba fault could be located in a place of slab retreat and slab break-off at the boundary between the Yangtze craton margin and a Paleozoic ocean.

The third aim of this proposal (Task 4) is to test this hypothesis, with geochemical tracer of the origin of these granites (major, trace and isotopic elements) and geochronological (U-Th-Pb system) data to understand the importance of geological inheritance to the present day tectonic setting. Via high-precision petrostructural study and dating (U-Th-Pb La-ICPMS and 39Ar-40Ar) we will produce scenarios for the deformation history of the Songpan Garze area and for the thickening of the eastern plateau margin since Triassic time.

Figure 1 : Secular block-motion model derived from synthesizing measurements of from 1999 to 2007 (Shen et al., 2009). GPS velocities are referenced to the south China block. Error ellipses represent 70% confidence. Red lines are the surface breaks of the Sichuan earthquake.
The Bayar Han block =Aba block+SW Longmen Shan block

Longriba Fault

Regional GPS data of Shen et al. (2005, 2009) show displacement of eastern Tibet toward the NE at 6 to 8 mm/yr, relative to a fixed Sichuan Basin. To examine how strain is partitioned, Shen et al. 2009 devised a block-motion model constrained using regional pre-earthquake GPS velocities (Fig. 3). For the region between the East Kunlun fault to the north and the Xianshuihe fault to the south, most of the relative motion between the eastern Tibetan plateau and Sichuan basin (4-5 mm/yr) appears to be accommodated along the dextral Longriba fault system, located 150 km northwest of and parallel to the Longmen Shan faults. The remaining part (<2 mm/yr) has to be absorbed by tectonic structures located between the two domains, in the SW Longmen Shan block and at the Longmen Shan front. We stress that these inferred slip rates are 5-10 times greater than those of the faults in the Longmen Shan described above.

The Longriba fault is a system of NE-trending parallel dextral and thrust faults (Xu et al., 2008) in the eastern Bayan Har block (that represents most of the Songpan Garze unit see the insert map of the Tibet). The northeastern segment of the Longriba fault consists of two subparallel N54±5°E trending branch faults about 30 km apart, with Quaternary offset landforms related to the fault segments. The northern branch fault, also termed the Longriba fault, has a relatively large reverse component, while the southern branch fault, the Maoergai fault, is inferred to be a pure right-lateral strike slip fault (Fig.1, Fig. 4). A swarm of seismicity has been observed along the southern part of the Longriba faults but no other studies were published on active deformation of Longriba fault in this area.

The previous regional geodetic studies have delivered a better understanding for the active tectonic framework of the area, showing that most of the deformation is taken up on quasi-unknown Longriba fault system. This partitioned system may explain why the present-day convergent rates are so low across the Longmen Shan belt. However, the lack of information on the structure and history of the Longriba fault, coupled with the recent demonstration that the greater Longmen Shan region continues to be tectonically active, leads to the conclusion that there is an urgent need for a better documentation of this fault system.