Late Quaternary reorientation of stress field and extension direction in the southern Gulf of Suez, Egypt: Evidence from uplifted coral terraces, mesoscopic fault arrays, and borehole breakouts-Reference-Cited by-同舟云学术

Late Quaternary reorientation of stress field and extension direction in the southern Gulf of Suez, Egypt: Evidence from uplifted coral terraces, mesoscopic fault arrays, and borehole breakouts

Published:1996-08 Issue:4 Volume:15 Page:791-802
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Bosworth William,Taviani Marco

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://www.agu.org/journals/tc/v015/i004/95TC03851/95TC03851.pdf

Reference72 articles.

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2. Quartore Strandterrassen an der Küste des Gebel Zeit (Golf von Suez/jgypten);Andres;Erdkunde,1988

3. Tectonic analysis of fault slip data sets;Angelier;J. Geophys. Res.,1984

4. Extension and rifting: The Zeit region, Gulf of Suez;Angelier;J. Struct. Geol.,1985

5. U-Th ages obtained by mass spectrometry in corals from Barbados: Sea-level during the past 130,000 years;Bard;Nature,1990

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