长岭断陷下白垩统湖相烃源岩形成古环境及主控因素

李浩; 陆建林; 李瑞磊; 王保华; 徐文; 左宗鑫; 王苗; 刘娅昭

doi:10.3799/dqkx.2017.539

Volume 42 Issue 10

Oct. 2017

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Article Navigation > Earth Science > 2017 > 42(10): 1774-1786

Li Hao, Lu Jianlin, Li Ruilei, Wang Baohua, Xu Wen, Zuo Zongxin, Wang Miao, Liu Yazhao, 2017. Generation Paleoenvironment and Its Controlling Factors of Lower Cretaceous Lacustrine Hydrocarbon Source Rocks in Changling Depression, South Songliao Basin. Earth Science, 42(10): 1774-1786. doi: 10.3799/dqkx.2017.539

Citation:

Li Hao, Lu Jianlin, Li Ruilei, Wang Baohua, Xu Wen, Zuo Zongxin, Wang Miao, Liu Yazhao, 2017. Generation Paleoenvironment and Its Controlling Factors of Lower Cretaceous Lacustrine Hydrocarbon Source Rocks in Changling Depression, South Songliao Basin. Earth Science, 42(10): 1774-1786. doi: 10.3799/dqkx.2017.539

Citation:

Li Hao, Lu Jianlin, Li Ruilei, Wang Baohua, Xu Wen, Zuo Zongxin, Wang Miao, Liu Yazhao, 2017. Generation Paleoenvironment and Its Controlling Factors of Lower Cretaceous Lacustrine Hydrocarbon Source Rocks in Changling Depression, South Songliao Basin. Earth Science, 42(10): 1774-1786. doi: 10.3799/dqkx.2017.539

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Generation Paleoenvironment and Its Controlling Factors of Lower Cretaceous Lacustrine Hydrocarbon Source Rocks in Changling Depression, South Songliao Basin

doi: 10.3799/dqkx.2017.539

1.
Wuxi Branch of SINOPEC Petroleum Exploration and Production Research Institute, Wuxi 214126, China
2.
Exploration and Development Research Institute, SINOPEC Northeast Oil & Gas Company, Changchun 130062, China

Received Date: 2017-03-10
Publish Date: 2017-10-18

Abstract

Abstract

Heterogeneity study of lacustrine source rocks relys heavily on a deeper understanding of paleoenvironment and the major controlling factors on their formation. Based on element geochemical and petrological analyses of the paleoenvironment of the Early Cretaceous (from K₁h to K₁yc) in Changling depression., the main controlling factors of organic source rocks development were analyzed according to the characteristics of its tectonics and sedimentary and the primary productivity of the source rocks in this study. Results show that from K₁h period to K₁sh stage to K₁yc stage, Changling depression experienced paleo-water depth change from deep to shallow, palaeoclimate from humid-semi-humid to semi-arid, palaesalinity from fresh water to brackish water, and reduction condition from enhanced to weakened. From K₁sh period to K₁yc, the paleoenvironment of Changling depression shows obvious zonation; The correlation between trace element indexs indicating the paleoclimate and water reduction and TOC (Total Organic Carbon) of the source rock samples is significant, while the correlation between the trace element indexs indicating the paleosalinity and TOC of the source rock samples is small. So the paleoclimatic and redox conditions are the main environmental factors of the development of Lower Cretaceous lacustrine source rocks in Changling fault depression; K₁sh₂ Formation high quality source rock which developed in equilibrium compensation stage, humid climate, hypoxia and high initial productivity is widely distributed. Followed by K₁sh₁ Formation and K₁h₂ Formation, the organic source rock of K₁yc Formation is relatively developed in the south and east, and the distribution is relatively limited.
- trace element,
- hydrocarbon source rock,
- paleoenvironment,
- main controlling factor,
- Changling depression,
- Songliao basin,
- petroleum geology

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Generation Paleoenvironment and Its Controlling Factors of Lower Cretaceous Lacustrine Hydrocarbon Source Rocks in Changling Depression, South Songliao Basin

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