CENOZOIC MARINE SEDIMENTATION PROBLEM OF THE TARIM BASIN

LI Jian-feng; ZHAO Yue; PEI Jun-ling; LIU Feng; ZHOU Zai-zheng; GAO Hai-long; GAO Liang; FU Zi-bo

Volume 23 Issue 1

Feb. 2017

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LI Jian-feng, ZHAO Yue, PEI Jun-ling, et al., 2017. CENOZOIC MARINE SEDIMENTATION PROBLEM OF THE TARIM BASIN. Journal of Geomechanics, 23 (1): 141-149.

Citation:

LI Jian-feng, ZHAO Yue, PEI Jun-ling, et al., 2017. CENOZOIC MARINE SEDIMENTATION PROBLEM OF THE TARIM BASIN. Journal of Geomechanics, 23 (1): 141-149.

Citation:

LI Jian-feng, ZHAO Yue, PEI Jun-ling, et al., 2017. CENOZOIC MARINE SEDIMENTATION PROBLEM OF THE TARIM BASIN. Journal of Geomechanics, 23 (1): 141-149.

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CENOZOIC MARINE SEDIMENTATION PROBLEM OF THE TARIM BASIN

LI Jian-feng^{1, 2
,},
ZHAO Yue^{1, 2
,
,},
PEI Jun-ling^{1, 2},
LIU Feng^{1, 2},
ZHOU Zai-zheng^{1, 2},
GAO Hai-long^{1, 2},
GAO Liang^{1, 2},
FU Zi-bo³

1.
Key Laboratory of Paleomagnetism and Tectonic Reconstruction of Ministry of Land and Resources, Beijing 100081, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
3.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

More Information

Received: 2016-06-13
Published: 2017-02-01

Abstract

Abstract

Based on former studies, this paper combines the problems on Cenozoic marine sedimentation of Tarim basin and discusses the times and scope of transgression, and time and cause of the Paratethys regression from Tarim basin in Cenozoic. The results suggest that Tarim basin experienced at least three marine incursions in Cenozoic, they are Late Aertashi-Early Qimugen (the Early Paleocene to Late Paleocene), Kalatar-Wulagen (the Middle Eocene) and Middle Bashibulake (the Late Eocene to Early Oligocene). Further evidence is needed for the recognition of the marine strata that existed in Tarim basin in Miocene. The maximum transgression corresponded to the Kalatar-Wulagen. Further, the seawater reached Mazhatagh, then the east of Kuala and the east of Aqike, which are northern and southern margins of Tarim basin, respectively. On the effect of global eustatic sea level change combined with tectonism in Cenozoic, the top of the Qimugen, the top of the Wulagen and, the fourth and fifth segments of the Bashibulake formed due to the Paratethys Sea regression, corresponding to Late Paleocene, Late Eocene and Early Oligocene, respectively.
- Tarim basin,
- Paratethys Sea,
- Cenozoic,
- transgression,
- regression

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References(52)

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