湘中坳陷泥盆系碳氧同位素特征及其古环境意义

刘安; 陈林; 陈孝红; 田巍; 李海; 郄文昆; 周鹏

doi:10.3799/dqkx.2020.362

Volume 46 Issue 4

Apr. 2021

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Liu An, Chen Lin, Chen Xiaohong, Tian Wei, Li Hai, Qie Wenkun, Zhou Peng, 2021. Carbon and Oxygen Isotopic Characteristics of Devonian in Central Hunan Depression and Its Paleoenvironmental Significance. Earth Science, 46(4): 1269-1281. doi: 10.3799/dqkx.2020.362

Citation:

Liu An, Chen Lin, Chen Xiaohong, Tian Wei, Li Hai, Qie Wenkun, Zhou Peng, 2021. Carbon and Oxygen Isotopic Characteristics of Devonian in Central Hunan Depression and Its Paleoenvironmental Significance. Earth Science, 46(4): 1269-1281. doi: 10.3799/dqkx.2020.362

Citation:

Liu An, Chen Lin, Chen Xiaohong, Tian Wei, Li Hai, Qie Wenkun, Zhou Peng, 2021. Carbon and Oxygen Isotopic Characteristics of Devonian in Central Hunan Depression and Its Paleoenvironmental Significance. Earth Science, 46(4): 1269-1281. doi: 10.3799/dqkx.2020.362

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Carbon and Oxygen Isotopic Characteristics of Devonian in Central Hunan Depression and Its Paleoenvironmental Significance

doi: 10.3799/dqkx.2020.362

Liu An^{1
,
,},
Chen Lin^{1
,
,
,},
Chen Xiaohong¹,
Tian Wei¹,
Li Hai¹,
Qie Wenkun²,
Zhou Peng¹

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China

Received Date: 2020-05-06
Publish Date: 2021-04-15

Abstract

Abstract

Based on the systematic carbon and oxygen isotope and organic carbon testing, the carbon and oxygen isotope characteristics of the Devonian in the Central Hunan depression were analyzed by fully proving the validity of the testing data. Results show that the δ¹³C values of Devonian are less affected by later alteration in the Central Hunan area. The δ¹³C of Devonian gradually decreases from the bottom to the top and shows a significant negative shift at the bottom of the Oujiachong Formation, and then gradually increases upward. The δ¹⁸O curve shows a slowly increasing trend from Middle Devonian to Upper Devonian. The above curves are similar to the carbon and oxygen isotopic curves of the global Devonian strata, and have a relatively consistent trend of change. The shape and migration degree of δ¹³C curve of Devonian strata in the area are highly comparable with Longmenshan Section in Sichuan Province, Qilinzhai Section in Dushan, Lali Section in Guangxi, and Euramerican platform section, which can be used as the basis for stratigraphic division and correlation in the area and analysis of paleo-marine environment evolution. Results show that there are differences between the δ¹³C curve and the sea level change from the top of Qiziqiao Formation to the bottom part of Shetianqiao Formation, indicating that the regional paleowater depth change is comprehensively dominated by the regional tectonic activities and the global sea level changes. There is a significant correlation between the δ¹³C positive drift and the high TOC in the shale of this area, which indicates that the organic-rich shale intervals at the lower part of Shetianqiao Formation and the upper part of Menggongao Formation are the products of large-scale transgression. The intervals consist of the main shale gas exploration target strata of Devonian in the study area.
- Central Hunan depression,
- Devonian,
- carbon and oxygen isotope,
- sedimentary environment,
- organic rich shale,
- shale gas

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References(70)

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Carbon and Oxygen Isotopic Characteristics of Devonian in Central Hunan Depression and Its Paleoenvironmental Significance

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