Petrography, geochemistry and genesis of dolomites in the upper Cambrian Sanshanzi Formation of the western Ordos Basin, northern China

Author:

Li Fengjie,Ma Xiaokang,Lai Xuelian

Funder

National Key Research and Development Program of China Stem Cell and Translational Research

National Key Research and Development Program of China

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference51 articles.

1. Dolomite Reservoirs: Geochemical Techniques for Evaluating Origin and Distribution (AAPG Continuing Education Course Note Series No.36);Allen,1993

2. A non-marine depositional setting for the northern Fortescue Group, Pilbara Craton, inferred from trace element geochemistry of stromatolitic carbonates;Bolhar;Precambrian Research,2007

3. Basin Evolution and Sediments Accumulation during Eopaleozoic in the Ordos continental Block;Chen;Chengdu University of Technology.,2007

4. Application of carbon and oxygen isotope to carbonate reservoirs in Northeast Sichuan Basin;Chen;Acta Sedimentologica Sinica,2011

5. Chen Z.Y., Ma Z.F., Zhang J.Q., 1998. Genesis of the dolomite in M5 subinterval Ordovician in the central Ordos Basin. Petroleum Exploration and Development 1998, 25(6): 20-22.

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