2017, 36(1) 174-181 DOI:   10.3969/j.issn.1004-5589.2017.01.015  ISSN: 1004-5589 CN: 22-1111/P

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Keywords
stratigraphic-structural framework
lithofacies distribution
favorable exploration play
Yushu Fault Depression
Songliao Basin
Authors
PubMed

Lithofacies distribution and prediction of favorable exploration play of Lower Cretacous in Yushu Fault Depression, eastern Songliao Basin

REN Yan-ning1, CUI Tong2, LIU Yang3, ZHU Ying1, ZHANG Hang1

1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. International Center for Geoscience Research and Education in Northeast Asia, Jilin University, Changchun 130026, China;
3. Exploration and Development Research Institute, Jilin Oil Field Company, PetroChina, Songyuan 138000, Jilin, China

Abstract��

Integrating drilling, well-logging and seismic data, in this study, we established the stratigraphic-structural framework, restored the lithofacies distribution of main stratigraphic units, analyzed the source-reservoir-trap assemblage and predicted favorable exploration play in Yushu Fault Depression. The results showed that the Yushu Fault Depression consists of Yudong and Yuxi sub-depressions, of which both are half-grabens controlled by the echelon fault combination. The two sub-depressions are separated by the Yushu uplift in the middle and mirrored each other. The depressions are mainly composed of lacustrine-fan delta-nearshore subaqueous fan systems, with large scale volcanic explosive and effusive facies occurred in Huoshiling Formation. This forms self-sourcing and self-reservoiring, lower-sourcing and upper-reservoiring, upper-sourcing and lower-reservoiring assemblages. The volcanic domes belt of central uplift adjacent to the source rocks in the Yudong sub-depression is the favorable exploration play in the study area.

Keywords�� stratigraphic-structural framework   lithofacies distribution   favorable exploration play   Yushu Fault Depression   Songliao Basin  
Received 2016-03-05 Revised 2016-09-11 Online:  
DOI: 10.3969/j.issn.1004-5589.2017.01.015
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