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    ZHOU Ken-ken, YIN Hai-sheng, LIN Jin-hui. Petrology and sedimentary environments of the lacustrine carbonate rocks from the Miocene Wudaoliang Group in the Hoh Xil Basin, Qinghai[J]. Sedimentary Geology and Tethyan Geology, 2007, 27(1): 25-31.
    Citation: ZHOU Ken-ken, YIN Hai-sheng, LIN Jin-hui. Petrology and sedimentary environments of the lacustrine carbonate rocks from the Miocene Wudaoliang Group in the Hoh Xil Basin, Qinghai[J]. Sedimentary Geology and Tethyan Geology, 2007, 27(1): 25-31.
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    Petrology and sedimentary environments of the lacustrine carbonate rocks from the Miocene Wudaoliang Group in the Hoh Xil Basin, Qinghai

    • Research Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China

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    • Received Date: July 02, 2006
    • Revised Date: September 24, 2006
    • Published Date: March 29, 2007
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    • The lacustrine carbonate rocks occur on a wide range of scales in the Palaogene and Neogene strata in the Hoh Xil Basin, Qinghai, and constitute an important part of the Miocene Wudaoliang Group sediments.The lacustrine carbonate rocks in the Wudaoliang Group consist of boundstone (stromatolite), micritic limestone, grainstone and micritic dolostone which were laid down in the shallow-water to bathyal, high-salinity and enclosed to semi-enclosed lak e systems.
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