多旋回叠合盆地烃流体源与构造变形响应: 以扬子地块中古生界海相为例

汤济广; 梅廉夫; 沈传波; 刘昭茜

doi:10.3799/dqkx.2012.059

Volume 37 Issue 3

May 2012

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Article Navigation > Earth Science > 2012 > 37(3): 526-534

TANG Ji-guang, MEI Lian-fu, SHEN Chuan-bo, LIU Zhao-qian, 2012. Response of Hydrocarbon Fluid Source to Tectonic Deformation in Multicycle Superimposed Basin: Example from Palaeozoic and Mesozoic Marine Strata in Yangtze Block. Earth Science, 37(3): 526-534. doi: 10.3799/dqkx.2012.059

Citation:

TANG Ji-guang, MEI Lian-fu, SHEN Chuan-bo, LIU Zhao-qian, 2012. Response of Hydrocarbon Fluid Source to Tectonic Deformation in Multicycle Superimposed Basin: Example from Palaeozoic and Mesozoic Marine Strata in Yangtze Block. Earth Science, 37(3): 526-534. doi: 10.3799/dqkx.2012.059

Citation:

TANG Ji-guang, MEI Lian-fu, SHEN Chuan-bo, LIU Zhao-qian, 2012. Response of Hydrocarbon Fluid Source to Tectonic Deformation in Multicycle Superimposed Basin: Example from Palaeozoic and Mesozoic Marine Strata in Yangtze Block. Earth Science, 37(3): 526-534. doi: 10.3799/dqkx.2012.059

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Response of Hydrocarbon Fluid Source to Tectonic Deformation in Multicycle Superimposed Basin: Example from Palaeozoic and Mesozoic Marine Strata in Yangtze Block

doi: 10.3799/dqkx.2012.059

TANG Ji-guang^{1, 2
,},
MEI Lian-fu^{2, 3},
SHEN Chuan-bo^{2, 3},
LIU Zhao-qian^{2, 3}

1.
Geosciences College, Yangtze University, Jingzhou 434023, China
2.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2011-09-23
Available Online: 2021-11-09
Publish Date: 2012-05-01

Abstract

Abstract

Multicycle tectonic evolution controls the hydrocarbon-generation evolution, and causes variegated genesis of hydrocarbon fluid source in the multicycle superimposed basin. The temperature is the essential factor to hydrocarbon-generation evolution, and it could be reflected by burial depth of geologic body, so the control of tectonic deformation on hydrocarbon-generation evolution of hydrocarbon fluid source is mainly displayed by the burial history of geologic body. According to the tectonic evolution characteristics, there are four kinds of different deformation in Yangtze block, such as inversion of fault depression, inversion of fault block, thrusting and composite superimpose, then, the four patterns of tectonic evolution-burial history are also established about the marine strata in Meso-Cenozoic. Based on the response of hydrocarbon fluid source to the type of tectonic evolution-burial history, the study indicates that there are vestigal protogenic hydrocarbon and hydrocarbon generated secondly from kerogen in Lower Yangtze region and Jianghan fault depression of whose tectonic evolution-burial history is consuming exposure-fault depression burial, and vestigal protogenic hydrocarbon in the western Hunan-Hubei and Dahongshan area in Middle Yangtze region of which is consuming uplift-marine strata exposure, kerogen-cracking gas, oil-cracking gas and vestigal protogenic hydrocarbon in the thrust belts of Longmenshan and Dabashan of which is late low uplift-thrust burial, kerogen-cracking gas and oil-cracking gas in the northern Jiangnan uplift of which is consuming uplift-thrust burial, kerogen-cracking gas, oil-cracking gas and bitumen-cracking gas in Upper Yangtze region whose type of ones is durative burial-later uplift.
- hydrocarbon fluid source,
- tectonic deformation,
- multicycle superimposed basin,
- marine strata,
- Yangtze block,
- petroleum geology

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References(46)

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Response of Hydrocarbon Fluid Source to Tectonic Deformation in Multicycle Superimposed Basin: Example from Palaeozoic and Mesozoic Marine Strata in Yangtze Block

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