Origin of a giant fuzzy reflection zone and its implication for natural gas exploration in the southwestern Qiongdongnan Basin of the South China Sea

Junhui YU; Pin YAN; Yanlin WANG; Yan QIU; Guanghong TU; Changliang CHEN

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Origin of a giant fuzzy reflection zone and its implication for natural gas exploration in the southwestern Qiongdongnan Basin of the South China Sea

Sedimentary processes and resource potential in the South China Sea | Updated：2024-10-12

- Origin of a giant fuzzy reflection zone and its implication for natural gas exploration in the southwestern Qiongdongnan Basin of the South China Sea
- Origin of a giant fuzzy reflection zone and its implication for natural gas exploration in the southwestern Qiongdongnan Basin of the South China Sea
- 海洋湖沼学报(英文) 2023年41卷第2期页码：710-728
- Affiliations：
  
  1.Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China
  2.Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
  3.Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  4.Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, China Geological Survey, Ministry of Natural Resources, Guangzhou 511458, China
  5.University of Chinese Academy of Sciences, Beijing 100049, China
- Author bio：
  
  yanpin@scsio.ac.cn
  chenchangliang@scsio.ac.cn
- Funds：
  
  the Guangdong Basic and Applied Basic Research Foundation(2022A1515011836;2021A1515110851);the Science and Technology Planning Project of Guangzhou(202201010230);the Guangdong Special Support Key Team Program(2019BT02H594);the Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0104);the Open Fund of Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences (CAS)(MGE2020KG01);the National Natural Science Foundation of China(U1901217;91855101;41876052;42076218);Dr. Junhui YU is funded by the Special Research Assistant Funding Program of CAS
- DOI：
  中图分类号：
- 收稿：2021-12-31，
  
  纸质出版：2023-03-01
- Accepted：
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Origin of a giant fuzzy reflection zone and its implication for natural gas exploration in the southwestern Qiongdongnan Basin of the South China Sea[J]. 海洋湖沼学报(英文), 2023,41(2):710-728.

YU Junhui,YAN Pin,WANG Yanlin,et al.Origin of a giant fuzzy reflection zone and its implication for natural gas exploration in the southwestern Qiongdongnan Basin of the South China Sea[J].Journal of Oceanology and Limnology,2023,41(02):710-728.
Origin of a giant fuzzy reflection zone and its implication for natural gas exploration in the southwestern Qiongdongnan Basin of the South China Sea[J]. 海洋湖沼学报(英文), 2023,41(2):710-728. DOI：

YU Junhui,YAN Pin,WANG Yanlin,et al.Origin of a giant fuzzy reflection zone and its implication for natural gas exploration in the southwestern Qiongdongnan Basin of the South China Sea[J].Journal of Oceanology and Limnology,2023,41(02):710-728. DOI：

摘要

Abstract

The southwestern depression of the Qiongdongnan Basin (QDNB) hosts thick Cenozoic sediments and awaits major hydrocarbon discovery. Multichannel seismic (MCS) profile CFT2011 across the southwestern QDNB reveals a ~60-km-wide fuzzy reflection zone (FRZ) within the sediments

but its origin and distribution remain unclear. Here ocean bottom seismometer (OBS) data of Line CFT2011 are processed with focus on the velocity structures by traveltime tomography inversion and analyzed together with the coincident and adjacent MCS profiles. The

OBS velocity results show that the giant FRZ features lower velocity with difference up to 1.5 km/s and smaller vertical velocity gradient than the surrounding sedimentary sequences at the same depth

likely resulting from enhanced fluid infilling. The MCS profile exhibits that the giant FRZ is about 3–9-km thick and extends from the Paleogene strata rich in organic matters upward to the lower Pleistocene sediments. Within the shallow overlying sediments

multiple bright spots with reverse polarity are imaged and their reflection amplitudes increase with offset

consistent with the features of gas-charged sediments. They are probably shallow gas reservoirs with gases sourced from the deep FRZ. Therefore

the FRZ is proposed to be a giant gas-charged zone

which probably contains lots of hydrocarbon gases migrated vertically from the deep Paleogene source rocks through the boundary faults of the depressions and the minor fractures generated under overpressure. This FRZ is also imaged on the adjacent MCS profiles MCS-L1 and MCS-L2 with the width of about 40 km and 68 km

respectively. It is roughly estimated to cover an area of ~1 900 km

and host a volume of ~11 400 km

assuming an average thickness of 6 km

implying huge natural gas potential in the sedimentary depression of the southwestern QDNB of the South China Sea.

关键词

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