Sedimentary record of the northward flight of India and its collision
Neotethys and continental collision in the NW Himalaya. Les phases initiales de la collision continentale et de I'obduction se sont.
Continental collision crustal thinning and nappe forming during the
Continental collision crustal thinning and nappe forming during the pre-Miocene R. (1993) Les formations oligo-miocenes supra-Malaguides. (Cordil-.
Continental margin response to multiple arc-continent collisions
The first heralds the arrival of the first intra- oceanic arc to the southernmost northern Andes in late Campanian times younging-northward as the collision
Strain partitioning in the transition area between oblique subduction
subduction and continental collision Hikurangi margin
Channel flow ductile extrusion and exhumation in continental
lower to mid-crust in continental collision zones' flow originated in the continental tectonics litera- ... en rubans dans les mylonites. Bulletin de la.
Godin etal ChannelFlow GSLSp
NUMERICAL MODELING OF INTRAPLATE DEFORMATION
Dec 10 1982 MODELS OF CONTINENTAL. COLLISION. J.P.. Vilotte and M. Daigni•res. Centre G•ologique et G•ophysique
Vilottedaignieres
Exhumation during a continental collision inferred from the
Exhumation during a continental collision inferred from the tectonometamorphic evolution of the Alpujarride Complex in the central Betics (Alboran Domain
Gondwanide continental collision and the origin of Patagonia
LES-119. Prietogranodiorite 273. 6.19 33.58. 0.1113 0.512232 0.512033. −5.0 1448 161 168 of continental collision in the formation of the.
Gondwanide continental collision and the origin of Patagonia - RJ
continental collision in the formation of the Gondwana fold belts of South America Africa LES-118. 250 ± 2. LES-119. 273 ± 2. LES-122. 246 ± 2. LES-125.
Pankhurst EARTH Text
Etude du magmatisme aux zones de subduction et de l'érosion
l'érosion continentale par les séries de l'Uranium : contraintes sur les processus et systematics across an active island arc-continent collision zone:.