北塘凹陷古近系沙河街组三段物源体系分析

黄传炎; 王华; 周立宏; 任培罡; 刘军; 白云风

Volume 34 Issue 6

Jun. 2009

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Article Navigation > Earth Science > 2009 > 34(6): 975-984

HUANG Chuan-yan, WANG Hua, ZHOU Li-hong, REN Pei-gang, LIU Jun, BAI Yun-feng, 2009. Provenance System Characters of the Third Member of Shahejie Formation in the Paleogene in Beitang Sag. Earth Science, 34(6): 975-984.

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Provenance System Characters of the Third Member of Shahejie Formation in the Paleogene in Beitang Sag

HUANG Chuan-yan^{1, 2
,},
WANG Hua^{1, 2},
ZHOU Li-hong³,
REN Pei-gang^{1, 2},
LIU Jun^{1, 2},
BAI Yun-feng^{1, 2}

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
Research Institute of Exploration and Development, PetroChina Dagang Oilfield Company, Tianjin 300280, China

Received Date: 2008-12-15
Publish Date: 2009-11-25

Abstract

Abstract

Provenance analysis is an important aspect of basin analysis. Beitang sag is an important breakthrough zone for future exploration in Dagang oilfield with its wide range of lake, deep sediment thickness, and low level of exploration of the third member of Shahejie Formation (Es₃). Detailed depiction of the provenance system using of Es₃ is of practical significance for reconstructing depositional system and forecasting favorable areas. This paper analyzes in detail the provenance system of Es₃ in Beitang sag from various angles and levels: the source area and the deposition area is macroscopically distinguished according to tectonic framework and palaeogeomorphology; the source block is determined according to the characteristics of detrital mineral assemblage; the direction of transporting clastic fragmen in the basin is described according to seismic reflection characteristics; and the source branches are finely pictured according to sandstone thickness distribution map and percent distribution map The research results show that provenances originated from Yanshan fold belt and Cangxian uplift. They are divided into western Cangxian source, north-west Hangu source, north Dashentang source and north-east Jiannan source. In the tectonic framework and the provenance system, there mainly developed fan-delta depositional system of Es₃ in Beitang sag.
- provenance analysis,
- sedimentation system,
- sedimentology,
- Beitang sag,
- the third member of Shahejie Formation

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References(48)

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Provenance System Characters of the Third Member of Shahejie Formation in the Paleogene in Beitang Sag

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