Depositional feature of sandy conglomerate in Tuo128 block, Shengtuo area

DOI

10.2991/iceep-17.2017.62How to use a DOI?

Keywords

Shengtuo area, sandy conglomerate, prograded-type fan delta, sedimentary types.

Abstract

Sandy conglomerate is the major sedimentary systems in the upper fourth member of Shahejie formation in Shengtuo area. In this paper, on the base of core observation and description, sedimentary characteristics are studied in the upper fourth member of Shahejie formationin Shengtuo area. The results show that the prograded-type fan delta is the major sedimentary system in Shengtuo area. There are two major sedimentary types: traction current deposits which is the most strikingly signified by Parallel bedding sandstone containing gravel, and debris flow deposits which is the most strikingly signified bymassive bedding sandy conglomerate.

Copyright

© 2017, 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  - Cunlei Li
AU  - Jianmei Liu
AU  - Peng Gao
AU  - Panpan Chen
PY  - 2017/06
DA  - 2017/06
TI  - Depositional feature of sandy conglomerate in Tuo128 block, Shengtuo area
BT  - Proceedings of the 2017 6th International Conference on Energy and Environmental Protection (ICEEP 2017)
PB  - Atlantis Press
SP  - 351
EP  - 355
SN  - 2352-5401
UR  - https://doi.org/10.2991/iceep-17.2017.62
DO  - 10.2991/iceep-17.2017.62
ID  - Li2017/06
ER  -