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首页> 外文期刊>Journal of Metamorphic Geology >The great eclogite debate of the Western Gneiss Region, Norwegian Caledonides: The in?situ crustal vv . exotic mantle origin controversy
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The great eclogite debate of the Western Gneiss Region, Norwegian Caledonides: The in?situ crustal vv . exotic mantle origin controversy

机译：诺威士州西康涅狄格州西方片兰德的伟大eClogite辩论：IN？原位点壳 v v。 异国情调的地幔争论争议

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Abstract > An entertaining debate arose in the latter half of the 20th century among scientists working on the spectacular eclogite facies rocks that occur within metamorphic rocks of the Western Gneiss Region (WGR) of the Norwegian Caledonides. It resulted in part from Eskola's influential publication “On the Eclogites of Norway” who concluded, incorrectly, that mafic eclogites within gneisses (external eclogites) and garnetiferous ultramafic rocks within peridotite lenses had a common origin. The debate featured two end‐member positions. One was that all these garnet‐bearing assemblages, regardless of association, had an exotic origin, where they recrystallized at extremely high pressures and temperatures ( P – T ) in the mantle and then were tectonically inserted upward into the crust. The other was the in?situ origin where this recrystallization occurred within the enclosing gneisses during regional metamorphism. Garnet peridotites and pyroxenites have compositions identical to ultramafic xenoliths in kimberlites and define P – T conditions that are appropriate to the upper mantle. Therefore, peridotite lenses were generally (and correctly) interpreted to be mantle fragments. However, some extended this exotic origin to external eclogites, particularly coarse‐grained orthopyroxene‐ (and coesite‐) bearing eclogites, which also formed at extremely high P – T . They noted an apparent pressure and temperature disequilibrium between anhydrous eclogites and the surrounding amphibolite facies gneisses. It was generally accepted that eclogites could form only in “dry” environments ( <mat:math xmlns:mat="http://www.w3.org/1998/Math/MathML" alti </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 XMLNS =“http://www.wiley.com/namespaces/wiley”type =“main”xml：id =“jmg12314-abs-0001”xml：lang =“en”> <title type =“main” >摘要</ title> >在20世纪的后一半的科学家们在营养壮观的eClogite面部岩石中摇滚的科学家们在挪威奶酪群岛西部（WGR）的变质岩中，这是一个有趣的辩论。它有部分来自Eskola的影响出版物“挪威的eGlogites”，他们在不正确的情况下得出结论，不正确的神火（外部eNlogites）中的乳头肠道和椭圆形镜片内的Garnetifien ultramfiC岩石的爆发症具有共同的起源。争论精选了两个最终成员职位。一个是，无论关联如何，所有这些装有的石榴石组件都具有异国情调的起源，在那里在地幔中以极高的压力和温度（ P </ i> - t </ i>）重结晶然后将向上插入地壳中。另一个是in？原位原产地，其中在区域变质期间发生这种重结晶在封闭的外茎内。石榴石终极性和辉兴纤维具有与金伯利岩中的超微XenoLiths相同的组合物，并限定适合于上部地幔的 P </ i>的条件。因此，恒星透镜通常（并且正确地）被解释为披风碎片。然而，一些将这种外来源性延伸到外部eGlogites，特别是粗粒胚层 - （和基氏岩）轴承的eClogites，其也形成在极高的 P“ - T”。他们注意到无水eClogites和周围的倒置锥形面形状的表观压力和温度不平衡。普遍认为，eClogites只能在“干燥”环境中形成（<mat：math xmlns：mat =“http://www.w3.org/1998/math/mathml”Alti </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-35076/'>《Journal of Metamorphic Geology》</a> <b style="margin: 0 2px;">|</b><span>2018年第5期</span><b style="margin: 0 2px;">|</b><span>共11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=Brueckner Hannes K.&option=202" target="_blank" rel="nofollow">Brueckner Hannes K.;</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>Lamont–Doherty Earth Observatory of Columbia UniversityPalisades New York;</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/165.html" title="地质学">地质学;</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=continental subduction&option=203" rel="nofollow">continental subduction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=eclogite&option=203" rel="nofollow">eclogite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=garnet peridotite&option=203" rel="nofollow">garnet peridotite;</a> </p> <div class="translation"> 机译：大陆俯冲;eClogite;石榴石洋光石; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025659564.html">The great eclogite debate of the Western Gneiss Region, Norwegian Caledonides: The in?situ crustal <i xmlns="http://www.wiley.com/namespaces/wiley">vv . exotic mantle origin controversy</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Brueckner Hannes K.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Brueckner Hannes K. </a> <a href="/journal-foreign-35076/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Metamorphic Geology .</a> <span>2018</span><span>,第5期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：诺威士州西康涅狄格州西方片兰德的伟大eClogite辩论：IN？原位点壳<i xmlns =“http://www.wiley.com/namespaces/wiley”> v </ i> v。 异国情调的地幔争论争议</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704020203489.html">Abnormal polar nanoregion evolution in (Bi <sub xmlns="http://www.wiley.com/namespaces/wiley">0.09</sub>0.09 Ba <sub xmlns="http://www.wiley.com/namespaces/wiley">0.91</sub>0.91 )(Zn <sub xmlns="http://www.wiley.com/namespaces/wiley">0.045</sub>0.045 Ti <sub xmlns="http://www.wiley.com/namespaces/wiley">0.955</sub>0.955 )O <sub xmlns="http://www.wiley.com/namespaces/wiley">3</sub>3 (9BZT‐BT) ceramic</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shi Jing&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Shi Jing,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cui Naiyuan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Cui Naiyuan,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Xiaoli&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wang Xiaoli,</a> <a href="/journal-foreign-29289/" target="_blank" rel="nofollow" class="tuijian_authcolor">Physica status solidi, B. 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