Types of Sedimentary Facies of Palace Area in Songliao Basin

DOI

10.2991/isci-15.2015.307How to use a DOI?

Keywords

Songliao Basin; palace rift; sedimentary facies

Abstract

The palace is located in the Songliao Basin, southeast regional uplift Palace rift, Denglouku off during the deposition of Au transition period for the basin, with more than provenance, short distance transport, Tianpingbuqi characteristics, Quantou deposition during the period of depression basin, with settlement rate, stable sedimentary environment and so on. According to the results of previous research and heavy mineral analysis to determine the palace area Denglouku - Quantou northeast direction during the deposition source and southern elm Dehui subject matter - Fulongquan provenance affects two provenances, braided river Delta - meandering river depositional environment. Total identify four kinds of sedimentary facies, seven kinds subfacies and 14 types of sedimentary microfacies.

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  - Jiaqi Zou
AU  - Wenguang Wang
AU  - Chengzhi Liu
PY  - 2015/01
DA  - 2015/01
TI  - Types of Sedimentary Facies of Palace Area in Songliao Basin
BT  - Proceedings of the 2015 International Symposium on Computers & Informatics
PB  - Atlantis Press
SP  - 2361
EP  - 2368
SN  - 2352-538X
UR  - https://doi.org/10.2991/isci-15.2015.307
DO  - 10.2991/isci-15.2015.307
ID  - Zou2015/01
ER  -