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首页> 外文期刊>Marine and Petroleum Geology >Regional stratigraphic framework and gas hydrate occurrence offshore eastern India: Core-log-seismic integration of National Gas Hydrate Program Expedition 02 (NGHP-02) Area-B drill sites
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Regional stratigraphic framework and gas hydrate occurrence offshore eastern India: Core-log-seismic integration of National Gas Hydrate Program Expedition 02 (NGHP-02) Area-B drill sites

机译:地区地层框架和天然气水合物发生海上印度东部:核心 - 震动整合国家天然气水合物计划探险02(NGHP-02)区域-B钻头

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摘要

The Indian National Gas Hydrate Program Expedition 02 (NGHP-02) was designed to study the occurrence of gas hydrate along the passive continental margin of the Indian Peninsula in the Bay of Bengal. Twelve holes were logged and measured with logging-while-drilling (LWD) and five holes were cored in Area-B of NGHP-02. The LWD and coring results in Area-B helped to understand the geological significance of sequence stratigraphy in Krishna-Godavari Basin and identified the occurrence of gas hydrate. This study summarized the log- and litho-units in Area-B and establish three integrated units based on the core-log-seismic integration. Most of the downhole log and core inferred gas hydrate occurrences are in the Late Miocene Integrated-Unit B with several sets of reservoir sections exhibiting favorable conditions for hosting gas hydrate. The gas hydrates reservoirs associated with reflectors R1 and R2 were identified and the R1 reservoirs are characterized by fracture- and pore-filling gas hydrate, and the R2 is in sand-rich sediments with pore-filling gas hydrate at high saturations. The thickness variations associated with the R1 and R2 are possibly associated with the development anticlinal structure and are likely related to syn-sedimentary growth of the folding structures. Major gas hydrate zones exist in and around the R1 and R2 near the BSR depth, and mostly have coincident with the fractures and mass-transport deposits. The spatial distribution of gas hydrate in the R1 and R2 reservoirs is highly influenced by the anticlinal structure. This study can be considered a good case for the future gas hydrate studies and explorations in the nearby areas.
机译:印度国家天然气水合物计划探险02(NGHP-02)旨在研究沿着孟加拉湾的印度半岛被动欧式边缘的天然气水合物的发生。通过钻孔(LWD)记录并测量12个孔,在NGHP-02的区域-B中核对五个孔。区域-B的LWD和羽毛效果有助于了解克里希纳 - 河东盆地序列地层的地质意义,并确定了天然气水合物的发生。本研究总结了区域-B中的log-和litho-obs,并根据核心对数集成建立三个集成单位。大多数井下日志和核心推断的天然气水合物发生在后期内联综合单元B中,几套储层部分表现出托管天然气水合物的有利条件。鉴定了与反射器R1和R2相关的气体水合物储存器,并且R1储存器的特征在于骨折和孔隙气体水合物,并且R2在富含孔填充气体水合物处于高饱和的气体水合物中的富含砂性沉积物。与R1和R2相关联的厚度变化可能与显影的抗线结构相关联,并且可能与折叠结构的同步生长有关。在BSR深度附近的R1和R2附近存在主要气体水合物区,并且主要与裂缝和大规模运输沉积物重合。 R1和R2储存器中天然气水合物的空间分布受到抗冲击结构的高度影响。本研究可被视为未来的天然气水合物研究和附近地区的探索案例。

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