Reconstructing the level of the central Red Sea evaporites at the end of the Miocene-Reference-Cited by-同舟云学术

Reconstructing the level of the central Red Sea evaporites at the end of the Miocene

Published:2020-10-02 Issue:2 Volume:33 Page:1266-1292
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Res

Author:

Mitchell Neil C.¹^ORCID,Shi Wen²,Izzeldin A.Y.³,Stewart Ian C. F.⁴

Affiliation:

1. Department of Earth and Environmental Sciences University of Manchester Manchester UK

2. 研究人员 ‐ Institute of GeophysicsChina Earthquake Administration Beijing China

3. Awasconrc Khartoum Sudan

4. Stewart Geophysical Consultants Pty. Ltd Adelaide SA Australia

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12513

Reference180 articles.

1. Afifi A. M. Tapponnier P. &Raterman N. S.(2014).The Messinian Unconformity in the Red Sea: Evidence for Widespread Dessication?AAPG Search and Discovery Article #90188 11th Middle East Geosciences Conference and Exhibition 10‐12 March 2014 Manama Bahrain.

2. Crustal structure of the Arabian plate: new constraints from the analysis of teleseismic receiver functions

3. Volcanic activity in the Red Sea axial trough — evidence for a large mantle diapir?

4. Hydrographic changes during 20 years in the brine-filled basins of the Red Sea

5. Climatic, eustatic, and tectonic controls on quaternary deposits and landforms, Red Sea coast, Egypt;Arvidson R.;Journal of Geophysical Research,1994

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