Journal article

Structural geometry, style and timing of deformation in the Hawasina window, Al Jabal al Akhdar and Saih Hatat culminations, Oman mountains

Abstract:: The Al Jabal al Akhdar and Saih Hatat culminations in the central Oman Mountains expose the complete mid-Permian to Late Cretaceous (Cenomanian) passive shelf and margin carbonate sequence beneath the allochtonous slope (Sumeini Group), basin (Hawasina complex), distal ocean-trench (Haybi complex) facies rocks, and the Semail ophiolite thrust sheets that were emplaced from NE to SW during the Late Cretaceous. Reconstruction of the pre-thrust sequences shows that time-equivalent rocks occur in...
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Publication status:: Published

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APA Style

Searle, M. (2007). Structural geometry, style and timing of deformation in the Hawasina window, Al Jabal al Akhdar and Saih Hatat culminations, Oman mountains. GEOARABIA, 12(2), 99–130.

MLA Style

Searle, M. “Structural Geometry, Style and Timing of Deformation in the Hawasina Window, Al Jabal Al Akhdar and Saih Hatat Culminations, Oman Mountains.” GEOARABIA, vol. 12, no. 2, 2007, pp. 99–130.

Chicago Style

Searle, M. 2007. “Structural Geometry, Style and Timing of Deformation in the Hawasina Window, Al Jabal Al Akhdar and Saih Hatat Culminations, Oman Mountains.” GEOARABIA 12 (2): 99–130.
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+ Searle, M More by this author

Institution:: University of Oxford
Division:: MPLS
Department:: Earth Sciences
Role:: Author

Journal:: GEOARABIA More from this journal
Volume:: 12
Issue:: 2
Pages:: 99-130
Publication date:: 2007-01-01
ISSN:: 1025-6059

Language:: English
Pubs id:: pubs:83385
UUID:: uuid:0e6ad91c-dcbd-4ca9-9eee-1567f925366f
Local pid:: pubs:83385
Source identifiers:: 83385
Deposit date:: 2012-12-19
ARK identifier:: ark:/29072/ora_0e6ad91cdcbd4ca99eee1567f925366f

Terms of use

Copyright date:: 2007

Licence:: Terms and Conditions of Use for Oxford University Research Archive

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