A fossil carbonate contourite drift on the Lower Ordovician palaeocontinental margin of the middle Yangtze Terrane, Jiuxi, northern Hunan, southern China-Reference-Cited by-同舟云学术

A fossil carbonate contourite drift on the Lower Ordovician palaeocontinental margin of the middle Yangtze Terrane, Jiuxi, northern Hunan, southern China

Published:1993-01 Issue:1-4 Volume:82 Page:271-284
ISSN:0037-0738
Container-title:Sedimentary Geology
language:en
Short-container-title:Sedimentary Geology

Author:

Duan Taizhong,Gao Zhenzhong,Zeng Yunfu,Stow Dorrik

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference19 articles.

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2. Analysis of tectonic evolution of paleocontinental margins in South China based on sedimentary history;Duan;Oil Gas Geol.,1988

3. Contourite drift molded by deep Mediterranean outflow;Faugères;Geology,1984

4. Submersible studies of deep-sea furrows and transverse ripples in cohesive sediments;Flood;Mar. Geol.,1980

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