HelioWebUniversite de Cergy-Pontoise, France
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I[Universite de Cergy-Pontoise, France]
PI["Parent Institutions (0)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (16)"]
CA["Linked Collaborating Authors (0)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Micro-seismicity recorded during a gallery excavation in the Opalinus Clay of the Mont Terri URL: preliminary description of in situ damage mechanism
- Using crustal thickness, subsidence and P-T-t history on the Iberia-Newfoundland & Alpine Tethys margins to constrain lithosphere deformation modes during continental breakup
- Constraining Lithosphere Deformation Modes during Continental Breakup for the Iberia-Newfoundland Conjugate Margins
- Laboratory study of mechanical and petrophysical properties of both intact and naturally fractured shale samples from the Tournemire Underground Research Laboratory
- Mechanical Weakening during Fluid Injection in Critically Stressed Sandstones with Acoustic Monitoring
- Structural and Stratigraphic Evolution of the Iberia and Newfoundland Rifted Margins: A Quantitative Modeling Approach
- Mechanical and petrophysical study of fractured shale materials
- Mechanical Anisotropies and Mechanisms of Mafic Magma Ascent in Middle Continental Crust: The Sondalo Gabbroic Complex (N Italy)
- Extreme Mesozoic crustal thinning in the Eastern Iberia margin: The example of the Columbrets Basin (Valencia Trough)
- Strength and Anisotropy in Tournemire Shale: Temperature, Pressure and Time Dependences
- Thinning of heterogeneous lithosphere: insights from field observations and numerical modelling
- Rapid Transition from Continental Breakup to Igneous Oceanic Crust in the South China Sea
- Rift-inheritance and subduction initiation at magma-poor rifted margins: implications for the formation of Alpine-type orogens
- Subduction Initiation at Passive Margins and Amagmatic Basin Closure: The Revival of Ampferer-Type Subduction and the Formation of Alpine-type Orogens
- Inverse Analysis of Pearl River Source-to-Sink System, South China: Implications for SE Tibetan Uplift and Asian Monsoon Intensities
- Time and Temperature Dependent Creep in Tournemire Shale