Sedimentary facies and its control over petroleum and other resources of the Upper Triassic Bagong Formation in Baqing area, southeastern Qiangtang Basin
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摘要:
羌塘盆地是青藏高原上最大的中生代海相沉积盆地，富含烃源岩和蒸发岩，也是中国油气勘探重要的场所之一。巴青地区的上三叠统巴贡组沉积相研究不仅能为特提斯洋的演化提供佐证，而且为羌塘盆地油气和钾盐资源勘探提供理论依据和实践指导。本文对巴青地区上三叠统巴贡组的古生物、沉积构造、岩石组合分析，结果表明：研究区主要发育障壁岛沉积体系下的潟湖相、潮坪相、三角洲相沉积相以及10种亚相。晚三叠世巴贡期，研究区是一个由北（巴青—索县）向南（班—怒缝合带）变深的伸展背景下的陆缘海沉积环境。
Abstract:The Qiangtang Basin is the largest Mesozoic marine sedimentary basin on the Tibetan Plateau. It is rich in source rocks and evaporites, and has become one of the most important places for petroleum exploration in China. The study of sedimentary facies of the Upper Triassic Bagong Formation in Tumen-Baqing area can not only provide evidence for the evolution of the Tethyan Ocean but also provide theoretical basis and practical guidance for the exploration of hydrocarbon and potassium resources in the Qiangtang Basin. An analysis of petrological characteristics, paleontology and sedimentary structures shows that the lagoon facies, tidal flat facies, delta facies and ten kinds of sub-facies are mainly developed in the study area. During the Bagong period of the Late Triassic, the study area was in a continental margin sea sedimentary environment under the extensional background from the north (Baqing-Suoxian) to the south (Ban-Nu suture zone).
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表 1 巴青及邻区上三叠统岩石地层划分对比
Table 1. Lithostratigraphic division and correlation of the Upper Triassic strata in Baqing area
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