Three-dimensional seismic characterization of a complex sediment drift in the South China Sea: Evidence for unsteady flow regime-Reference-Cited by-同舟云学术

Three-dimensional seismic characterization of a complex sediment drift in the South China Sea: Evidence for unsteady flow regime

Published:2016-11-26 Issue:3 Volume:64 Page:832-853
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Sun Qiliang¹²,Cartwright Joe³,Lüdmann Thomas⁴,Wu Shiguo⁵,Yao Genshun⁶

Affiliation:

1. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education; Faculty of Resources; China University of Geosciences; Wuhan 430074 China

2. Department of Marine Science and Engineering; Faculty of Resources; China University of Geosciences; Wuhan 430074 China

3. Department of Earth Sciences; University of Oxford; Oxford OX1 3AN UK

4. Department of Geosciences; Centre for Earth System Research and Sustainability; University of Hamburg; Bundesstrasse 55 20146 Hamburg Germany

5. Sanya Institute of Deep-sea Science and Engineering; Chinese Academy of Sciences; Sanya 572000 China

6. PetroChina Hangzhou Institute of Geology; Hangzhou 310023 China

Funder

National Scientific Foundation of China

National Basic Research Program of China

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/sed.12330/fullpdf

Reference54 articles.

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2. Depositional characteristics and processes of alongslope currents related to a seamount on the northwestern margin of the Northwest Sub-Basin, South China Sea;Chen;Mar. Geol.,2014

3. Key controls on submarine channel development in structurally active settings;Clark;Mar. Pet. Geol.,2011

4. Contour Currents and Contourite Drifts

5. Seismic features diagnostic of contourite drifts;Faugères;Mar. Geol.,1999

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