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Nature of methane gas hydrate BSR(Bottom Simulating Reflector) from elastic wave simulation

机译:来自弹性波模拟的甲烷气体水合物BSR(底部模拟反射器)的性质

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Methane gas hydrate studies have recentlyattracted attention due to their importance for significant naturalresource and the global tectonic and dynamic linkage of the earth.Free gas zone below a hydrate stability zone is also focused on asignificant reservoir of natural gas. Reflection seismic survey is aparticularly important method to detect the base of gas hydratestability zone as a BSR. Elastic wave simulations are carried outto understand the acoustic nature of methane gas hydrate BSR insediments. Two geological models are presented, and have beenused for computer simulations. According to the results, BSRsare recognized quite well anywhere at the BSR potentialboundaries, if low-velocity zone is present just beneath themethane gas hydrate layer. BSR amplitude is strong enough to berecognized in a seismic profile, but it should be paid dueattention for the interpretation of the phase and amplitude of BSR.
机译:甲烷天然气水合物研究由于其重要性对显着的天然源和地球的全球构造和动态连杆而言,甲烷天然气水合物研究近似存在。水合物稳定区下方的煤气区也集中在天然气的尽心可见的储层。 反射地震勘测是检测天然气疏水性区作为BSR的气体疏水性区基础的局部重要方法。 弹性波模拟进行了解甲烷气水合物BSR常见的声学性质。 提出了两个地质模型,并已被分发用于计算机模拟。 根据结果,BSRSARE在BSR潜在的任何地方都认识到,如果低速区仅存在甲乙烷气水合物层。 BSR幅度足以在地震剖面中被释放出来,但应对BSR的阶段和幅度的解释进行偿还。

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