西沙群岛西科1井碳酸盐岩稳定同位素地层学

乔培军; 朱伟林; 邵磊; 张道军; 成鑫荣; 宋亚敏

doi:10.3799/dqkx.2015.060

Volume 40 Issue 4

Apr. 2015

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Article Navigation > Earth Science > 2015 > 40(4): 725-732

Qiao Peijun, Zhu Weilin, Shao Lei, Zhang Daojun, Cheng Xinrong, Song Yamin, 2015. Carbonate Stable Isotope Stratigraphy of Well Xike-1, Xisha Islands. Earth Science, 40(4): 725-732. doi: 10.3799/dqkx.2015.060

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Qiao Peijun, Zhu Weilin, Shao Lei, Zhang Daojun, Cheng Xinrong, Song Yamin, 2015. Carbonate Stable Isotope Stratigraphy of Well Xike-1, Xisha Islands. Earth Science, 40(4): 725-732. doi: 10.3799/dqkx.2015.060

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Carbonate Stable Isotope Stratigraphy of Well Xike-1, Xisha Islands

doi: 10.3799/dqkx.2015.060

1.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
2.
China National Offshore Oil Corporation, Beijing 100010, China
3.
Zhanjiang Branch of China National Offshore Oil Corporation Limited, Zhanjiang 524057, China

Received Date: 2014-11-06
Publish Date: 2015-04-01

Abstract

Abstract

The oxygen stable isotopes in carbonate sediment of well Xike-1 cannot be used to calibrate strata ages due to the destructive effect of recrystallization and dolomitization, while the paired δ¹³C records can be used to calibrate Xike-1 strata age since 200 ka, because of the similar patterns with those of the South China Sea and other oceans. Accordingly, the 0-50 m sediment of the well corresponds to the oxygen isotope stages (MIS) 1-7, with the MIS 1/2 boundary (14 ka) at 5 m, the MIS 2/3 boundary (29 ka) at 11.70 m, the MIS 3/4 boundary (57 ka) at 13.90 m, the MIS 4/5 boundary (71 ka) at 16.8 m, the MIS 5/6 boundary (129 ka) at 23.8 m and the MIS 6/7 boundary at 35.65 m respectively. Moreover, the δ¹³C records exhibit low values in glacial periods and high values in interglacial periods. The U-Th dating of coral from 25.21 m is 131.062±2.320 ka. It is concluded from the dating that there are no sediments younger than 5 ka existing on the Shidao Island of Xisha, and the transition from the interglacial to glacial periods with downward movement of global sea-level lead to the exposition and erosion of the local carbonate platform, which indicates that the abrupt changes of the δ¹³C records of the carbonate sediments from Xike-1 are responses to global climate variations.
- Xisha Islands,
- coral reef,
- stable isotope,
- strata,
- palaeoceanography,
- marine geology

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References(41)

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Carbonate Stable Isotope Stratigraphy of Well Xike-1, Xisha Islands

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