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Preliminary Results of Characteristic Seismic Anisotropy Beneath Sunda-Banda Subduction-Collision Zone

机译:SUNDA-BANDA郊区碰撞区中特征地震各向异性的初步结果

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Determining of seismic anisotropy allowed us for understanding the deformation processes that occured in the past and present. In this study, we performed shear wave splitting to characterize seismic anisotropy beneath Sunda-Banda subduction-collision zone. For about 1,610 XKS waveforms from INATEWS-BMKG networks have been analyzed. From its measurements showed that fast polarization direction is consistent with trench-perpendicular orientation but several stations presented different orientation. We also compared between fast polarization direction with absolute plate motion in the no net rotation and hotspot frame. Its result showed that both absolute plate motion frame had strong correlation with fast polarization direction. Strong correlation between the fast polarization direction and the absolute plate motion can be interpreted as the possibility of dominant anisotropy is in the asthenosphere..
机译:确定地震各向异性允许我们了解过去和现在发生的变形过程。在这项研究中,我们进行了剪力波分裂,以表征Sunda-Banda郊区碰撞区下的地震各向异性。已经分析了来自Inatews-BMKG网络的大约1,610个XKS波形。从其测量结果表明,快速偏振方向与沟槽垂直取向一致,但几个站呈现不同的取向。我们还在NO净旋转和热点框架中具有绝对板运动的快速偏振方向之间。其结果表明,两个绝对板运动框架与快速偏振方向具有很强的相关性。快速偏振方向与绝对板运动之间的强关系可以被解释为主导各向异性的可能性是在近距离圈中。

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