S
Siegfried Lallemant
Researcher at Cergy-Pontoise University
Publications - 50
Citations - 3479
Siegfried Lallemant is an academic researcher from Cergy-Pontoise University. The author has contributed to research in topics: Accretionary wedge & Subduction. The author has an hindex of 29, co-authored 50 publications receiving 3320 citations. Previous affiliations of Siegfried Lallemant include École Normale Supérieure.
Papers
More filters
Journal ArticleDOI
Geodetic determination of the kinematics of central Greece with respect to Europe: Implications for eastern Mediterranean tectonics
TL;DR: In this paper, the authors used a new satellite laser ranging/global positioning system (SLR/GPS) solution at seven sites in Anatolia and Aegea to obtain a better definition of the extrusion motion of the Anatolian-Aegean block with respect to Europe.
Journal ArticleDOI
Two‐ship deep seismic soundings in the basins of the Eastern Mediterranean Sea (Pasiphae cruise)
B. de Voogd,C. Truffert,Nicolas Chamot-Rooke,Philippe Huchon,Siegfried Lallemant,X. Le Pichon +5 more
TL;DR: In this article, a two-ship refraction and oblique reflection deep seismic cruise is used to discuss the nature of the crust in the Ionian, Sirte and Herodotus abyssal plains.
Journal ArticleDOI
Origin and evolution of a splay fault in the Nankai accretionary wedge
Michael Strasser,Gregory F. Moore,Gregory F. Moore,Gaku Kimura,Gaku Kimura,Yujin Kitamura,Achim J Kopf,Siegfried Lallemant,Jin-Oh Park,Jin-Oh Park,Elizabeth J. Screaton,Xin Su,Michael B. Underwood,Xixi Zhao +13 more
TL;DR: In this article, the authors combine seismic reflection data from the Nankai accretionary wedge with geological data collected by the Integrated Ocean Drilling Program (IODP) and find that the splay fault cutting this wedge initiated approximately 1.95 million years ago in the lower part of the prism as an out-of-sequence thrust (OOST).
Journal ArticleDOI
E–W opening of the Algerian Basin (Western Mediterranean)
TL;DR: In this article, geophysical and geological evidence of fast (2 cm yr )1 in the east and 5 cm yr 1 in the west) E-W spreading between 16 and 8 Ma in the region behind the Gibraltar Arc in the Algerian Basin.