西昆仑山前侏罗-白垩系分布特征及其控制因素

程晓敢; 陈汉林; 师骏; 廖林; 杜治利; 黄智斌

doi:10.3799/dqkx.2012.073

Volume 37 Issue 4

Jul. 2012

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Article Navigation > Earth Science > 2012 > 37(4): 635-644

CHENG Xiao-gan, CHEN Han-lin, SHI Jun, LIAO Lin, DU Zhi-li, HUANG Zhi-Bin, 2012. Distribution Characteristics and Controlling Factors of Jurassic-Cretaceous in the Front of West Kunlun Mountains. Earth Science, 37(4): 635-644. doi: 10.3799/dqkx.2012.073

Citation:

CHENG Xiao-gan, CHEN Han-lin, SHI Jun, LIAO Lin, DU Zhi-li, HUANG Zhi-Bin, 2012. Distribution Characteristics and Controlling Factors of Jurassic-Cretaceous in the Front of West Kunlun Mountains. Earth Science, 37(4): 635-644. doi: 10.3799/dqkx.2012.073

Citation:

CHENG Xiao-gan, CHEN Han-lin, SHI Jun, LIAO Lin, DU Zhi-li, HUANG Zhi-Bin, 2012. Distribution Characteristics and Controlling Factors of Jurassic-Cretaceous in the Front of West Kunlun Mountains. Earth Science, 37(4): 635-644. doi: 10.3799/dqkx.2012.073

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Distribution Characteristics and Controlling Factors of Jurassic-Cretaceous in the Front of West Kunlun Mountains

doi: 10.3799/dqkx.2012.073

CHENG Xiao-gan^{1, 2
,},
CHEN Han-lin^{1, 2
,
,},
SHI Jun³,
LIAO Lin⁴,
DU Zhi-li³,
HUANG Zhi-Bin³

1.
Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China
2.
Structural Research Center of Oil and Gas Bearing Basin of Ministry of Education, Hangzhou 310027, China
3.
Exploration and Development Research Institute of Tarim Oil Field, PetroChina, Korla 841000, China
4.
Guangzhou Marine Geological Survey, Guangzhou 510075, China

Received Date: 2012-01-18
Available Online: 2021-10-13
Publish Date: 2012-07-15

Abstract

Abstract

Jurassic-Cretaceous strata are widespread in outcrops of northern margin of West Kunlun Mountains. However, drilling data indicate that they are sparsely and discontinuously distributed in the foreland overlaid regions. To determine the contact relations between the Jurassic-Cretaceous and overlaying and underlying strata, and their distribution and thickness variation, new data of field geologic investigation and interpretation of seismic profiles are presented, which suggest that the Jurassic-Cretaceous strata overlay the beneath sequences in an angular unconformity and contact with the overlaying sediments in a parallel unconformity, while within the Jurassic-Cretaceous sequence they contact with each other in conformity or parallel unconformity. These contact relations show totally different features compared to those of adjacent regions. Based on these contact relations, we establish structural interpretation models. The structural interpretation of seismic profiles and subsequent strata distribution and thickness variation indicate that compression event in End Triassic and its remnant paleo-tectonotopography has controlled occurrence and thickness of Jurassic-Cretaceous strata, while compression since Neogene has reconstructed their distribution and thickness patterns. The study results provide significant constraints for the Mesozoic-Cenozoic evolution of piedmont fold and thrust belt in the front of West Kunlun Mountains and petroleum exploration in this region.
- the front of West Kunlun Mountains,
- Mesozoic,
- stratigraphic contact relationship,
- depositional model,
- controlling factors,
- geophysics,
- tectonics

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References(44)

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Distribution Characteristics and Controlling Factors of Jurassic-Cretaceous in the Front of West Kunlun Mountains

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