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anticlinoria

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Series: GSA Field Guide
Published: 01 January 2017
DOI: 10.1130/2017.0047(01)
EISBN: 9780813756479
FIGURES | View All (36)
Series: GSA Field Guide
Published: 01 January 2010
DOI: 10.1130/2010.0016(05)
EISBN: 9780813756165
Journal Article
Journal: GSA Bulletin
Published: 01 August 1998
GSA Bulletin (1998) 110 (8): 1060-1074.
Journal Article
Journal: GSA Bulletin
Published: 01 March 1998
GSA Bulletin (1998) 110 (3): 311-325.
Journal Article
Published: 01 March 1998
Journal of Paleontology (1998) 72 (2): 303-316.
Journal Article
Published: 01 June 1996
Bulletin of Canadian Petroleum Geology (1996) 44 (2): 337-348.
Journal Article
Published: 01 October 1995
Canadian Journal of Earth Sciences (1995) 32 (10): 1564-1583.
Journal Article
Published: 01 October 1995
Canadian Journal of Earth Sciences (1995) 32 (10): 1720-1739.
Journal Article
Journal: GSA Bulletin
Published: 01 June 1995
GSA Bulletin (1995) 107 (6): 642-664.
Journal Article
Journal: Geology
Published: 01 February 1995
Geology (1995) 23 (2): 141-144.
Journal Article
Journal: Geology
Published: 01 January 1995
Geology (1995) 23 (1): 65-68.
..., extending to nearly 30 km depth above a south-dipping basal decollement, has produced latest Cretaceous to Cenozoic antiforms, including the Doonerak antiform in the central Brooks Range and anticlinoria near the northern range front. (3) The duplexing occurs in basement rocks of the North Slope subterrane...
Journal Article
Journal: GSA Bulletin
Published: 01 November 1994
GSA Bulletin (1994) 106 (11): 1502-1511.
Journal Article
Published: 01 November 1994
Canadian Journal of Earth Sciences (1994) 31 (11): 1672-1686.
Journal Article
Journal: GSA Bulletin
Published: 01 August 1994
GSA Bulletin (1994) 106 (8): 1017-1032.
Journal Article
Journal: GSA Bulletin
Published: 01 June 1994
GSA Bulletin (1994) 106 (6): 803-823.
Journal Article
Journal: GSA Bulletin
Published: 01 July 1991
GSA Bulletin (1991) 103 (7): 861-875.
Journal Article
Published: 01 October 1990
Canadian Journal of Earth Sciences (1990) 27 (10): 1359-1370.
... formation. Bedding-parallel slip indicates a flexural slip mechanism of folding. The geometry of several large-scale anticlinoria has been interpreted as being due to formation of these structures over detachments and thrust ramps.The constant fold geometry, the parallel orientation of faults and large...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1989
AAPG Bulletin (1989) 73 (3): 276-288.
FIGURES | View All (12)
Series: GSA Special Papers
Published: 01 January 1989
DOI: 10.1130/SPE230-p115
Journal Article
Journal: Geology
Published: 01 December 1988
Geology (1988) 16 (12): 1112-1116.