Abstract
Abstract Tauch mountain southeast of the Mouthoumet Paleozoic massif, France, is composed of Aptian and Cenomanian (Cretaceous) deposits and has generally been considered a remnant of the Mesozoic sedimentary cover which formerly capped the massif. The Cretaceous deposits of the mountain are folded, and the structure may represent a second-order thrust without an overturned flank. The mechanics of emplacement are discussed.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
