土耳其东部东安纳托利亚断裂带运动学及其地震构造意义

Aylin Tan, H. Eyidog̃an
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引用次数: 0

摘要

东安纳托利亚断裂带(East Anatolian Fault Zone, EAFZ)是土耳其东部最突出和活跃的断层之一,其长度约为500 km。在这项研究中,我们从2006年以来在TURDEP项目内的断裂带周围建立的34个三维宽带地震台站的记录中获得了EAFZ最近的地震活动性。进一步研究了土耳其东部EAFZ的地震活动性和断层机制解。除了先前公布的220次震级≥2.0的地震外,新的断层机制解是由局部矩张量解和纵波第一运动数据确定的。认为特科格鲁以南的鄂西断裂带最近的构造变形是由Amik盆地和Adana盆地之间的左旋走滑活动断裂承担的,年轻的反拉应力也很活跃。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Kinematics of the East Anatolian Fault Zone, Eastern Turkey and Seismotectonic Implications
One of most prominent and active faults in Eastern Turkey is the NE-SW oriented left-lateral strike-slip East Anatolian Fault Zone (EAFZ) with a length of approximately 500 km. In this study, we have examined the recent seismicity of EAFZ that was obtained from the records of 34 three-dimensional broad-band earthquake stations established around the fault zone within TURDEP project since 2006. Further the seismicity and fault mechanism solutions of EAFZ, Eastern Turkey have been examined. The new fault mechanism solutions in addition to previously published 220 earthquakes, with a magnitude of M L =2.0 or more were determined by a local moment tensor solution and P-wave first motion data. It was suggested that the recent tectonic deformation of EAFZ south of Turkoglu was taken up by the left-lateral strike-slip active faults in between Amik and Adana Basins were young trans-tensional stress regime was also active.
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