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The characteristics of Triassic detrital components and provenance analysis in the western Tabei Uplift

机译:Tabei隆起中三叠纪滴乳成分及源分析的特点

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Triassic in the western Tabei uplift is detrital sedimentary. Based on the data of the conglomerate, sandstone framework components and heavy mineral to analyze the Triassic of research area, the result shows that the source rocks are metamorphic rocks, magmatic rocks and sedimentary rocks, whose sources come from Xiqiu Uplift and Luntai Uplift. The western of research area is magmatic and sedimentary rock deposit zone, where is mainly influenced by the Xiqiu Uplift. The middle part of research area is metamorphic and sedimentary rock deposit zone where is mainly influenced by the Xiqiu Uplift and Luntai Uplift. The eastern of research area is metamorphic, sedimentary and magmatic rock deposit zone where is mainly influenced by the Luntai Uplift. The proximal clastic deposits are mainly influenced by the hydrodynamic conditions, palaeohigh and tectonization, so provenance has the characteristics of region and multiple evolutions.
机译:The Western Tabei Uplift中的三叠纪是脱脂沉积物。 基于集团的数据,砂岩框架组件和重型矿物分析研究区域的三叠岩,结果表明,源岩石是变质岩石,岩浆岩石和沉积岩,其来源来自西丘隆起和龙台隆起。 研究领域的西方是岩浆和沉积岩沉积区,主要受到Xiqiu隆起的影响。 研究领域的中间部分是变质和沉积岩沉积区,主要受到西秋隆起和龙台隆起的影响。 研究领域的东部是变质,沉积和岩浆岩沉积区,主要受到拉伊隆起的影响。 近端碎屑沉积物主要受水动力学条件,帕拉西和构造化的影响,因此物质具有区域的特征和多种进化。

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