沙垒田凸起前古近系基岩分布及源—汇过程

刘强虎; 朱筱敏; 李顺利; 李慧勇; 石文龙

doi:10.3799/dqkx.2016.134

Volume 41 Issue 11

Nov. 2016

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Liu Qianghu, Zhu Xiaomin, Li Shunli, Li Huiyong, Shi Wenlong, 2016. Pre-Palaeogene Bedrock Distribution and Source-to-Sink System Analysis in the Shaleitian Uplift. Earth Science, 41(11): 1935-1949. doi: 10.3799/dqkx.2016.134

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Liu Qianghu, Zhu Xiaomin, Li Shunli, Li Huiyong, Shi Wenlong, 2016. Pre-Palaeogene Bedrock Distribution and Source-to-Sink System Analysis in the Shaleitian Uplift. Earth Science, 41(11): 1935-1949. doi: 10.3799/dqkx.2016.134

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Pre-Palaeogene Bedrock Distribution and Source-to-Sink System Analysis in the Shaleitian Uplift

doi: 10.3799/dqkx.2016.134

Liu Qianghu^{1,2
,},
Zhu Xiaomin^{1,2
,
,},
Li Shunli^1,2,
Li Huiyong³,
Shi Wenlong³

1.
State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China
2.
College of Geosciences, China University of Petroleum, Beijing 102249, China
3.
Tianjin Branch of China National Offshore Oil Corporation Limited, Tianjin 300452, China

Received Date: 2016-05-23
Publish Date: 2016-11-15

Abstract

Abstract

During the early stage of the Palaeogene, the Shaleitian uplift and its surrounding areas constituted a complete source-to-sink system. In this paper, we analysze the characteristics of Pre-Palaeogene bedrocks and sediment-dispersal patterns of the source-to-sink systems based on detritus, thin section, zircon and integrated seismic-logging data analysis. The results show that the Shaleitian uplift was filled by Archeozoic and Proterozoic metamorphic rock sediments, and Lower Palaeozoic carbonate rocks stacked with southward Mesozoic igneous rocks. The bedrocks mainly consist of Proterozoic metamorphic rocks in the southern part of eastern Shaleitian uplift, while the Lower Palaeozoic carbonate rocks in the northern part of western Shaleitian uplift. Based on the palaeogeomorphology, it is found a sand-rich area corresponds to a complete source-to-sink coupling system in the rift basin, and the stacked style and size of sandbodies in the sink are jointly controlled by the composition of bedrocks, catchment areas, sediment-transport pathways, fracture system and detritus accommodation space. It is concluded thateffective source-to-sink systems are mainly located in the southern part of the eastern Shaleitian uplift through comparative analysis of the coupling relationship among the various controls with sandbodies properties in the Shaleitian uplift and surrounding areas.
- bedrocks,
- source-to-sink system,
- zircon U-Pb ages,
- Paleogeomorphic,
- Shaleitian uplift,
- sedimentology

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References(51)

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Pre-Palaeogene Bedrock Distribution and Source-to-Sink System Analysis in the Shaleitian Uplift

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