Complex fault-fold interactions during the growth of the Jabal Qusaybah anticline at the western tip of the Salakh Arch, Oman-Reference-Cited by-同舟云学术

Complex fault-fold interactions during the growth of the Jabal Qusaybah anticline at the western tip of the Salakh Arch, Oman

Author:

Storti F.¹,Balsamo F.¹,Clemenzi L.¹,Mozafari M.²,Al-Kindy M. H. N.³,Solum J.⁴,Swennen R.²,Taberner C.⁴,Tueckmantel C.⁴

Affiliation:

1. Natural and Experimental Tectonics Research Group, Department of Physics and Earth Sciences “Macedonio Melloni”; University of Parma; Parma Italy

2. Department of Earth and Environmental Sciences; KU Leuven; Leuven Belgium

3. Petroleum Development of Oman; Muscat Sultanate of Oman

4. Shell Global Solutions International B. V.; Rijswijk Netherlands

Funder

Shell Global Solutions

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference73 articles.

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

4. Al-Kindi , M. H. 2006 Structural evolution and fracture pattern of Salakh Arch

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