Energy Balance From a Mantle Pseudotachylyte, Balmuccia, Italy

机译：来自披风的能量平衡，意大利帕梅西亚

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Abstract > In the Balmuccia massif (NW Italy), a pseudotachylyte vein network (N068 trending) in a spinel lherzolite is interpreted as the product of frictional melting during a single <fi>M</fi> <sub> <fi>w</fi> </sub> ?>?6 earthquake. The subvertical fault underwent a metric dextral coseismic displacement, raking 60°SW. The average width of the main slip surface is type="mathematics">~ ?5?mm. A dense network of thin (20–200?μm) injection and ultramylonite‐like veins decorates the fault walls. In the injection veins, Raman microspectrometry mapping reveals pockets of still preserved amorphous silicate, containing ≈?1% of structurally bound H <sub>2</sub> O. In the ultramylonite‐like veins, electron backscattered diffraction mapping reveals that ultrafine (0.2–2?μm) olivine grains exhibit a strong fabric with (010) planes parallel to shearing, consistent with temperatures above 1250°C during deformation and suggesting fast recrystallization from the frictional melt. The veins also exhibit pyroxene and recrystallized spinel, which proves that the earthquake occurred at a minimum depth of 40?km. The energy balance demonstrates that complete fault lubrication must have occurred during coseismic sliding (i.e., dynamic friction coefficient ??0.1). Because of the low viscosity of slightly hydrated ultramafic liquids (≈?1?Pa·s), we argue that lubrication was only transient, as the melt could rapidly flow into tensile fractures, which led to rapid cooling and promoted strength recovery and sliding arrest. Combined together, our observations suggest that this pseudotachylyte is the frozen record of a deep (>40?km) earthquake of 6?<? <fi>M</fi> <sub> <fi>w</fi> </sub> ?<?7. Its focal mechanism is deduced from the crystal preferred orien </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> >在Balmuccia Massif（NW Italy），一个假静脉静脉网络（N068趋势）尖晶石LherzoLite被解释为摩擦熔化在单个<fi> m </ fi> <sub> <fi> w </ fi> </ sub>？> 6地震期间的产物。复杂故障接受了公制的右旋电动发电机，耙60°SW。主滑动表面的平均宽度是<跨度型=“数学”>〜</ span>？5？mm。密集的薄（20-200？μm）注射和ultramylonite样静脉装饰故障墙。在注射静脉中，拉曼微穴位测绘揭示仍然保存的无定形硅酸盐的口袋，含有≈α1％的在结构上结合的H <sub> 2℃。在亚超散纹静脉中，电子背散射衍射映射显示超细（ 0.2-2αμm）橄榄石晶粒表现出具有平行于剪切的（010）平面的强织物，在变形期间与1250℃高于1250℃的温度，并表明从摩擦熔体的快速重结晶。静脉还表现出辉石和再结晶的尖晶石，证明地震发生在最小深度为40 km。能量平衡表明，在电动发射滑动期间必须发生完全故障润滑（即动态摩擦系数？0.1）。由于略微水合的超空白液体的低粘度（≈α1≤Pa·s），我们认为润滑仅是瞬态的，因为熔体可以迅速流入拉伸骨折，这导致快速冷却和促进强度回收和滑动。结合在一起，我们的观察结果表明，这种假震性是6？<？ <fi> m </ fi> <sub> <fi> w </ fi> </ sub>？<？7。它的焦点机制从晶体首选的orien推导出来 </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25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=Ferrand Thomas P.&option=202" target="_blank" rel="nofollow">Ferrand Thomas P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Labrousse Lo?c&option=202" target="_blank" rel="nofollow">Labrousse Lo?c;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Eloy Grégoire&option=202" target="_blank" rel="nofollow">Eloy Grégoire;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fabbri Olivier&option=202" target="_blank" rel="nofollow">Fabbri Olivier;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hilairet Nadège&option=202" target="_blank" rel="nofollow">Hilairet Nadège;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schubnel Alexandre&option=202" target="_blank" rel="nofollow">Schubnel Alexandre;</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>Laboratoire de Géologie – UMR 8538 CNRS Ecole Normale SupérieurePSL★ Research UniversityParis France;</p> <p>Institut des Sciences de la Terre de Paris – UMR 7193 CNRSUniversité Pierre et Marie CurieParis France;</p> <p>Laboratoire de Géologie – UMR 8538 CNRS Ecole Normale SupérieurePSL★ Research UniversityParis France;</p> <p>Laboratoire Chrono‐environnement – UMR 6249 CNRSUniversité Bourgogne – Franche‐ComtéBesan?on France;</p> <p>Univ. Lille CNRS INRA ENSCL UMR 8207 ‐ UMET ‐ Unité Matériaux et TransformationsLille France;</p> <p>Laboratoire de Géologie – UMR 8538 CNRS Ecole Normale SupérieurePSL★ Research UniversityParis France;</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=pseudotachylyte&option=203" rel="nofollow">pseudotachylyte;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle&option=203" rel="nofollow">mantle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake&option=203" rel="nofollow">earthquake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=high‐pressure fault&option=203" rel="nofollow">high‐pressure fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=energy balance&option=203" rel="nofollow">energy balance;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Balmuccia&option=203" rel="nofollow">Balmuccia;</a> </p> <div class="translation"> 机译：假静置;地幔;地震;高压故障;能量平衡;BALMUCCIA; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025592434.html">Energy Balance From a Mantle Pseudotachylyte, Balmuccia, Italy</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ferrand Thomas P.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ferrand Thomas P.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Labrousse Lo?c&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Labrousse Lo?c,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Eloy Grégoire&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Eloy Grégoire,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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