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Journal Article

Are Neoproterozoic glacial deposits preserved on the margins of Laurentia related to the fragmentation of two supercontinents?: Comment and Reply Available to Purchase

C. McA. Powell, Grant M. Young
Published: 01 November 1995
Geology (1995) 23 (11): 1053–1055.
DOI: https://doi.org/10.1130/0091-7613(1995)023<1053:ANGDPO>2.3.CO;2
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Journal Article

Platform-margin collapse during Famennian reef evolution, Canning Basin, Western Australia Available to Purchase

Annette D. George, Phillip E. Playford, C. McA. Powell
Published: 01 August 1995
Geology (1995) 23 (8): 691–694.
DOI: https://doi.org/10.1130/0091-7613(1995)023<0691:PMCDFR>2.3.CO;2
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Journal Article

Paleomagnetic constraints on timing of the Neoproterozoic breakup of Rodinia and the Cambrian formation of Gondwana Available to Purchase

C. McA. Powell, Z. X. Li, M. W. McElhinny, J. G. Meert, J. K. Park
Published: 01 October 1993
Geology (1993) 21 (10): 889–892.
DOI: https://doi.org/10.1130/0091-7613(1993)021<0889:PCOTOT>2.3.CO;2
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Journal Article

Curvature of the Himalayan arc related to Miocene normal faults in southern Tibet Available to Purchase

C. McA. Powell
Published: 01 April 1986
Geology (1986) 14 (4): 358–359.
DOI: https://doi.org/10.1130/0091-7613(1986)14<358:COTHAR>2.0.CO;2
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Journal Article

Slaty cleavage and the dewatering hypothesis: An examination of some critical evidence: Comments and reply: COMMENT Available to Purchase

C. McA. Powell
Published: 01 December 1976
Geology (1976) 4 (12): 792.
DOI: https://doi.org/10.1130/0091-7613(1976)4<792a:SCATDH>2.0.CO;2
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Journal Article

Tectonic models of the Tibetan plateau: Comment and reply: REPLY Available to Purchase

C. McA. Powell, P. J. Conaghan
Published: 01 July 1976
Geology (1976) 4 (7): 390.
DOI: https://doi.org/10.1130/0091-7613(1976)4<390b:TMOTTP>2.0.CO;2
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Journal Article

Tectonic models of the Tibetan plateau Available to Purchase

C. McA. Powell, P. J. Conaghan
Published: 01 December 1975
Geology (1975) 3 (12): 727–731.
DOI: https://doi.org/10.1130/0091-7613(1975)3<727:TMOTTP>2.0.CO;2
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