RECONSTRUCTION OF PALAEO-WATER DEPTH OF NEOCENE SHRINKING LAKE: AN EXAMPLE FROM THE SOUTH OF BODONG LOW UPLIFT, BOHAI SEA

PAN Wenjing; LIU Shilei; TIAN Derui; GUO Longlong; WANG Xiaoling; WANG Lihong

doi:10.16028/j.1009-2722.2019.04003

2019 Vol. 35, No. 4

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Article navigation > Marine Geology Frontiers > 2019 > 35(4): 18-25

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PAN Wenjing, LIU Shilei, TIAN Derui, GUO Longlong, WANG Xiaoling, WANG Lihong. RECONSTRUCTION OF PALAEO-WATER DEPTH OF NEOCENE SHRINKING LAKE: AN EXAMPLE FROM THE SOUTH OF BODONG LOW UPLIFT, BOHAI SEA[J]. Marine Geology Frontiers, 2019, 35(4): 18-25. doi: 10.16028/j.1009-2722.2019.04003

Citation:

PAN Wenjing, LIU Shilei, TIAN Derui, GUO Longlong, WANG Xiaoling, WANG Lihong. RECONSTRUCTION OF PALAEO-WATER DEPTH OF NEOCENE SHRINKING LAKE: AN EXAMPLE FROM THE SOUTH OF BODONG LOW UPLIFT, BOHAI SEA[J]. Marine Geology Frontiers, 2019, 35(4): 18-25. doi: 10.16028/j.1009-2722.2019.04003

RECONSTRUCTION OF PALAEO-WATER DEPTH OF NEOCENE SHRINKING LAKE: AN EXAMPLE FROM THE SOUTH OF BODONG LOW UPLIFT, BOHAI SEA

1.
CNOOC Tianjin Company, Tianjin 300459, China
2.
CNOOC Energy Technology & Services Limited, Tianjin 300459, China

Received Date: 16 October 2018

Publish Date: 28 April 2019

Abstract

Abstract

The Neocene in the southeast Bohai Sea consists mainly of lacustrine, shallow water deltaic and fluvial facies. Drastic facies changes have made sandbody prediction very difficult. Palaeo-water depth of a lake is one of the key factors to sandbody distribution pattern. Based on geochemical data, INPEFA, paleontological and lithological data, the Neogene palaeo-water depth in the Penglai 7 area is investigated. The study area is located on the South of Bodong Low Uplift of the Bohai Sea.Results show that the area surrounding the Penglai 7 area was a fresh water lake with gentle slopes in Neogene. Lake level fluctuated frequently. The average depth of the area was around 3 m when the Guantao Formation was deposited. By the end of Guantao Formation, the lake level started rising. In the beginning, the water depth is deeper in south. However, it was reversed by the end of Guantao Formation and it became deeper in north. Water depth reached its peak in Late Minghuazhen Formation. The average depth of Penglai 7 area was around 4-6 m in the time when the Lower Member of Minghuazhen Formation was deposited.
- Bohai Sea /
- Neocene /
- palaeontology /
- palaeo-lacustrine basin /
- palaeo-water depth

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