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

DOI

10.2991/icemct-15.2015.370How to use a DOI?

Keywords

detrital component characteristics, provenance analysis, Triassic.

Abstract

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.

Copyright

© 2015, the Authors. Published by Atlantis Press.

Open Access

This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

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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  - 10.2991/icemct-15.2015.370
ID  - Chi2015/06
ER  -