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《Science & Technology Vision》 2014-11
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Sedimentary Environment Analysis for Sha Mu Luo Formation of Upper-Jurassic to Lower- Cretaceous,Eastern Gaize,Tibet

The research area is in Gaize, located in the hinterland of Qinghai-Tibet Plateau. The location in geotectonic belongs to combination belt of Bangong lake- Nu river-Changning-Menglian, including residual arc basin of south Qiangtang. North Qiangtang-Tian shui sea plate in north and Gangdese plate in south. This paper concentrate on the Shamuluo formation of Jurassic- Early Cretaceous in Gaize, in the hinterland of QinghaiTibet Plateau. On the basis of field reconnaissance and measured profile, by differenciating contrast of layers and sedimentary facies analysis, we have built the order of basin filling, then discuss the mechanism of basin controlling and geotectonic background. With research, the Shamuluo formation's time is fixed between later Jurassic and early Cretaceous. Shamuluo formation contains continental shelf face with complex sediments and continental slope face. We propose that the ocean of Bangonghu-Nu river is residual basin of ancient ocean.
【Fund】: 西藏改则东四幅1:5万(I45E021002 I45E021003 I45E021004 I45E022002)区域地质调查项目
【CateGory Index】: P534.5
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