Late Ordovician, deep-water gravity-flow deposits, palaeogeography and tectonic setting, Tarim Basin, Northwest China

Author:

Lin C.1,Liu J.2,Eriksson K.3,Yang H.4,Cai Z.4,Li H.2,Yang Z.3,Rui Z.2

Affiliation:

1. School of Ocean Sciences and Resources; China University of Geosciences; Beijing China

2. School of Energy and Resources; China University of Geosciences; Beijing China

3. Department of Geosciences; Virginia Tech; Blacksburg VA USA

4. Petroleum Exploration & Production Institute; PetroChina Company Limited; Beijing China

Publisher

Wiley

Subject

Geology

Reference85 articles.

1. Isotope and trace element evolution: responding to sea level fluctuation - an example of Ordovician in middle Tarim Basin;Bao;Acta Sedimentol. Sinica,1998

2. Walled sedimentary basins of China;Carroll;Basin Res.,2010

3. Palaeozoic tectonic evolution of the Tianshan belt, NW China;Charvent;Sci. China,2011

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