Jabal Hafit anticline (UAE and Oman) formed by décollement folding followed by trishear fault-propagation folding

Author:

Hansman Reuben J.ORCID,Ring Uwe

Funder

Royal Swedish Academy of Sciences

Bolin Centre for Climate Research Area 6

Stiftelsen Anna-Greta och Holger Crafoords fond

Stockholm University

Publisher

Elsevier BV

Subject

Geology

Reference67 articles.

1. Biostratigraphy (Turboratalia cunialensis/Cribrohantkenina inflata concurrent-range zone, P16) of the late Eocene Dammam Formation, west of the northern Oman mountains;Abdelghany;Micropaleontology,2002

2. Subsidence history, gravity anomalies and flexure of the United Arab Emirates (UAE) foreland basin;Ali;GeoArabia,2009

3. Geophysical investigation of Al Jaww Plain, eastern Abu Dhabi: implications for structure and evolution of the frontal fold belts of the Oman Mountains;Ali;GeoArabia,2008

4. Integrated gravity and seismic investigation over the Jabal Hafit structure: implications for basement configuration of the frontal fold-and-thrust belt of the Northern Oman Mountains;Ali;J. Petrol. Geol.,2009

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