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The Konya earthquakes of 10–11 September 2009 and soil conditions in Konya, Central Anatolia, Turkey

机译:2009年9月10日至11日的Konya地震和土耳其中央安纳托利亚科尼亚的土壤条件

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Earthquakes registering magnitudes Md = 4.5 and 4.7 struck the city of Konya, Central Anatolia, on 10–11 September 2009, causing very slight damages. The earthquake epicenters were located at the east of Sille District along the Konya Fault Zone, a dip-slip fault. The nature and seismicity of the fault zone indicates that it is capable of producing earthquakes of moderate magnitudes. This paper summarizes the geologic data along the fault zone and documents groundwater conditions and analyzes borehole and geotechnical data of the Konya city. The residential area of the city covers an area of approximately 1150 square kilometers and consists almost entirely of flat land except for a small part of rugged land in the southwestern corner. Groundwater and geotechnical data were collected and analyzed to evaluate the liquefaction potential of deposits under the Konya city. This preliminary investigation indicates that areas for liquefaction are generally limited to the eastern and east central parts of the city.
机译:地震登记量大MD = 4.5和4.7袭击了2009年9月10日至11日,安纳托利亚市科尼亚市袭击了科尼亚市,造成了非常轻微的损害。地震震中位于沿Konya断层区的锡尔斯区东部,浸式拖放故障。故障区的性质和地震性表明它能够产生中等大小的地震。本文总结了沿着故障区的地质数据和文档地下水条件,分析了Konya城市的钻孔和岩土资料。该市的住宅区占地面积约1150平方公里,几乎完全由平坦的土地组成,除了西南角落里的一小部分崎岖的土地。收集地下水和地土科数据,并分析,评价Konya市下矿床的液化潜力。这种初步调查表明液化领域通常限于城市的东部和东部地区。

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