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    Chengdu Institute of Geology and Mineral Resources. 1:250 000 Tug, Jangngaidarina, Heihuling and Dogai Coring Sheets in Xizang[J]. Sedimentary Geology and Tethyan Geology, 2005, 25(1-2): 34-38.
    Citation: Chengdu Institute of Geology and Mineral Resources. 1:250 000 Tug, Jangngaidarina, Heihuling and Dogai Coring Sheets in Xizang[J]. Sedimentary Geology and Tethyan Geology, 2005, 25(1-2): 34-38.

    1:250 000 Tug, Jangngaidarina, Heihuling and Dogai Coring Sheets in Xizang

    • The flyschoid-dominated deep-water sediments especially the "glaciofluvial diamictites" are found to be overlain by the formerly Lugu Formation limestones and volcanic horizons. The pre-Devonian "Gomori Group" shallow metamorphic rock series are mostly redelineated as the Permian strata. A well-exposed Triassic stratigraphic section is constructed. Three formation-scale lithostratigraphic units are established in southern Qiangtang. Tectonically, the "Central Uplift" is interpreted as part of the Lungmuco-Shuanghu tectonic zone. The Shuanghu tectonic mélange zone is separated both at the northern and southern boundaries by giant ductile shear zones. The island-arc volcanic rocks are observed in the Upper Triassic Rola Kangri Group. The important advance has been made for the examination of the NS-trending neotectonics. Abundant larger asphalt veins, heavy oil shows and oil shows are identified in the surveyed areas.
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