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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >The Seismic History of the Pisia Fault (Eastern Corinth Rift, Greece) From Fault Plane Weathering Features and Cosmogenic 3636 Cl Dating
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The Seismic History of the Pisia Fault (Eastern Corinth Rift, Greece) From Fault Plane Weathering Features and Cosmogenic 3636 Cl Dating

机译：来自断层型风化特征和宇宙原性的PISIA故障（东康森特裂谷，希腊）的地震史和宇宙原性 36 36 cl约会

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Abstract > The deformation of the eastern Corinth rift (Greece) is distributed along several E‐W trending active normal faults. Here the 25‐km‐long Pisia fault experienced up to 150?cm of coseismic displacement during the 1981 Alkyonides earthquake sequence ( M ?=?6.7, 6.4, 6.3). Using terrestrial laser scanning, coupled with analyses of color changes, lichen colonization, and karstic features, we identify differentially weathered horizontal stripes on the exposed Pisia fault plane. The stripe boundaries occur at scarp heights of 1.10, 2.05, 2.85, 3.60, 4.15, and 5.15?m, with two additional possible boundaries at 3.10 and 4.65?m (~±0.1?m, respectively). This indicates that six to eight paleoearthquakes have exhumed the fault plane in a series of distinct coseismic slip events. A vertical profile of cosmogenic 36 Cl measurements is used to constrain age models of the exhumation. The results imply that, in addition to the last earthquake of 1981 (EQ1), exhumation events occurred at ~2.0?kyr (EQ2), ~3.1?kyr (EQ3), ~4.5?kyr (EQ4/4a,b), ~6.0?kyr (EQ5), and ~7.3?kyr (EQ6/6a,b), with modeled age uncertainties of ~0.7?kyr. Bayesian modeling provides a middle and late Holocene slip rate of 0.5–0.6?mm/yr (last 7.3?±?0.7?kyr), while the upper part of the 8.45‐m‐high fault plane was exhumed at a higher rate of 0.8–2.3?mm/yr (7.3?±?0.7?kyr to 10.2?±?1.9?kyr). This slip rate variability suggests an increased seismicity or larger slip events during the early Holocene. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >东康森特裂痕（希腊）的变形沿着几个e-w趋势活跃分发正常故障。在这里，在1981年烷基化地震序列（ m </ i> =Δ6.7,6.4,6.3）中，25公里长的PISIA故障经历了高达150？CM的电影位移。使用地面激光扫描，加上颜色变化，地衣殖民化和岩溶特征的分析，我们在暴露的PISIA断层平面上识别差异风化的水平条纹。条纹边界发生在1.10,2.05,2.85,3.60,4.15和5.15？m的围巾高度，分别为3.10和4.65Ω（分别为4.65Ω（分别为4.65）。这表明六到八个古老地震已经在一系列不同的电影滑动事件中挖掘了故障平面。轴上的垂直轮廓的轴上的 36 </ sup> cl测量用于约束送达的年龄模型。结果意味着，除了1981年的最后一个地震（EQ1）外，挖掘事件发生在〜2.0？Kyr（EQ2），〜3.1？Kyr（EQ3），〜4.5？kyr（Eq4 / 4a，b），〜 6.0？Kyr（EQ5），〜7.3？Kyr（EQ6 / 6A，B），模拟年龄不确定性为0.7 kyr。贝叶斯造型提供了0.5-0.6？mm / yr（最后7.3？±0.7？kyr）的中间和晚期的全新世滑率（最后7.3？±0.7 kyr），而8.45 m高断层平面的上部以0.8的更高速度膨胀-2.3？mm / yr（7.3？±0.7？kyr至10.2？±1.9？kyr）。这种滑动率变异性表明全新世时期的震荡或更大的滑动事件增加了。 </ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第5期</span><b style="margin: 0 2px;">|</b><span>共19页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mechernich Silke&option=202" target="_blank" rel="nofollow">Mechernich Silke;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schneiderwind Sascha&option=202" target="_blank" rel="nofollow">Schneiderwind Sascha;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mason Jack&option=202" target="_blank" rel="nofollow">Mason Jack;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Papanikolaou Ioannis D.&option=202" target="_blank" rel="nofollow">Papanikolaou Ioannis D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deligiannakis Georgios&option=202" target="_blank" rel="nofollow">Deligiannakis Georgios;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pallikarakis Aggelos&option=202" target="_blank" rel="nofollow">Pallikarakis Aggelos;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Binnie Steven A.&option=202" target="_blank" rel="nofollow">Binnie Steven A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dunai Tibor J.&option=202" target="_blank" rel="nofollow">Dunai Tibor J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Reicherter Klaus&option=202" target="_blank" rel="nofollow">Reicherter Klaus;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Institute of Geology and MineralogyUniversity of CologneK?ln Germany;</p> <p>Institute of Neotectonics and Natural HazardsRWTH Aachen UniversityAachen Germany;</p> <p>Institute of Neotectonics and Natural HazardsRWTH Aachen UniversityAachen Germany;</p> <p>Laboratory of Mineralogy and Geology Department of Natural Resources Development and Agricultural EngineeringAgricultural University of AthensAthens Greece;</p> <p>Laboratory of Mineralogy and Geology Department of Natural Resources Development and Agricultural EngineeringAgricultural University of AthensAthens Greece;</p> <p>Laboratory of Mineralogy and Geology Department of Natural Resources Development and Agricultural EngineeringAgricultural University of AthensAthens Greece;</p> <p>Institute of Geology and MineralogyUniversity of CologneK?ln Germany;</p> <p>Institute of Geology and MineralogyUniversity of CologneK?ln Germany;</p> <p>Institute of Neotectonics and Natural HazardsRWTH Aachen UniversityAachen Germany;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=bedrock normal fault&option=203" rel="nofollow">bedrock normal fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fault scarp analyses&option=203" rel="nofollow">fault scarp analyses;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=active fault&option=203" rel="nofollow">active fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=terrestrial laser scanning&option=203" rel="nofollow">terrestrial laser scanning;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=slip rate&option=203" rel="nofollow">slip rate;</a> </p> <div class="translation"> 机译：基岩正常故障;故障围巾分析;主动故障;陆地激光扫描;滑动率; 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