Strain Field Associated With a Component of Divergent Motion Along the Southern Dead Sea Fault: Insights From Magnetic Fabrics-Reference-Cited by-同舟云学术

Strain Field Associated With a Component of Divergent Motion Along the Southern Dead Sea Fault: Insights From Magnetic Fabrics

Published:2019-01 Issue:1 Volume:38 Page:335-353
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Issachar R.¹²^ORCID,Levi T.²^ORCID,Marco S.¹^ORCID,Weinberger R.²³^ORCID

Affiliation:

1. Department of Geophysics; Tel Aviv University; Tel Aviv Israel

2. Geological Survey of Israel; Jerusalem Israel

3. Department of Geological and Environmental Sciences, Ben-Gurion University of the Negev; Beer-Sheva Israel

Funder

Israel Science Foundation

NSF Instruments and Facilities program and by the University of Minnesota

Israel Science Foundation Center of Excellence

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018TC005168/fullpdf

Reference103 articles.

1. Magnetic anisotropy reveals Neogene tectonic overprint in highly strained carbonate mylonites from the Morcles nappe, Switzerland;Almqvist;Journal of Structural Geology,2011

2. GPS measurements of near-field deformation along the southern Dead Sea Fault System;Al-Tarazi;Geochemistry, Geophysics, Geosystems,2011

3. Avni , Y. 1997 Geological evolution of the central and southern Negev as an indicator of the evolution of the Dead Sea transform western margin in the late Neogene and Quaternary

4. Evolution of the Paran drainage basin and its relation to the Plio-Pleistocene history of the Arava Rift western margin, Israel;Avni;Israel Journal of Earth Sciences,2000

5. The Arava Formation-A Pliocene sequence in the Arava Valley and its western margin, southern Israel;Avni;Israel Journal of Earth Sciences,2001

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