The characteristics of Triassic detrital components and provenance analysis in the western Tabei Uplift
- https://doi.org/10.2991/icemct-15.2015.370How to use a DOI?
- detrital component characteristics, provenance analysis, Triassic.
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 evolution.
- © 2015, the Authors. Published by Atlantis Press.
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Cite this article
TY - CONF AU - Yanqiang Chi AU - Jingyan Liu AU - Xiaoni Wang AU - Jun Jiang AU - Guifen Xu PY - 2015/06 DA - 2015/06 TI - The characteristics of Triassic detrital components and provenance analysis in the western Tabei Uplift BT - Proceedings of the 2015 International Conference on Education, Management and Computing Technology PB - Atlantis Press SP - 1768 EP - 1774 SN - 2352-5398 UR - https://doi.org/10.2991/icemct-15.2015.370 DO - https://doi.org/10.2991/icemct-15.2015.370 ID - Chi2015/06 ER -