首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >First seismic record for intra-arc strike-slip tectonics along the Liquine-Ofqui fault zone at the obliquely convergent plate margin of the southern Andes
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First seismic record for intra-arc strike-slip tectonics along the Liquine-Ofqui fault zone at the obliquely convergent plate margin of the southern Andes

机译:沿安第斯山脉南部倾斜收敛的板块边缘的Liquine-Ofqui断裂带的弧内走滑构造的首次地震记录

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摘要

A temporal seismic network recorded local seismicity along a 130 km long segment of the transpressional dextral strike-slip Liquine-Ofqui fault zone (LOFZ) in southern Chile. Seventy five shallow crustal events with magnitudes up to M-w 3.8 and depths shallower than 25 km were observed in an 11-month period mainly occurring in different clusters. Those clusters are spatially related to the LOFZ, to the volcanoes Chaiten, Michinmahuida and Corcovado, and to active faulting on secondary faults. Further activity along the LOFZ is indicated by individual events located in direct vicinity of the surface expression of the LOFZ. Focal mechanisms were calculated using deviatoric moment tensor inversion of body wave amplitude spectra which mostly yield strike-slip mechanisms indicating a NE-SW direction of the P-axis for the LOFZ at this latitude. The seismic activity reveals the present-day activity of the fault zone. The recent Mw 6.2 event near Puerto Aysen, Southern Chile at 45.4 degrees S on April 21, 2007 shows that the LOFZ is also capable of producing large magnitude earthquakes and therefore imposing significant seismic hazard to this region.
机译:时域地震网络记录了智利南部沿压转右旋走滑的利奎因-奥奎断裂带(LOFZ)130公里长段的局部地震活动。在11个月内观测到75个M-w 3.8级以下深度浅层地壳事件,主要发生在不同的类群中。这些群在空间上与LOFZ,火山Chaiten,Michinmahuida和Corcovado以及次要断层上的活动断层有关。沿着LOFZ的进一步活动由位于LOFZ表面表达直接附近的单个事件指示。使用体波振幅谱的偏斜矩张量反演来计算震源机制,其主要产生走滑机制,指示在该纬度下LOFZ的P轴的NE-SW方向。地震活动揭示了断层带的当前活动。 2007年4月21日,南智利南部艾森港附近发生的6.2级Mw事件,于2007年4月21日显示,该LOFZ也能够产生大地震,因此对该地区构成了重大地震危险。

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