...
首页> 外文期刊>Journal of the Geological Society of India >First Active Fault Exposure Identified along Kachchh Mainland Fault: Evidence from Trench Excavation near Lodai Village, Gujarat, Western India
【24h】

First Active Fault Exposure Identified along Kachchh Mainland Fault: Evidence from Trench Excavation near Lodai Village, Gujarat, Western India

机译:沿着卡奇大陆断裂确定了首次活动断层暴露:来自印度西部古吉拉特邦洛代村附近沟槽发掘的证据

获取原文
获取原文并翻译 | 示例
           

摘要

We report first identified active fault exposure from Kachchh region along the Kachchh Mainland Fault (KMF) other than the 1819 Allah Bund earthquake,. The active fault scarps striking E-W were identified near Lodai village along KMF, North facing scarps with height from 10-15 m are the manifestation of the displaced alluvial fan surface along this fault Occurrence of discontinuous linear mound ranging in height from 3-5 m aligned along the strike about 100 m north of the main scarp are suggestive of younger tectonic movement and progressive shift of tectonic activity towards north along new imbricated fault Three low to high angle reverse fault strands (Fl, F2 and F3) displacing young Quaternary deposits (late Pleistocene-Holocene?) classified as A to F units comprising gravel and sand-silt fades were identified in a trench excavated at the base of the linear mound along KMF Our preliminary observations revealed occurrence of at least two large magnitude earthquakes along the F3 fault, and may be older events along the Fl and F2, Latest event (Event-I) occurred along F3 after the deposition of unit B registering the displacement of -33 cm, penultimate event (Event-II) occurred after the deposition of unit C with -40 cm of displacement. The maximum displacement of about 73 cm along F3 indicates cumulative displacement accommodated during more than one event. The total displacement of -98 cm along F2 strand displacing the E and F units is the result of more than one event, and since the F2 probably displaced the unit C suggests that the movements occurred during penultimate (Event II) and during the Event III, older than penultimate,. Displacement of Mesozoic succession during older events and unit B during the latest Event I along Fl suggests repetitive movement along this fault The fragile nature of -3-4 m wide shear zone formed in Mesozoic rocks (shale+sandstone) also point towards repetitive tectonic movement along KMF.
机译:我们报告了除了1819年阿拉德外滩地震以外,沿着卡奇大陆断裂(KMF)沿卡奇地区首次发现的活动断层。在肯尼迪沙漠附近的洛代村附近发现了活动的EW断裂断层,北向的断层高度为10-15 m,是沿着该断层错位的冲积扇面的表现。高度为3-5 m的不连续线性丘发生沿主要断层以北约100 m的走向,暗示了年轻的构造运动和构造活动沿着新的盘状断层向北逐渐移动的趋势。三个低至高角度的反向断层股线(F1,F2和F3)取代了年轻的第四纪沉积(晚期)。在沿KMF的线性土墩底部开挖的沟槽中发现了分类为A至F的包括砾石和粉砂淤泥褪色的更新世-全新世?并且可能是沿F1和F2的较早事件,最新事件(Event-I)沿F3发生在单元B沉积后记录了-的位移33 cm,倒数第二个事件(事件II)发生在单元C沉积-40 cm位移之后。沿着F3的最大位移约为73厘米,表明在一个以上的事件中累积了位移。沿着F2链移动E和F单元的总位移-98 cm是一个以上事件的结果,并且由于F2可能移动了C单元,因此表明运动发生在倒数第二个(事件II)和事件III期间,比倒数第二大。在较早的事件中中生代演替的位移和在Fl上的最新事件I中的B单元的位移表明沿着该断层的重复运动。中生代岩石(页岩+砂岩)中形成的-3-4 m宽剪切带的脆弱性质也表明了重复的构造运动。沿着KMF。

著录项

相似文献

  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号