scholarly journals Crustal structure of the basin and ridge system west of New Caledonia (southwest Pacific) from wide-angle and reflection seismic data

2007 ◽  
Vol 112 (B11) ◽  
Author(s):  
F. Klingelhoefer ◽  
Y. Lafoy ◽  
J. Collot ◽  
E. Cosquer ◽  
L. Géli ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Seismic Data ◽  
New Caledonia ◽  
Wide Angle ◽  
Southwest Pacific ◽  
Reflection Seismic ◽  
Ridge System

scholarly journals The crustal structure of the NW Moroccan continental margin from wide-angle and reflection seismic data

2004 ◽  
Vol 159 (1) ◽  
pp. 117-128 ◽  
Author(s):  
I. Contrucci ◽  
F. Klingelhöfer ◽  
J. Perrot ◽  
R. Bartolome ◽  
M.-A. Gutscher ◽  
...  
Keyword(s):  
Continental Margin ◽  
Crustal Structure ◽  
Seismic Data ◽  
Wide Angle ◽  
Reflection Seismic

The crustal structure of the Moroccan continental margin from wide-angle and reflection seismic data

2007 ◽  
Author(s):  
Frauke Klingelhoefer ◽  
Daniel Aslanian* ◽  
Cynthia Labails ◽  
Jean-Louis Olivet ◽  
Hervé Nouzé ◽  
...  
Keyword(s):  
Continental Margin ◽  
Crustal Structure ◽  
Seismic Data ◽  
Wide Angle ◽  
Reflection Seismic

The crustal structure of the Moroccan continental margin from wide-angle and reflection seismic data

2007 ◽  
Author(s):  
Frauke Klingelhoefer ◽  
Isabelle Contrucci ◽  
Daniel Aslanian ◽  
Cynthia Labails ◽  
Jean-Louis Olivet ◽  
...  
Keyword(s):  
Continental Margin ◽  
Crustal Structure ◽  
Seismic Data ◽  
Wide Angle ◽  
Reflection Seismic

scholarly journals Crustal structure of the SW-Moroccan margin from wide-angle and reflection seismic data (the DAKHLA experiment) Part A: Wide-angle seismic models

2009 ◽  
Vol 468 (1-4) ◽  
pp. 63-82 ◽  
Author(s):  
F. Klingelhoefer ◽  
C. Labails ◽  
E. Cosquer ◽  
S. Rouzo ◽  
L. Géli ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Seismic Data ◽  
Wide Angle ◽  
Reflection Seismic ◽  
Seismic Models

scholarly journals Deep crustal structure of the North-West African margin from combined wide-angle and reflection seismic data (MIRROR seismic survey)

2015 ◽  
Vol 656 ◽  
pp. 154-174 ◽  
Author(s):  
Y. Biari ◽  
F. Klingelhoefer ◽  
M. Sahabi ◽  
D. Aslanian ◽  
P. Schnurle ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Seismic Data ◽  
West African ◽  
Seismic Survey ◽  
Wide Angle ◽  
North West ◽  
Reflection Seismic ◽  
The North ◽  
Deep Crustal Structure

scholarly journals Crustal structure variations along the NW-African continental margin: A comparison of new and existing models from wide-angle and reflection seismic data

2016 ◽  
Vol 674 ◽  
pp. 227-252 ◽  
Author(s):  
Frauke Klingelhoefer ◽  
Youssef Biari ◽  
Mohamed Sahabi ◽  
Daniel Aslanian ◽  
Michael Schnabel ◽  
...  
Keyword(s):  
Continental Margin ◽  
Crustal Structure ◽  
Seismic Data ◽  
Wide Angle ◽  
Reflection Seismic

Deep crustal structure across a young passive margin from wide-angle and reflection seismic data (The SARDINIA Experiment) – II. Sardinia’s margin

2015 ◽  
Vol 186 (4-5) ◽  
pp. 331-351 ◽  
Author(s):  
Alexandra Afilhado ◽  
Maryline Moulin ◽  
Daniel Aslanian ◽  
Philippe Schnürle ◽  
Frauke Klingelhoefer ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Passive Margin ◽  
Data Sets ◽  
Wide Angle ◽  
Seismic Velocities ◽  
The West ◽  
Reflection Seismic ◽  
Gulf Of Lion ◽  
Deep Crustal Structure ◽  
Domain Iii

Abstract Geophysical data acquired on the conjugate margins system of the Gulf of Lion and West Sardinia (GLWS) is unique in its ability to address fundamental questions about rifting (i.e. crustal thinning, the nature of the continent-ocean transition zone, the style of rifting and subsequent evolution, and the connection between deep and surface processes). While the Gulf of Lion (GoL) was the site of several deep seismic experiments, which occurred before the SARDINIA Experiment (ESP and ECORS Experiments in 1981 and 1988 respectively), the crustal structure of the West Sardinia margin remains unknown. This paper describes the first modeling of wide-angle and near-vertical reflection multi-channel seismic (MCS) profiles crossing the West Sardinia margin, in the Mediterranean Sea. The profiles were acquired, together with the exact conjugate of the profiles crossing the GoL, during the SARDINIA experiment in December 2006 with the French R/V L’Atalante. Forward wide-angle modeling of both data sets (wide-angle and multi-channel seismic) confirms that the margin is characterized by three distinct domains following the onshore unthinned, 26 km-thick continental crust : Domain V, where the crust thins from ~26 to 6 km in a width of about 75 km; Domain IV where the basement is characterized by high velocity gradients and lower crustal seismic velocities from 6.8 to 7.25 km/s, which are atypical for either crustal or upper mantle material, and Domain III composed of “atypical” oceanic crust. The structure observed on the West Sardinian margin presents a distribution of seismic velocities that is symmetrical with those observed on the Gulf of Lion’s side, except for the dimension of each domain and with respect to the initiation of seafloor spreading. This result does not support the hypothesis of simple shear mechanism operating along a lithospheric detachment during the formation of the Liguro-Provencal basin.

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