首页> 外文期刊>Journal of Asian earth sciences >Three-dimensional seismic velocity imaging of the Kachchh rift zone, Gujarat, India: Implications toward the crustal mafic pluton induced intraplate seismicity
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Three-dimensional seismic velocity imaging of the Kachchh rift zone, Gujarat, India: Implications toward the crustal mafic pluton induced intraplate seismicity

机译:印度古吉拉特邦Kachchh裂谷带的三维地震速度成像:对地壳镁铁质岩体诱发板内地震活动的影响

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摘要

Three-dimensional tomographic images of seismic velocities have been constructed for the 2001 M-w 7.7 Bhuj earthquake region using data from a dense 58-station seismograph network, during 2001-16. Two distinct, prominent high-velocity anomalies (10-14% increase in Vp and Vs, and 10-11% decrease in Vp/Vs) have been mapped at 2-40 km depths below the Banni and Wagad uplift regions, which could be attributed to mafic plutons. We also image several high-velocity zones (intrusive mafic rocks) and some low-velocity patches (meteoric water/metamorphic fluids/volatile CO2) within the main rupture zone of the 2001 Bhuj earthquake, where maximum confinement of seismicity is noticed. We propose that stresses induced by mafic plutons in response to the N-S compression of the Indian plate might have resulted in a stress regime near to critical for thesub-parallel rift associated fault system within the main rupture zone, thereby, generating small to large earthquakes through small stress perturbations caused by crustal fluid flows and stress transfer.
机译:使用2001-16年期间密集的58站地震仪网络的数据,为2001 M-w 7.7布吉地震区构建了地震速度的三维断层图像。在Banni和Wagad隆升区以下2-40 km的深度处绘制了两个不同的,显着的高速异常(Vp和Vs分别增加10-14%,Vp / Vs减少10-11%)。归因于黑手党的plutons。我们还对2001年布吉地震的主要破裂带内的几个高速带(侵入性铁镁质岩)和一些低速斑片(流水/变质流体/挥发性CO2)进行了成像,其中地震活动受到最大限制。我们认为,铁镁质岩体响应印度板块的NS压缩而引起的应力可能已导致对主破裂带内次平行裂谷相关断层系统接近临界的应力状态,从而通过由地壳流体流动和应力传递引起的较小的应力扰动。

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