Formation of intracontinental basins in the opposite corners of the Tabas block as coeval structures controlled by transpressional faulting, Iran-Reference-Cited by-同舟云学术

Formation of intracontinental basins in the opposite corners of the Tabas block as coeval structures controlled by transpressional faulting, Iran

Published:2016-05-11 Issue:11-12 Volume:128 Page:1593-1617
ISSN:0016-7606
Container-title:Geological Society of America Bulletin
language:en
Short-container-title:Geological Society of America Bulletin

Author:

Konon Andrzej,Nadimi Alireza,Koprianiuk Marek,Wysocka Anna,Szaniawski Rafał,Wyglądała Michał,Słaby Ewa,Beygi Soheyla,Barski Marcin

Publisher

Geological Society of America

Subject

Geology

Reference130 articles.

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3. Aghanabati, A. , and Haghipour, A. , 1975, Geological Quadrangle Map of Tabas, Sheet No. 1: Tehran, Geological Survey of Iran, scale 1:250,000.

4. Aghanabati, A. , Ruttner, A. , Nabavi, M.H. , and Hajian, J. , 1994a, Geological Map of Shirgesht: Tehran, Geological Survey of Iran, scale 1:100,000.

5. Aghanabati, A. , Ruttner, A. Nabavi, M.H. , Hajaian, J. , and Alavi Naini, M. , 1994b, Geological Map of Eshskabad: Tehran, Geological Survey of Iran, scale 1:100,000.

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