ACCUMULATION PATTERN OF ORGANIC MATTER IN SHALES OF THE LOWER CAMBRIAN NIUTITANG FORMATION, CHUANDONG-WULINGSHAN AREA

ZHOU Lei; WANG Zongxiu; LI Huijun; ZHANG Linyan; ZHANG Kaixun; LIANG Mingliang

doi:10.12090/j.issn.1006-6616.2018.24.05.062

Volume 24 Issue 5

Oct. 2018

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Article Navigation > Journal of Geomechanics > 2018 > 24(5): 617-626

ZHOU Lei, WANG Zongxiu, LI Huijun, et al., 2018. ACCUMULATION PATTERN OF ORGANIC MATTER IN SHALES OF THE LOWER CAMBRIAN NIUTITANG FORMATION, CHUANDONG-WULINGSHAN AREA. Journal of Geomechanics, 24 (5): 617-626. DOI: 10.12090/j.issn.1006-6616.2018.24.05.062

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ACCUMULATION PATTERN OF ORGANIC MATTER IN SHALES OF THE LOWER CAMBRIAN NIUTITANG FORMATION, CHUANDONG-WULINGSHAN AREA

doi: 10.12090/j.issn.1006-6616.2018.24.05.062

ZHOU Lei^{1, 2
,},
WANG Zongxiu^{1, 2
,
,},
LI Huijun^{1, 2},
ZHANG Linyan^{1, 2},
ZHANG Kaixun^{1, 2},
LIANG Mingliang^{1, 2}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Key Lab of Shale Oil and Gas Geological Survey, Chinese Academy of Geological Sciences, Beijing 100081, China

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Received: 2018-05-04
Revised: 2018-07-25
Published: 2018-10-01

Abstract

Abstract

The accumulation and preservation of organic matter have great guiding significance for the evaluation of oil and gas reservoirs and the survey and exploration of targeting exploration area. Based on the technologies and methods of lithogeochemistry, petroleum geochemistry and sedimentology, the richness and source of organic matter and paleoenviroment evolution of the Lower Cambrian Niutitang Formation in Chuandong-Wulingshan area were analyzed. The enrichment and preservation conditions of organic matter were evaluated preliminarily. The results show that planktonic algae (including blue-green algae, rhodophyta and phaeophyta) are the primary producers of organic matter. Compared with the upper domain of Niutitang Formation, during the deposition period of transgression, the warm and humid paleoclimate and large-scale transgression made the sea level rise rapidly, and the transgression caused deep continental shelf, slope and even shallow continental shelf to be in an oxygen-deficient or anoxic environment. This deep water oxygen-deficient and anoxic reduction environment (partial sulfide reduction environment) is favorable for the preservation of organic matter, and a large area of organic-rich shales were formed in the area of Chuandong-Wulingshan area.
- organic matter,
- accumulation model,
- shale,
- Niutitang Formation,
- Chuandong-Wulingshan area

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ACCUMULATION PATTERN OF ORGANIC MATTER IN SHALES OF THE LOWER CAMBRIAN NIUTITANG FORMATION, CHUANDONG-WULINGSHAN AREA

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ACCUMULATION PATTERN OF ORGANIC MATTER IN SHALES OF THE LOWER CAMBRIAN NIUTITANG FORMATION, CHUANDONG-WULINGSHAN AREA

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