Stratigraphy and provenance of forearc sequences in the Lichi Mélange, Coastal Range: Geological records of the active Taiwan arc‐continent collision

Chen Wen‐Huang; Huang Chi‐Yue; Yan Yi; Dilek Yildirim; Chen Duofu; Wang Ming‐Huei; Zhang Xinchang; Lan Qing; Yu Mengming

摘要

Abstract >The Lichi Mélange in the Coastal Range, eastern Taiwan, is considered as sheared forearc sequences. However, the age of these sequences is still uncertain, and their significance for the arc‐continent collision has been overlooked. Based on field surveys and micropaleontological analysis, four independent biostratigraphic units ranging from 8.5 to 3.0?Ma are discerned in the Lichi Mélange. These units are obviously older than the remnant forearc sequences in the east (3.4–1.2?Ma), supporting the interpretation that the Lichi Mélange arose from the shearing of the lower forearc basin sequences. The stratigraphy also suggests that the older forearc strata (8.5–3.4?Ma) were deformed and uplifted as a bathymetric high similar to the Huatung Ridge in the western North Luzon Trough by arcward back thrusting before 3.4?Ma, while sedimentation continued in the remnant forearc basin in the east during 3.4–1.2?Ma. The older forearc strata possess vitrinite reflectance values even lower than those of the remnant forearc sequences, which also supports that they were uplifted by back thrusting and therefore did not experience significant burial. Neodymium isotope analysis shows that the 8.5–6.4?Ma forearc sediments were sourced from both the volcanic arc and the accretionary prism, indicating the emergence of the accretionary prism within 8.5–6.4?Ma. It might have resulted from the underplating of thinned continental crust and provides a good time constraint for the onset of arc‐continent collision. The post 6.4?Ma forearc sediments were mainly derived from the accretionary prism, reflecting its constant uplift and large‐scale exposure. </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> >台湾东部沿海范围的LichiMélange被认为是剪切前臂序列。然而，这些序列的年龄仍然不确定，并且忽略了对弧形碰撞的重要性。基于现场调查和微燕麦族分析，在LichiMélange中，四个独立的生物数据学单位范围为8.5至3.0？MA被辨别出来。这些单位明显比东部的残余前臂序列（3.4-1.2？ma）显然是较大的，支持丽氏美的解释是从下前叉盆腔序列的剪切产生的解释。地层也表明，较旧的前臂地层（＆ 8.5-3.4？ma）被变形并升高，因为在3.4 ma之前通过arcward背推着Wastween Luzon槽的华尚山脉的碱基高，而沉淀继续在3.4-1.2的东西中，在东部的残余前臂盆。较旧的前臂地层具有甚至低于残余前臂序列的vitriinite反射值，这也支持它们被反射升高，因此没有经历重大埋葬。钕同位素分析表明，来自火山弧和增生棱镜的沉积物的沉积物，表明在8.5-6.4的＆lt中产生的棱镜的出现。由于薄薄的大陆地壳的底层可能导致了对弧形大陆碰撞的发作提供了一个很好的时光约束。第6.4篇？马队沉积物主要来自增生棱镜，反映其恒定的隆起和大规模暴露。</ 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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2017年第9期</span><b style="margin: 0 2px;">|</b><span>共29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=Chen Wen‐Huang&option=202" target="_blank" rel="nofollow">Chen Wen‐Huang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Chi‐Yue&option=202" target="_blank" rel="nofollow">Huang Chi‐Yue;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yan Yi&option=202" target="_blank" rel="nofollow">Yan Yi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dilek Yildirim&option=202" target="_blank" rel="nofollow">Dilek Yildirim;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Duofu&option=202" target="_blank" rel="nofollow">Chen Duofu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Ming‐Huei&option=202" target="_blank" rel="nofollow">Wang Ming‐Huei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Xinchang&option=202" target="_blank" rel="nofollow">Zhang Xinchang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lan Qing&option=202" target="_blank" rel="nofollow">Lan Qing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yu Mengming&option=202" target="_blank" rel="nofollow">Yu Mengming;</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>Key Laboratory of Ocean and Marginal Sea Geology Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>Key Laboratory of Ocean and Marginal Sea Geology Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>Key Laboratory of Ocean and Marginal Sea Geology Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>Department of Geology and Environmental Earth ScienceMiami UniversityOxford Ohio USA;</p> <p>Key Laboratory of Ocean and Marginal Sea Geology Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>Exploration and Development Research InstituteCPC Corporation TaiwanMiaoli Taiwan;</p> <p>Key Laboratory of Ocean and Marginal Sea Geology Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>State Key Laboratory of Ore Deposit Geochemistry Institute of GeochemistryChinese Academy of SciencesGuiyang China;</p> <p>Key Laboratory of Ocean and Marginal Sea Geology Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</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=fore‐arc basin&option=203" rel="nofollow">fore‐arc basin;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lichi Mélange&option=203" rel="nofollow">Lichi Mélange;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=biostratigraphy&option=203" rel="nofollow">biostratigraphy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=back thrusting&option=203" rel="nofollow">back thrusting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Taiwan arc‐continent collision&option=203" rel="nofollow">Taiwan arc‐continent collision;</a> </p> <div class="translation"> 机译：前弧盆地;LichiMélange;生物数据库;背部推进;台湾弧形碰撞; 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