Thermochronometric evidence for diffuse extension and two-phase rifting within the Central Arabian Margin of the Red Sea Rift-Reference-Cited by-同舟云学术

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Thermochronometric evidence for diffuse extension and two-phase rifting within the Central Arabian Margin of the Red Sea Rift

Published:2016-12 Issue:12 Volume:35 Page:2863-2895
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Szymanski E.¹²^ORCID,Stockli D. F.¹³^ORCID,Johnson P. R.⁴^ORCID,Hager C.¹⁵

Affiliation:

1. Department of Geology; University of Kansas; Lawrence Kansas USA

2. Earth Science Department; Chevron Energy Technology Company; Houston Texas USA

3. Department of Geological Sciences; University of Texas at Austin; Austin Texas USA

4. 6016 SW Haines Street; Portland OR 97219 USA

5. Chevron U.S.A. Inc.; Bakersfield CA USA

Funder

Iran National Science Foundation

The Geological Society of America

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016TC004336/fullpdf

Reference166 articles.

1. Morphostructural development of the Eritrean rift flank (southern Red Sea) inferred from apatite fission track analysis;Abbate;J. Geophys. Res.,2002

2. The Najd fault system revisited: A two-way strike-slip orogen in the Saudi Arabian Shield;Agar;J. Struct. Geol.,1987

3. A new look at the Middle to Lower Cretaceous stratigraphy, offshore Kuwait;Al-Fares;GeoArabia,1998

4. Am. Assoc. Pet. Geol. Mem.;Al-Laboun,1986

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