A genetic and evolutionary model for the Pliocene granular limestone reef in the Madura Strait Basin, Indonesia

LIU Jiacheng; LUAN Xiwu; RAN Weinmin; WEI Xinyuan; WANG Kuo; ZHANG Hao; SHI Yanfeng; LU Yintao; Mohammad Saiful Islam

doi:10.16562/j.cnki.0256-1492.2019021401

2020 Vol. 40, No. 3

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Article navigation > Marine Geology & Quaternary Geology > 2020 > 40(3): 87-98

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LIU Jiacheng, LUAN Xiwu, RAN Weinmin, WEI Xinyuan, WANG Kuo, ZHANG Hao, SHI Yanfeng, LU Yintao, Mohammad Saiful Islam. A genetic and evolutionary model for the Pliocene granular limestone reef in the Madura Strait Basin, Indonesia[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 87-98. doi: 10.16562/j.cnki.0256-1492.2019021401

Citation:

LIU Jiacheng, LUAN Xiwu, RAN Weinmin, WEI Xinyuan, WANG Kuo, ZHANG Hao, SHI Yanfeng, LU Yintao, Mohammad Saiful Islam. A genetic and evolutionary model for the Pliocene granular limestone reef in the Madura Strait Basin, Indonesia[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 87-98. doi: 10.16562/j.cnki.0256-1492.2019021401

A genetic and evolutionary model for the Pliocene granular limestone reef in the Madura Strait Basin, Indonesia

1.
Institute of Exploration and Development, SINOPEC Shanghai Offshore Oil & Gas Company, Shanghai 200120, China
2.
Evaluation and Detection Technology Laboratory of Marine Mineral Resources, Qingdao Pilot National Laboratory for Marine Science and Technology, Qingdao 266237, China
3.
Qingdao Institute of Marine Geology, Qingdao 266071, China
4.
Shandong University of Science and Technology, Qingdao 266590, China
5.
China University of Petroleum, Qingdao 266580, China
6.
PetroChina Hangzhou Research Institute of Geology, Hangzhou 310023, China
7.
University of Dhaka, Dhaka 1000, Bangladesh

More Information

Corresponding author: LUAN Xiwu, xluan@qnlm.ac

Received Date: 14 February 2019

Revised Date: 12 May 2019

Publish Date: 25 June 2020

Abstract

Abstract

Granular limestone reefs in an east-west direction are well developed on the outer shelf platform along the northern margin of the Madura Strait Basin, Indonesia. The reefs were formed by foraminifera shells during the compression and inversion period of early Pliocene in this region. Because of their specific origin, the petrological characteristics and seismic reflection attributes are obviously different from the surrounding rocks. These differences make it possible to identify reefs from others with seismic interpretation and seismic attribute extraction technology. For example, the reefs are often in a symmetrical hilly shape in seismic profiles, with inclined fore-reef reflection, disordered reflection and discontinuous strong reflections etc. This paper is devoted to the deposits of Pliocene Mundu Formation in the Madura Strait Basin mainly consisting of coccidian fossils from the drilling hole of Well O-2. It starts from the geological background of the region. An introduction is made to the Cenozoic tectonics and stratigraphic sequences of the basin. Through horizon calibration and three-dimensional seismic interpretation with seismic attribute extraction technology, and considering the development history and environmental patterns of the reefs, the spatial distribution of the granular coccidia limestone reefs in the basin is finally described. The study of the basin history suggests that the inverted fault zone activity is an important factor to control the reef growth in the study area. Upon the basis of this, a reef development model of the Madura Strait Basin is summarized.
- granular limestone reef /
- reverse fault zone /
- depositional environment /
- Madura Strait Basin

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