4.6 Article

Astronomical time scale of a Middle Eocene lacustrine sequence from the Dongpu Sag, Bohai Bay Basin, Eastern China

Journal

JOURNAL OF ASIAN EARTH SCIENCES
Volume 214, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.jseaes.2021.104747

Keywords

ATS; Eocene Shahejie Formation; Lacustrine sequence; Oil and gas exploration; Cyclostratigraphy

Funding

  1. program of the National Science & Technology Major Project of China [2017ZX05009001]
  2. National Natural Science Foundation of China [41772138]

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Located in the SW part of the Bohai Bay Basin, the Dongpu Sag is rich in oil and gas, with the main source rock found in the third member (Es3) of the Middle Eocene Shahejie Formation. Due to the complex geology of the area, the stratigraphic subdivision and deposition timing of each member and sub-member in the Shahejie Formation is challenging and controversial. By establishing a high-resolution cyclostratigraphic framework, the study provides a more precise time interval to locate the effective source rocks in the sag and allows for fine-scale stratigraphic correlation within the region and beyond.
Being a part of the petroliferous Linqing depression, the Dongpu Sag is located in the SW part of the Bohai Bay Basin, eastern China, and is rich in oil and gas. As new discoveries of conventional, structural, and stratigraphic plays of oil and gas have been gradually diminished in the sag, there is an urgent requirement to explore unconventional shale oil and gas, for which the effective source rocks must be located accurately. In the Dongpu Sag, the main source rock is present in the third member (Es3) of the Middle Eocene Shahejie Formation, with the hydrocarbon generation potential being relatively variable in each sub-member. The optimum source rock is perceived to be present between the lower and middle parts of Es3. However, as the Dongpu Sag is full of complex fault blocks and salt formations, the stratigraphic subdivision and deposition timing of each member and sub-member in the Shahejie Formation is rather challenging and controversial. Based on the paleontology and wireline (esp. gamma-ray) log data of the P6-65 well in the center of the sag, a high-resolution cyclostratigraphic framework of the lower and middle parts of Es3 has been established, with sediment accumulation rates and paleoenvironment being validated by chemostratigraphy (elemental data from spot X-ray fluorescence analysis) from the nearby W-410 well. This astronomical framework is more precise than the paleontology framework established previously in the Dongpu Sag. Additionally, it provides a precise time interval to locate the effective source rocks within the sag, allowing a fine-scale stratigraphic correlation within the sag and to other sags in the Bohai Bay Basin, which is otherwise not possible due to insufficient absolute age data in the Dongpu Sag.

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