Comptes Rendus

Sommaire

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 ?
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