The tectonic evolution of a Neo-Tethyan (Eocene-Oligocene) island-arc (Walash and Naopurdan groups) in the Kurdistan region of the Northeast Iraqi Zagros Suture Zone-Reference-Cited by-同舟云学术

The tectonic evolution of a Neo-Tethyan (Eocene-Oligocene) island-arc (Walash and Naopurdan groups) in the Kurdistan region of the Northeast Iraqi Zagros Suture Zone

Published:2012-12-07 Issue:1 Volume:22 Page:104-125
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

Ali Sarmad A.¹²,Buckman Solomon¹,Aswad Khalid J.³,Jones Brian G.¹,Ismail Sabah A.²,Nutman Allen P.¹

Affiliation:

1. School of Earth and Environmental Sciences; University of Wollongong; Wollongong New South Wales Australia

2. Department of Applied Geology; College of Science; Kirkuk University; Kirkuk Iraq

3. Department of Geology; College of Science; Mosul University; Mosul Iraq

Publisher

Wiley

Subject

Geology

Reference62 articles.

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2. Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolution;Alavi;American Journal of Science,2004

3. Microfacies and age determination of the sedimentary sequences within Walash volcanosedimentary series, Mawat nappes, NE Iraq;Al-Banna;Tikrit Journal of Pure Science,2008

4. Ali S. A. 2012 Geochemistry of Tethyan-arc related volcanic rocks. NE Iraq

5. Recognition of Late Cretaceous Hasanbag ophiolite-arc rocks in the Kurdistan region of the Iraqi Zagros Thrust Zone: A missing link in the paleogeography of the closing Neo-Tethys Ocean;Ali;Lithosphere,2012

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