Long-term hydrodynamic response induced by past climatic and geomorphologic forcing: The case of the Paris basin, France

[1]  S. Violette,et al.  Osmotic interpretation of overpressures from monovalent based triple layer model, in the Callovo-Oxfordian at the Bure site , 2007 .

[2]  L. Millet,et al.  Late-Glacial climatic changes in Eastern France (Lake Lautrey) from pollen, lake-levels, and chironomids , 2005, Quaternary Research.

[3]  A. Jost.  Caractérisation des forçages climatiques et géomorphologiques des cinq derniers millions d'années et modélisation de leurs conséquences sur un système aquifère complexe : le bassin de Paris , 2005 .

[4]  P. Valdes,et al.  High-resolution simulations of the last glacial maximum climate over Europe: a solution to discrepancies with continental palaeoclimatic reconstructions? , 2005 .

[5]  Maurice Pagel,et al.  Contribution of a three‐dimensional regional scale basin model to the study of the past fluid flow evolution and the present hydrology of the Paris basin, France , 2004 .

[6]  U. Michie,et al.  Estimating hydrogeological conditions over the last 120 ka: an example from the Sellafield area, UK , 2004, Journal of the Geological Society.

[7]  S. Violette,et al.  Analytical and numerical solutions for alternative overpressuring processes: Application to the Callovo-Oxfordian sedimentary sequence in the Paris basin, France , 2004 .

[8]  P. Courville,et al.  Mio–Pliocene to Pleistocene paleotopographic evolution of Brittany (France) from a sequence stratigraphic analysis: relative influence of tectonics and climate , 2004 .

[9]  Z. X. Li,et al.  Transient response of an atmospheric GCM to North Atlantic SST anomalies , 2003 .

[10]  T. Zhou,et al.  Simulation of the east asian summer monsoon using a variable resolution atmospheric GCM , 2002 .

[11]  Paul Johnston,et al.  Timing of the Last Glacial Maximum from observed sea-level minima , 2000, Nature.

[12]  J. Brun,et al.  Large‐scale relief development related to Quaternary tectonic uplift of a Proterozoic‐Paleozoic basement: The Armorican Massif, NW France , 2000 .

[13]  P. Allemand,et al.  Meso-Cenozoic geodynamic evolution of the Paris Basin: 3D stratigraphic constraints , 2000 .

[14]  P. Antoine,et al.  Long-term fluvial archives in NW France: response of the Seine and Somme rivers to tectonic movements, climatic variations and sea-level changes , 2000 .

[15]  J. Vandenberghe,et al.  River response to variations of periglacial climate in mid-latitude Europe , 2000 .

[16]  C. E. Neuzil,et al.  Osmotic generation of ‘anomalous’ fluid pressures in geological environments , 2000, Nature.

[17]  S. Occhietti,et al.  Le fleuve Seine, le fleuve Manche , 1999 .

[18]  J. Vandenberghe,et al.  Climatic reconstruction of the Weichselian Pleniglacial in northwestern and Central Europe , 1998 .

[19]  J. Roux,et al.  Contrôle morphostructural de l'histoire d'un réseau hydrographique: le site de capture de la Moselle , 1998 .

[20]  J. Burrus.  Memoir 70, Chapter 3: Overpressure Models for Clastic Rocks, Their Relation to Hydrocarbon , 1998 .

[21]  Y. Dewolf,et al.  Surfaces d9erosion polygeniques dans les formations cenozoiques du bassin Parisien , 1997 .

[22]  K. Høeg,et al.  Effects of burial diagenesis on stresses, compaction and fluid flow in sedimentary basins , 1997 .

[23]  Gilles Lericolais.  Evolution plio-quaternaire du fleuve Manche : stratigraphie et géomorphologie d'une plateforme continentale en régime périglaciaire , 1997 .

[24]  C. Neuzil.  Abnormal pressures as hydrodynamic phenomena , 1995 .

[25]  M. Sarnthein,et al.  Astronomic timescale for the Pliocene Atlantic δ18O and dust flux records of Ocean Drilling Program Site 659 , 1994 .

[26]  T. C. Winter,et al.  The role of permafrost and seasonal frost in the hydrology of northern wetlands in North America , 1993 .

[27]  J. Vandenberghe.  Changing fluvial processes under changing periglacial conditions. , 1993 .

[28]  S. Ge,et al.  Hydromechanical modeling of tectonically driven groundwater flow with application to the Arkoma Foreland Basin , 1992 .

[29]  Julian A. Dowdeswell,et al.  Glacimarine Environments: Processes and Sediments , 1990 .

[30]  E. Bard,et al.  U-Th ages obtained by mass spectrometry in corals from Barbados: sea level during the past 130,000 years , 1990, Nature.

[31]  E. Bard,et al.  Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U–Th ages from Barbados corals , 1990, Nature.

[32]  Harry J. Dowsett,et al.  High eustatic sea level during the middle Pliocene:Evidence from the southeastern U.S. Atlantic Coastal Plain , 1990 .

[33]  R. Fairbanks.  A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation , 1989, Nature.

[34]  L. L. Sloss.  The geology of North America , 1988 .

[35]  C. E. Sloan,et al.  Region 28, Permafrost Region , 1988 .

[36]  S. M. Greenlee,et al.  Recognition and Interpretation of Depositional Sequences and Calculation of Sea-Level Changes From Stratigraphic Data—Offshore New Jersey and Alabama Tertiary , 1988 .

[37]  C. A. Ross,et al.  Sea-level changes: An integrated approach , 1986 .

[38]  J. Tóth,et al.  Possible effects of erosional changes of the topographic relief on pore pressures at depth , 1983 .

[39]  C. Neuzil,et al.  Erosional Unloading and Fluid Pressures in Hydraulically "Tight" Rocks , 1983, The Journal of Geology.