Facies distribution in the Ordovician Pingliang Formation (southern Ordos Basin, China) and the role of turbidity currents

Author:

He Youbin,van Loon A.J. (Tom),Li Hua

Publisher

Elsevier

Reference26 articles.

1. The cretaceous Talme Yafe formation: a contour current shaped sedimentary prism of calcareous detritus at the continental margin of the Arabian craton;Bein;Sedimentology,1976

2. Characteristics and formational mechanism of the sediment gravity flow of the Tangwang Ling Formation of Shaanxi;Chen;Exp. Petrol. Geol.,1984

3. A fossil carbonate contourite drift on the lower Ordovician palaeocontinental margin of the middle Yangtze Terrane, Jiuxi, northern Hunan, southern China;Duan;Sediment. Geol.,1993

4. Deep-Water Traction Current Deposits—the Study of Internal-Tide, Internal-Wave, and Contour Current Deposits;Gao,1996

5. Middle Miocene reworked turbidites in the Baiyun Sag of the Pearl River Mouth Basin, northern South China Sea margin: processes, genesis, and implications;Gong;J. Asian Earth Sci.,2016

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