Knowledge Management System Of Guangzhou Institute of Energy Conversion, CAS
| Research on the formation model of gas hydrate deposits in the Shenhu Area, northern South China Sea | |
| Su Zheng1; Cao Yun-Cheng2; Yang Rui1; Wu Neng-You1; Chen Duo-Fu2; Yang Sheng-Xiong3; Wang Hong-Bin3 | |
| 2014-05-01 | |
| Source Publication | CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
 |
| Volume | 57Issue:5Pages:1664-1674 |
| Abstract | The Shenhu area on the northern continental slope of the South China Sea is considered as a promising target for gas hydrate exploration and exploitation. Its special hydrate occurrence makes it difficult to explain and quantitatively describe its formation mechanism by using the deposition rates and fluid flow conditions at present. Its formation evolution mode and controlling factors are unclear yet. In this paper a dynamic model for the hydrate accumulation is constructed with two controlling parameters, i.e. the sedimentation rate and fluid water flow rate. The model is used to simulate the hydrate accumulation in the Shenhu area and testified with saturation data derived from salinity. Finally, a hydrate formation pattern in the Shenhu area is built based on the investigation of tectonic activities and the dynamics of hydrate accumulation in the area. The model indicates that Shenhu hydrates were developed from the hydrates formed in late tectonic activities during the late Pliocene Epoch-early Pleistocene Epoch. The gas hydrate formation in the Shenhu area has a typical dual pattern. In the first stage the hydrate grew in fractured sediments formed by tectonic activities 1. 5 Ma. The water flow rate was up to 50 m/ka, and abundant methane gas was carried into the hydrate stability zone and led to a rapid hydrate formation. The hydrate saturation went up to 20% in the duration of 40 ka. In the second stage of the following 1. 5 Mas, permeability of the sediment reduced sharply due to the sedimentation of clay silts. Fluid flux was 0. 7 m/ka and methane supply was inadequate. Thus hydrates could not form in shallow sediments and only grew slowly on the base of the hydrate stability zone, and then formed the feature of hydrate occurrence observed currently in the Shenhu area. And also the resource amount of hydrate continued reducing. |
| Subtype | Article |
| Keyword | Shenhu Area Gas Hydrate Tectonic Activity Formation Pattern Numerical Modeling |
| WOS Headings | Science & Technology ; Physical Sciences |
| DOI | 10.6038/cjg20140529 |
| WOS Subject Extended | Geochemistry & Geophysics |
| WOS Keyword | METHANE HYDRATE ; MARINE-SEDIMENTS ; ANAEROBIC OXIDATION ; SULFATE REDUCTION ; RIDGE ; CONSTRAINTS ; COMPACTION ; EVOLUTION ; TRANSPORT ; OREGON |
| Indexed By | SCI |
| Language | 英语 |
| WOS Subject | Geochemistry & Geophysics |
| WOS ID | WOS:000336701200029 |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.giec.ac.cn/handle/344007/10697 |
| Collection | 中国科学院广州能源研究所 |
| Affiliation | 1.Chinese Acad Sci, Guangzhou Inst Energy Convers, Guangzhou 510640, Guangdong, Peoples R China 2.Chinese Acad Sci, South China Sea Inst Oceanol, Guangzhou 510640, Guangdong, Peoples R China 3.Guangzhou Marine Geol Survey, Guangzhou 510075, Guangdong, Peoples R China |
| Recommended Citation GB/T 7714 | Su Zheng,Cao Yun-Cheng,Yang Rui,et al. Research on the formation model of gas hydrate deposits in the Shenhu Area, northern South China Sea[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2014,57(5):1664-1674. |
| APA | Su Zheng.,Cao Yun-Cheng.,Yang Rui.,Wu Neng-You.,Chen Duo-Fu.,...&Wang Hong-Bin.(2014).Research on the formation model of gas hydrate deposits in the Shenhu Area, northern South China Sea.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,57(5),1664-1674. |
| MLA | Su Zheng,et al."Research on the formation model of gas hydrate deposits in the Shenhu Area, northern South China Sea".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 57.5(2014):1664-1674. |
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