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Magnetotelluric studies in the epicenter zone of 2001, Bhuj earthquake

机译:布吉地震2001年震中区的大地电磁研究

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摘要

Some earthquakes to Mw5 level are occurring along two faults viz. Kachchh Mainland Fault and South Wagad Fault near the epicenter of Mw7.7 Bhuj earthquake of 2001. These faults are not the causative fault of the 2001 earthquake and suspect for future large earthquake. In absence of detail geophysical surveys, the sub-surface orientation of these faults was not known and MT profiles have proved useful in delineating the subsurface trends. Two MT profiles having lengths of 24 km and 15 km (with an inter station spacing of 1-3 km) are taken about 10 km east and west of the epicenter of Mw7.7, 2001 Bhuj earthquake, respectively. The profiles are in nearly N-S direction to detect the faults which trend E-W in the area. From 2-D inversion of MT data of 23 stations, it is found that there are two distinctive conductive features matching with the South Wagad Fault and Kachchh Mainland Fault south of it both being about 10 km apart. The South Wagad Fault is seen extending to Banni low lying area 30 km west of the present trace.
机译:沿着两个断层即Mw5级发生了一些地震。 2001年普吉7.7级地震震中附近的卡奇大陆断裂和南瓦加德断裂。这些断裂不是2001年地震的成因,并且可能会引起未来的大地震。在缺乏详细的地球物理勘测的情况下,这些断层的地下方向是未知的,并且MT剖面已被证明可用于描述地下趋势。分别在2001年普杰Mw7.7地震震中中心以东和以西约10 km处拍摄了两个长度分别为24 km和15 km(站间间距为1-3 km)的MT剖面。这些剖面几乎在N-S方向上,以检测在该地区趋于E-W的断层。从23个台站的MT数据进行二维反演,发现有两个与南瓦格德断层和南部的Kachchh大陆断层相匹配的导电特征,两者相距约10 km。可以看到南瓦加德断层延伸到本迹以西30公里处的班尼低洼地区。

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