Zobrazeno 1 - 10
of 46
pro vyhledávání: '"Siegfried Lallemant"'
Autor:
Hideki Masago, Moe Kyaw Thu, Elizabeth Screaton, Gaku Kimura, Siegfried Lallemant, Juichiro Ashi, Masataka Kinoshita, Harold Tobin, Daniel Curewitz, IODP Expeditions 314/315/316 Scientific Party
Publikováno v:
Scientific Drilling, Iss 8, Pp 4-17 (2009)
Integrated Ocean Drilling Program (IODP) Expeditions 314, 315, and 316 were carried out as a unified program of drilling collectively known as Stage 1 of the Nankai Trough Seismogenic Zone Experiment, or NanTroSEIZE, the first multi-stage complex dri
Externí odkaz:
https://doaj.org/article/1256974cba3544ac81e3acb8c312c3e8
Autor:
Matthias Delescluse, Nicolas Chamot-Rooke, Siegfried Lallemant, Philippe Huchon, Marc Fournier, Mathieu Rodriguez, Sébastien Zaragosi, Nicolas Mouchot
Publikováno v:
Tectonophysics
Tectonophysics, Elsevier, 2014, pp.1-49. ⟨10.1016/j.tecto.2014.08.001⟩
Tectonophysics, 2014, pp.1-49. ⟨10.1016/j.tecto.2014.08.001⟩
Tectonophysics, Elsevier, 2014, pp.1-49. ⟨10.1016/j.tecto.2014.08.001⟩
Tectonophysics, 2014, pp.1-49. ⟨10.1016/j.tecto.2014.08.001⟩
International audience; The Dalrymple Trough is a 150-km-long, 30-km-wide basin located at the northern termination of the Owen Fracture Zone (OFZ), which is the present-day active India-Arabia plate boundary. The Dalrymple Trough is closely associat
Publikováno v:
Earth and Planetary Science Letters
Earth and Planetary Science Letters, Elsevier, 2013, pp.43-60. ⟨10.1016/j.epsl.2013.02.038⟩
Earth and Planetary Science Letters, Elsevier, 2013, pp.43-60. ⟨10.1016/j.epsl.2013.02.038⟩
The maximum strength theorem is applied to determine the pressure conditions in accretionary wedges responsible for the activation of splay faults (SF). This theorem, based on the limit analysis developed in soil mechanics, selects among several mode
Autor:
Julien Bourget, Thierry Garlan, Nicolas Mouchot, Nadine Ellouz-Zimmermann, Siegfried Lallemant, Valentine Lanfumey, Sébastien Zaragosi, Jean-Luc Schneider
Publikováno v:
Sedimentology. 58:376-406
Julien Bourget, Sebastien Zaragosi, Nadine Ellouz-Zimmermann, Nicolas Mouchot, Thierry Garlan, Jean-Luc Schneider, Valentine Lanfumey and Sigfried Lallemant
Autor:
Lies Loncke, Siegfried Lallemant, Julien Bourget, Geoffroy Mahieux, Pascale Leturmy, Nadine Ellouz-Zimmermann, Nicolas Mouchot
Publikováno v:
Marine Geology. 271:17-31
A geophysical and geological survey (CHAMAK) has been carried out on the Makran accretionary wedge off Pakistan in order to understand the structure of the margin and the recent sedimentary processes in this self-maintaining prism disconnected from t
Publikováno v:
Basin Research. 22:361-379
This paper discusses the origin and the dynamics of subsurface sediment mobilization processes in tectonically mobile regions and shale-rich environment. This is illustrated by the example of Trinidad and the south of the Barbados prism. In this area
Autor:
Siegfried Lallemant, Xin Su, Elizabeth J. Screaton, Michael B. Underwood, Jin-Oh Park, Yujin Kitamura, Achim J Kopf, Xixi Zhao, Gregory F. Moore, Gaku Kimura, Michael Strasser
Publikováno v:
Nature Geoscience. 2:648-652
Subduction zones are often characterized by wedge-shaped sedimentary complexes—called accretionary prisms—that form when sediments are scraped off the subducting plate and added to the overriding plate. Large, landward-dipping thrust faults can c
Autor:
Jean-Paul Cadet, Siegfried Lallemant, Pierre Cochonat, Christine Fouchet, Jean Paul Foucher, Stéphane Mazzotti, Hervé Nouzé
Publikováno v:
Marine Geology. 187:193-202
One main feature imaged on the Nankai slope by using the SAR/PASISAR system (deep-tow single-channel seismic streamer) during the Franco-Japanese KAIKO-Tokai cruise in April 1996 is the gravitational displacement of large volumes of the sediment. Thi
Autor:
Pierre Henry, Xavier Le Pichon, Siegfried Lallemant, Hidekazu Tokuyama, Stéphane Mazzotti, Narumi Takahashi
Publikováno v:
Marine Geology. 187:63-88
Due to the collision of the Izu-Bonin arc with central Japan, the subducting Philippine Sea oceanic plate is affected by lithospheric shortening seaward of the eastern Nankai trough, in the Zenisu ridge area. Seismic reflection and refraction profile
Publikováno v:
Marine Geology. 186:111-125
The core of the Mediterranean Ridge backstop consists of a pile of Hellenic nappes that migrated outward from the Aegean continent within the adjacent Mediterranean basins during late middle Miocene, about 15 Ma, and the present Mediterranean Ridge h