0191-8141/94 $07.00+0.00 Extensional origin of ductile fabrics in the Schist Belt, Central Brooks

Abstract--A regional system of S-dipping faults is exposed in the Florence and Fall Creeks area of the south-central Brooks Range. This fault system has previously been mapped as the 'root zone ' of a N-vergent fold-and-thrust belt of Jurassic-Cretaceous age, although individual faults jux...

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Bibliographic Details
Main Authors: Alaskamii Microstructural, Petrofabric Evidence, Richard D. Law, Elizabeth L. Miller, Timothy A. Liti'le
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1992
Subjects:
Bya
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.517.6687
http://www.geology.cwu.edu/facstaff/lee/publications/pdf.papers/AL2.JSG.pdf