Upper Miocene–Pliocene provenance evolution of the Central Canyon in northwestern South China Sea-Reference-Cited by-同舟云学术

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Upper Miocene–Pliocene provenance evolution of the Central Canyon in northwestern South China Sea

Published:2018-06-05 Issue:2 Volume:40 Page:223-235
ISSN:0025-3235
Container-title:Marine Geophysical Research
language:en
Short-container-title:Mar Geophys Res

Author:

Cui Yuchi,Shao Lei^ORCID,Qiao Peijun,Pei Jianxiang,Zhang Daojun,Tran Huyen

Funder

National Natural Science Foundation of China

National Science and Technology Major Project

Fundamental Research Funds for the Central Universities

State Key Laboratory of Marine Geology, Tongji University

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Oceanography

Link

http://link.springer.com/content/pdf/10.1007/s11001-018-9359-2.pdf

Reference74 articles.

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2. Antobreh AA, Krastel S (2006) Morphology, seismic characteristics and development of Cap Timiris Canyon, offshore Mauritania: a newly discovered canyon preserved-off a major arid climatic region. Mar Pet Geol 23:37–59

3. Arzola RG, Wynn RB, Lastras G, Masson DG, Weaver PPE (2008) Sedimentary features and processes in the Nazaré and Setúbal submarine canyons, west Iberian margin. Mar Geol 250:64–88

4. Bayliss N, Pickering KT (2015) Transition from deep-marine lower-slope erosional channels to proximal basin-floor stacked channel–levée–overbank deposits, and syn-sedimentary growth structures, middle eocene banastón system, Ainsa Basin, Spanish Pyrenees. Earth Sci Rev 144:23–46

5. Boynton WV (1984) Cosmochemistry of the rare earth elements; meteorite studies. Elsevier Science Publication Cooporation, Amsterdam

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