Skip to main content


eCommons@Cornell

eCommons@Cornell >
College of Engineering >
Earth and Atmospheric Sciences >
Active Tectonics, Geophysics, and Structure >
Middle East and North Africa Region Projects >

Please use this identifier to cite or link to this item: http://hdl.handle.net/1813/5271
Title: Inversion of synrift normal faults in the High Atlas Mountains, Morocco
Authors: Beauchamp, W.
Barazangi, M.
Demnati, A.
El Alji, M.
Keywords: Atlas Mountains
Morocco
Inversion of synrift normal fault
Inversion tectonics
Issue Date: 1997
Publisher: Society for Exploration Geophysics (SEG)
Citation: The Leading Edge, vol. 16, p. 1171-1175, 1997
Abstract: Structural inversion related to intracontinental rifting occurs when extensional rift faults reverse their sense of motion during subsequent episodes of compressional tectonics. Features generated by extension, such as half grabens, are uplifted to form positive anticlinal structures.
Description: Copyright 1997, Society for Exploration Geophysics. See also: http://segdl.aip.org/getabs/servlet/GetabsServlet?prog=normal&id=LEEDFF000016000008001171000001&idtype=cvips&gifs=Yes; http://atlas.geo.cornell.edu/morocco/publications/beauchamp1997.htm
URI: http://hdl.handle.net/1813/5271
ISSN: 1070-485X
Appears in Collections:Prof. Muawia Barazangi
Middle East and North Africa Region Projects

Files in This Item:

File Description SizeFormat
Beauchamp et al 1997 TLE.pdf943.95 kBAdobe PDFView/Open

Refworks Export

Items in eCommons are protected by copyright, with all rights reserved, unless otherwise indicated.

 

© 2014 Cornell University Library Contact Us