Journal of Tropical Oceanography ›› 2021, Vol. 40 ›› Issue (3): 34-43.doi: 10.11978/YG2020008CSTR: 32234.14.YG2020008

• Review • Previous Articles     Next Articles

Surveying mud volcanoes over the Dongsha Waters in the South China Sea

YAN Pin1,2,3(), WANG Yanlin1,2,3, YU Junhui1,2,3, LUO Wei1,4,5, LIU Xingjian1,2,3, JIN Yongbin1,2,3, LI Pengchun1,2,3, LIU Jie1,2,3, ZHONG Guangjian6, YI Hai6   

  1. 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 5111458, China
    3. Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Qingdao 266071, China
    4. CNOOC (China) Co., Ltd. Shenzhen Branch, Shenzhen 518054, China
    5. University of Chinese Academy of Sciences, Beijing 100049, China
    6. Guangzhou Marine Geological Survey, Guangzhou 510760, China
  • Received:2020-11-26 Revised:2020-12-13 Online:2021-05-10 Published:2020-12-13
  • Contact: YAN Pin E-mail:yanpin@scsio.ac.cn
  • Supported by:
    National Natural Science Foundation of China(U1901217);National Natural Science Foundation of China(91855101);National Natural Science Foundation of China(41876052);Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0104);Special Support Program for Cultivating High-level Talents in Guangdong Province(2019BT02H594);CAS Senior User Project of RV KEXUE(KEXUE2019G10);CAS Open Fund of the Key Laboratory of Marine Geology and Environment(MGE2018KG14);Geological Survey Program of the Ministry of Natural Resources of the People’s Republic of China(DD20190212);National Natural Science Foundation of Guangdong Province, China(2018A0303130125)

Abstract:

As an important expression of Earth’s movement and a migration way for fluid-rich materials from substrates to the surface, mud volcanism and the entrained materials carry with ample information that is important for understanding the geodynamics, stratigraphic lithology, resources, and environment. Featuring thin (~1 km) Cenozoic Erathem and considerably thick (>5 km) Mesozoic Erathem, the Dongsha Waters is deemed as the best but unproven prospect for petroleum sourced from the Mesozoic Erathem. It is also rich with seamounts and submarine hills that are believed as magmatic volcanoes, a potential risk factor for petroleum accumulation. However, it is revealed from recent geophysical surveys that many of the seamounts and hills have developed with remarkable diapiric deformation and faults, fluid infill-led blank reflection zone, fluid seepage, and emission. By sampling with box dredges over tens of seamount and hill, plentiful authigenic carbonate nodules and deep-water corals, sponges, etc., have been collected, which feature them mud volcanoes. Discovery of the mud volcanoes shows favorable conditions for petroleum source and migration over the waters, and provides excellent lines to explore the petroleum and gas hydrates sourced from the Mesozoic Erathem. Abundance of deep-sea coral, sponge and others implies the Dongsha mud volcanoes as potential province for deep-sea coral and sponge reefs, meaningful to study the relationship among petroleum seepage, growth of chemosynthetic community and marine environment.

Key words: Dongsha Waters, mud volcano, deep-water coral, authigenic carbonates, petroleum and hydrate prospect, Mesozoic Erathem

CLC Number: 

  • P618.13