The Oligo-/Miocene Qom Formation (Iran): evidence for an early Burdigalian restriction of the Tethyan Seaway and closure of its Iranian gateways-Reference-Cited by-同舟云学术

The Oligo-/Miocene Qom Formation (Iran): evidence for an early Burdigalian restriction of the Tethyan Seaway and closure of its Iranian gateways

Published:2007-11-28 Issue:3 Volume:98 Page:627-650
ISSN:1437-3254
Container-title:International Journal of Earth Sciences
language:en
Short-container-title:Int J Earth Sci (Geol Rundsch)

Author:

Reuter M.,Piller W. E.,Harzhauser M.,Mandic O.,Berning B.,Rögl F.,Kroh A.,Aubry M.-P.,Wielandt-Schuster U.,Hamedani A.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s00531-007-0269-9.pdf

Reference59 articles.

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3. Adams CG, Gentry AW, Whybrow PJ (1983) Dating the terminal Tethyan event. Utrecht Micropaleontol Bull 30:273–298

4. Ala MA (1982) Chronology of trap formation and migration of hydrocarbons in Zagros sector of southwest Iran. AAPG Bull 66:1536–1542

5. Alsharhan AS, Nairn AEM (1995) Tertiary of the Arabian Gulf: sedimentology and hydrocarbon potential. Palaeogeogr Palaeoclimatol Palaeoecol 114:369–384

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