Inversion of synrift normal faults in the High Atlas Mountains, Morocco

dc.contributor.author	Beauchamp, W.
dc.contributor.author	Barazangi, M.
dc.contributor.author	Demnati, A.
dc.contributor.author	El Alji, M.
dc.date.accessioned	2007-01-26T16:18:24Z
dc.date.available	2007-01-26T16:18:24Z
dc.date.issued	1997
dc.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	en_US
dc.description.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.	en_US
dc.format.extent	966600 bytes
dc.format.mimetype	application/pdf
dc.identifier.citation	The Leading Edge, vol. 16, p. 1171-1175, 1997	en_US
dc.identifier.issn	1070-485X
dc.identifier.uri	https://hdl.handle.net/1813/5271
dc.language.iso	en	en_US
dc.publisher	Society for Exploration Geophysics (SEG)	en_US
dc.subject	Atlas Mountains	en_US
dc.subject	Morocco	en_US
dc.subject	Inversion of synrift normal fault	en_US
dc.subject	Inversion tectonics	en_US
dc.title	Inversion of synrift normal faults in the High Atlas Mountains, Morocco	en_US
dc.type	periodical	en_US

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