THE JURASSIC METAMORPHISM IN THE CENTRAL HIGH ATLAS (MOROCCO) - SUCCESSIVE SYNTECTONIC AND HYDROTHERMAL EPISODES

Citation
E. Laville et al., THE JURASSIC METAMORPHISM IN THE CENTRAL HIGH ATLAS (MOROCCO) - SUCCESSIVE SYNTECTONIC AND HYDROTHERMAL EPISODES, Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 318(10), 1994, pp. 1349-1356
Citations number
23
Categorie Soggetti
Multidisciplinary Sciences
ISSN journal
07644450
Volume
318
Issue
10
Year of publication
1994
Part
2
Pages
1349 - 1356
Database
ISI
SICI code
0764-4450(1994)318:10<1349:TJMITC>2.0.ZU;2-#
Abstract
In the Central High Atlas axis, the Triassic to Mid-Jurassic sedimenta ry and magmatic rocks have been affected by a polyphased contact and h ydrothermal metamorphism characterized by a relatively high geothermal gradient, contemporaneous with the emplacement of the Jurassic pluton ic suite in a transcurrent setting.