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Table of contents


CV2 - Editorial board ENG
p. IFC

Page de Sommaire
p. iii

Comment la Terre a-t-elle pu vieillir de plus de quatre milliards d’années en quatre siècles ?
[How could the Earth become more than 4 billions years old in only four centuries?]
Géré par Vincent Courtillot Hubert Krivine
p. 91-95

Internal Geophysics
Intraplate earthquakes and their link with mantle dynamics: Insights from P-wave teleseismic tomography along the northern part of the North–South Tectonic Zone in China
Handled by Michel Campillo Chuansong He; M. Santosh
p. 96-105

Internal Geophysics
Local gravity field modeling using spherical radial basis functions and a genetic algorithm
Handled by Philippe Cardin Hany Mahbuby; Abdolreza Safari; Ismael Foroughi
p. 106-113

Petrology, Geochemistry
Measuring the surface roughness of geological rock surfaces in SAR data using fractal geometry
Handled by Isabelle Manighetti Ali Ghafouri; Jalal Amini; Mojtaba Dehmollaian; Mohammad Ali Kavoosi
p. 114-125

Tectonics, Tectonophysics
The northwest-directed “Bretonian phase” in the French Variscan Belt (Massif Central and Massif Armoricain): A consequence of the Early Carboniferous Gondwana–Laurussia collision
Handled by Vincent Courtillot Michel Faure; Xian-Hua Li; Wei Lin
p. 126-136
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Published by : Académie des Sciences CNRS
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