Structurally-controlled hydrothermal fluid flow in an extensional tectonic regime: A case study of Cretaceous Qamchuqa Formation, Zagros Basin, Kurdistan Iraq-Reference-Cited by-同舟云学术

Structurally-controlled hydrothermal fluid flow in an extensional tectonic regime: A case study of Cretaceous Qamchuqa Formation, Zagros Basin, Kurdistan Iraq

Published:2019-05 Issue: Volume:386 Page:52-78
ISSN:0037-0738
Container-title:Sedimentary Geology
language:en
Short-container-title:Sedimentary Geology

Author:

Kareem Kareem H.,Al-Aasm Ihsan S.,Mansurbeg Howri

Funder

Ministry of Higher Education and Scientific Research

Natural Sciences and Engineering Research Council of Canada

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference105 articles.

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3. The effect of hydrothermal fluid flow on early diagenetic dolomitization: an example from the Devonian Slave Point Formation, northwest Alberta, Canada;Al-Aasm,2004

4. Dolomitization and related fluid evolution in the Oligocene-Miocene Asmari Formation, Gachsaran area, SW Iran: petrographic and isotopic evidence;Al-Aasm;J. Pet. Geol.,2009

5. Multiple fluid flow events and the formation of saddle dolomite: case studies from the middle Devonian of the Western Canada sedimentary Basin;Al-Aasm;Mar. Pet. Geol.,2002

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