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Marine Volcaniclastic Record of Early Arc Evolution in the Eastern Ritter Range Pendant, Central Sierra Nevada, California

机译：东部Ritter Range吊坠早期弧形演进的海洋火山 - 中央塞拉尼达，加利福尼亚州

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Abstract >Marine volcaniclastic rocks in the Sierra Nevada preserve a critical record of silicic magmatism in the early Sierra Nevada volcanic arc, and this magmatic record provides precise minimum age constraints on subduction inception and tectonic evolution of the early Mesozoic Cordilleran convergent margin at this latitude. New zircon Pb/U ages from the Ritter Range pendant and regional correlations indicate arc inception no later than mid‐Triassic time between 37°N and 38°N. The regional first‐order felsic magma eruption rate as recorded by marine volcanic arc rocks was episodic, with distinct pulses of ignimbrite emplacement at ca. 221–216 and 174–167 Ma. Ignimbrites range from dacite to rhyolite in bulk composition, and are petrographically similar to modern arc‐type, monotonous intermediate dacite or phenocryst‐poor, low‐silica rhyolite. Zircon trace element geochemistry indicates that Jurassic silicic melts were consistently Ti‐enriched and light rare earth‐enriched and U‐depleted in comparison to Triassic melts of the juvenile arc, suggesting Jurassic silicic melts were hotter, drier, and derived from distinct lithospheric sources not tapped in the juvenile stage of arc construction. Pulses of ignimbrite deposition were coeval with granodioritic to granitic components of the underlying early Mesozoic Sierra Nevada batholith, suggesting explosive silicic volcanism and batholith construction were closely coupled at 1–2 million‐year time scales. </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> >塞拉尼达的海洋火山岩岩石在早期的塞拉尼达火山弧中保护了硅岩岩石的批判性记录，这座岩浆记录为这一纬度的早期中生代科特里兰收敛余量的俯冲初始化和构造演变提供了精确的最低龄限制。来自Ritter Range吊坠和区域相关性的新锆石PB / U老年表示不迟于37°N和38°N之间的中三叠级时间的弧形成立。海洋火山岩岩石岩石记录的区域一流的猫咪岩浆爆发率是剧目的，在加利福尼亚州的Ignimbrite施加明显脉冲。 221-216和174-167 MA。 Ignimbrites系列从甲板到块状组成中的菱形，并且岩体类似于现代弧形，单调中间粘土或苯杂交差，低二氧化硅流纹岩。锆石痕量元素地球化学表明，与少年弧的三叠纪熔体相比，侏罗纪硅熔体始终如一的富含富含Ti富含的富含稀土和U-耗尽，表明侏罗纪硅熔体更热，干燥剂，并来自不同的岩石熔体，并来自不同的岩石熔池在弧形施工的少年阶段中挖掘。 Ignimbrite沉积的脉冲与鳞状细胞到底层中生代塞拉尼亚斯拉斯拉内华达山脉的花岗岩成分，暗示爆炸性的硅藻和浴池建设在1-2百万年的时间尺度上密切联系。</ p> </摘要> </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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2018年第8期</span><b style="margin: 0 2px;">|</b><span>共17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=Barth A. P.&option=202" target="_blank" rel="nofollow">Barth A. P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wooden J. L.&option=202" target="_blank" rel="nofollow">Wooden J. L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Riggs N. R.&option=202" target="_blank" rel="nofollow">Riggs N. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Walker J. D.&option=202" target="_blank" rel="nofollow">Walker J. D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tani K.&option=202" target="_blank" rel="nofollow">Tani K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Penniston‐Dorland S. C.&option=202" target="_blank" rel="nofollow">Penniston‐Dorland S. C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jacobson C. E.&option=202" target="_blank" rel="nofollow">Jacobson C. E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Laughlin J. A.&option=202" target="_blank" rel="nofollow">Laughlin J. A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hiramatsu R.&option=202" target="_blank" rel="nofollow">Hiramatsu R.;</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 Earth SciencesIndiana University‐Purdue University IndianapolisIndianapolis IN USA;</p> <p>U.S. Geological SurveyMenlo Park CA USA (retired);</p> <p>School of Earth Sciences and Environmental SustainabilityNorthern Arizona UniversityFlagstaff AZ USA;</p> <p>Department of GeologyUniversity of KansasLawrence KS USA;</p> <p>National Museum of Nature and ScienceTokyo Japan;</p> <p>Department of GeologyUniversity of MarylandCollege Park MD USA;</p> <p>Department of Earth and Space SciencesWest Chester UniversityWest Chester PA USA;</p> <p>Department of Earth SciencesIndiana University‐Purdue University IndianapolisIndianapolis IN USA;</p> <p>Department of Earth SciencesIndiana University‐Purdue University IndianapolisIndianapolis IN 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=sedimentary geochronology&option=203" rel="nofollow">sedimentary geochronology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=zircon geochemistry&option=203" rel="nofollow">zircon geochemistry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volcanic arcs&option=203" rel="nofollow">volcanic arcs;</a> </p> <div class="translation"> 机译：沉积地质学;锆石地球化学;火山弧; </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 >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360500.html">Marine Volcaniclastic Record of Early Arc Evolution in the Eastern Ritter Range Pendant, Central Sierra Nevada, California</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barth A. 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architecture comprising lateral extensions extending according to profile of propeller until ends of blades</a> <b>[P]</b> . <span> 外国专利： <!-- 法国专利： --> FR2915172A1 </span> <span> . 2008-10-24</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：潜艇潜水员使用的可操作螺旋桨，具有包围中央结构的半壳体，内部结构包括根据螺旋桨轮廓延伸直至叶片末端的横向延伸部分 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023360500','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div 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