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《Earth Science(Journal of China University of Geosciences)》 2013-01
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Late Miocene-Pleistocene Calcareous Nannofossil Biostratigraphy of Shenhu Gas Hydrate Drilling Area in the South China Sea and Variations in Sedimentation Rates

CHEN Fang 1,2,SU Xin 3,ZHOU Yang 1,2 1.Guangzhou Marine Geological Survey,Guangzhou 510760,China 2.Key Laboratory of Subseafloor Mineral Resources and Geological Environment,Ministry of Land and Resources,Guangzhou 510760,China 3.School of Marine Geosciences,China University of Geosciences,Beijing 100083,China  
The first Chinese gas hydrate drilling program was carried out on the Shenhu area in 2007and obtained gas hydrate samples.In order to understand the strata,age of the zone of gas hydrate occurrence and features of sedimentation rates,Late Miocene to Pleistocene calcareous nanofossil biostratigraphy in 4holes(SH1B,SH2B,SH5Cand SH7B)from the Shenhu gas hydrate drilling area of the northern South China Sea have been studied.A total of 17Late Miocene to Pleistocene nanofossil events are recognized.The oldest sediments recovered are in an age of late Miocene,younger than 7.362Ma,and the age assigned for gas hydrate occurrence zone is late Miocene in Hole SH2Band late Miocene to early Pliocene in Hole SH7B.Sedimentation rates varied with holes and times,increasing from Pliocene,and reaching the highest values in Holocene,for example,1.88-3.27cm/ka during Pliocene and 20-34.16cm/ka in Holocene,respectively.Sedimentation rates of 1.88cm/ka to 4.18cm/ka were estimated for sediment sequences in gas hydrate occurrence zone.The results suggest that the relationship between sedimentation rates and occurrence of gas hydrates should be more complicated than our earlier knowledge.
【Fund】: 国家重点基础发展研究规划项目(No.2009CB219502);; 国土资源部公益性行业科研基金项目课题(No.200811014-02-02);; 国家专项项目课题(No.GZH2011003050602)
【CateGory Index】: P736
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