Southeast slope belt sequence stratigraphy and sedimentary facies of pear rift

DOI

10.2991/isci-15.2015.308How to use a DOI?

Keywords

pear faulted southeast slope belt; stratigraphic division; sedimentary facies.

Abstract

Application of sequence stratigraphy theory, utilization of core, log and seismic data, divided the southeast slope with pear rift sequence stratigraphy. The pear rift southeast slope zone is divided into five one sequence (Quantou, Denglouku, Yingcheng, Shahezi, Huoshiling), 10 two sequences (four springs, Quan three sections, K1q2, spring period, Denglouku, four camp, camp three sections, Sec Sha, Sha, Huoshiling), on the basis of sequence stratigraphic units above division and comparison of sedimentary facies and sequence stratigraphy of sedimentary facies within the law were studied to identify the main types of sedimentary facies in the study area include lacustrine, fan delta and braided river delta, meandering river with the conclusions of fan delta underwater distributary channel analysis and the oil-rich delta braided river sand body type most favorable to.

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  - Shuangting Guo
AU  - Hongqi Yuan
PY  - 2015/01
DA  - 2015/01
TI  - Southeast slope belt sequence stratigraphy and sedimentary facies of pear rift
BT  - Proceedings of the 2015 International Symposium on Computers & Informatics
PB  - Atlantis Press
SP  - 2369
EP  - 2376
SN  - 2352-538X
UR  - https://doi.org/10.2991/isci-15.2015.308
DO  - 10.2991/isci-15.2015.308
ID  - Guo2015/01
ER  -