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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Interpreting Granitic Fabrics in Terms of Rhyolitic Melt Segregation, Accumulation, and Escape Via Tectonic Filter Pressing in the Huemul Pluton, Chile
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Interpreting Granitic Fabrics in Terms of Rhyolitic Melt Segregation, Accumulation, and Escape Via Tectonic Filter Pressing in the Huemul Pluton, Chile

机译：在智利Huemul芦苇中压制压网熔体偏析，积累和逃逸方面解释花岗岩织物。

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Abstract > The physical process of rhyolite segregation from crystal mushes remains elusive as microstructural evidence of conventional segregation mechanisms is not available. This study provides direct fabric evidence for deformation‐assisted segregation of eruptible rhyolite in the Chilean Andean arc. The shallow (7?km), 6.4–6.2?Ma Huemul pluton comprises domains of quartz monzonite , granite , and high‐silica granite . Compositional modeling shows that rhyolitic melt ( high‐silica granite ) was extracted from a granitic parent, leaving behind silicic cumulates ( quartz monzonite ). To understand mechanisms of rhyolite segregation, we investigate magmatic fabrics in the pluton. Anisotropy of Magnetic Susceptibility analyses reveal oblate magnetic fabrics and NNW‐striking, subvertical magnetic foliations throughout Huemul. Within the high‐silica granite , magnetic lineations are subvertical and parallel to elongate miarolitic cavities. Magnetic lineations in the quartz monzonite plunge moderately to the NNW, away from the high‐silica granite . In the quartz monzonite , the Shape‐Preferred Orientation of early feldspars is parallel to the magnetic lineation and developed while suspended in melt. Estimations of early feldspar clustering and crystallinity yield ~38% of interstitial volume loss in the quartz monzonite and no volume loss in the granite . These fabric data suggest ENE tectonic shortening coeval with rhyolite extraction. We explain these observations with a model of tectonic filter pressing in which shortening is accommodated by interstitial melt flow at slow (10 ?5</sup </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”>摘要</标题> >从晶体糊状物的水流石偏析的物理过程仍然难以捉摸，因为传统隔离机制的微观结构证据是难以捉摸无法使用。本研究为智利Andean弧中的可爆发菱形的变形辅助分离提供了直接的织物证据。浅（＆7Ωkm），6.4-6.2？ma huemul pluton包括石英蒙扎钛矿的结构域，花岗岩</ i>，和高二氧化硅花岗岩</ i >。组合模拟表明，从花岗母母细胞中萃取卟啉熔体（高二氧化硅花岗岩），留下硅累积（ Quartz monzonite </ i）。为了理解流纹岩隔离的机制，我们研究了芦苇的岩浆织物。磁性敏感性分析的各向异性揭示了恒定磁性织物和NNW引人注目的摇头型，摇头。在高二氧化硅花岗岩中，磁性线eations是混合的，平行于细长的米星腔。磁性基氨酸在石英蒙扎钛矿中适度地进入NNW，远离高二氧化硅花岗岩</ i>。在 Quartz monzonite </ i>中，早期长度的形状优选的取向平行于磁性线聚氨酸，并在熔体中悬浮而开发。早期长石聚类和结晶度产率的估计〜38％的间质体积损失在石英岩岩中的</ i>在花岗岩中没有体积损失</ i>。这些织物数据表明了eNE构造缩短符合细胞纹提取。我们用慢性熔体流动慢（10 5 </ sup </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10期</span><b style="margin: 0 2px;">|</b><span>共20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=Garibaldi Nicolas&option=202" target="_blank" rel="nofollow">Garibaldi Nicolas;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tikoff Basil&option=202" target="_blank" rel="nofollow">Tikoff Basil;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schaen Allen J.&option=202" target="_blank" rel="nofollow">Schaen Allen J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Singer Brad S.&option=202" target="_blank" rel="nofollow">Singer Brad S.;</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>Department of GeoscienceUniversity of Wisconsin‐MadisonMadison WI USA;</p> <p>Department of GeoscienceUniversity of Wisconsin‐MadisonMadison WI USA;</p> <p>Department of GeoscienceUniversity of Wisconsin‐MadisonMadison WI USA;</p> <p>Department of GeoscienceUniversity of Wisconsin‐MadisonMadison WI USA;</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=granitic fabrics&option=203" rel="nofollow">granitic fabrics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rhyolite segregation&option=203" rel="nofollow">rhyolite segregation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tectonic filter pressing&option=203" rel="nofollow">tectonic filter pressing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magmatic arc&option=203" rel="nofollow">magmatic arc;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=AMS&option=203" rel="nofollow">AMS;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=SPO&option=203" rel="nofollow">SPO;</a> </p> <div class="translation"> 机译：花岗岩织物;流石岩隔离;构造滤波器压缩;魔术弧;ams;opo; 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