HVSR微震法在占壁丹戎Batu玄武岩露头的应用

H. Mz, Surya Bakti Rangkuti
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引用次数: 1

摘要

在南苏门答腊弧后盆地丹中巴图露头火成岩周围采集了15点的微震数据,类似于在占碑次盆地进行的微震数据。该地区发现的火成岩为玄武岩,分布于±825 Ha,位于Desa Tanjung Batu Geragai Jambi。这个露头的独特之处在于它侵入了厚达1000多米的沉积岩,位于苏门答腊岛东部,远离火山。1-11和15测点的固有频率在6 Hz-19 Hz之间变化。1-10和15测点的放大值在0.8 Hz- 2.2 Hz之间变化,但测点4和11的放大值在3.4 Hz和4.8 Hz之间变化。1-10和15测点的地震易损性变化范围为0.8 - 1.8。但4点和11点的地震易损性值为1,4和2,3。根据这些结果,露头的固有频率、放大和地震易损性在各图中具有对比值,可识别为玄武岩侵入断层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Application of the HVSR Microtremor Method for Basalt Outcrops in Tanjung Batu, Jambi
Microtremor data at 15 point had been taken at tanjung batu around of outcrop igneous rock in back arc basin South Sumatra such as carried out at sub basin Jambi. The igneous rock, which is found in this area, is basalt and distributed in ± 825 Ha and located in Desa Tanjung Batu Geragai Jambi. The uniqueness of this outcrop is it intrudes the thick of sedimentary rock which have the thickness around more than 1000 meter, located in east cost of Sumatera Island and far away from the volcanoes. The natural frequency from 1-11 and 15 measurement point varied from 6 Hz-19 Hz. The amplification value from 1-10 and 15 measurement point varied from 0,8 Hz-2,2Hz, but at points 4 and 11 have amplification value from 3,4 Hz and 4,8 Hz. Seismic vulnerability at 1-10 and 15 measurement point varied from 0,8-1,8. but at points 4 and 11 have seismic vulnerability value from 1,4 and 2,3. From these result of natural frequency, amplification, and Seismic vulnerability in the outcrops have contrasting value in each map can be identified as fault from intrusion of basalt.
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