Comment on “Sedimentary and Tectonic Evolution of the Southern Qiangtang Basin: Implications for the Lhasa‐Qiangtang Collision Timing” by A. Ma et al.

Chen Wei‐Yan; Hu Xiu‐Cheng; Zhong Yun; Fu Yuan‐Bin; Li Fang; Wang Yu‐Guang

摘要

Abstract > Ma et al. (2017, <url href="https://doi.org/10.1002/2017JB014211">https://doi.org/10.1002/2017JB014211</url> ) proposed that the Lhasa‐Qiangtang collision commenced in late Bathonian time (~166?Ma), based on the observation of an angular unconformity that truncated the Bathonian Buqu Formation from the late Bathonian‐early Callovian Biluoco Formation and the recognition of siliciclastic provenance switch from arc igneous source to uplifted orogenic source in the Biluoco‐Qixiangco area of the southern Qiangtang basin. Unfortunately, however, extensive exposure of Late Jurassic‐Middle Cretaceous ophiolite fragments and marine sedimentary rocks along the Bangong suture zone indicates that the Bangong Meso‐Tethys Ocean did not close until the Late Cretaceous, which is consistent with a Late Jurassic‐Middle Cretaceous magmatic arc in the southern Qiangtang terrane as well as paleomagnetic data. The late Bathonian orogenic event in the southern Qiantang area observed by Ma et al. (2017, <url href="https://doi.org/10.1002/2017JB014211">https://doi.org/10.1002/2017JB014211</url> ) can be explained by subduction of oceanic highs on the Bangong Meso‐Tethyan Ocean. Clearly, our submission is a significant clearance to Ma et al.'s work and the Tibetan Plateau geology and of timely significance in correctly understanding the evolution history of the Tibetan Plateau. Therefore, our paper possibly is of broad interest to our international colleagues. </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”> <title type =“main”>抽象</ title> > ma等。（2017，<url href =“https://doi.org/10.1002/2017JB014211”> https://doi.org/10.1002/2017Jb014111基于从晚期浴室 - 早期的Callovian Biluoco Biluoco形成的角度无关的观察到角度无关的观察，从弧形火射源识别来自火炬源的硅砾原子源，在Biluoco-Qixiangco地区升起造山电源南羌塘盆地南部。然而，遗憾的是，沿着邦贡缝合区的晚期侏罗纪中间白垩丙酸酯碎片和海洋沉积岩的广泛暴露表明，邦戈梅索 - 特提什海海洋直到晚白垩纪直到白垩纪，这与侏罗纪中间白垩纪千变万化一致在南羌塘地区的弧形以及古磁性数据。 Ma等人观察到的南方塘地区的后期浴室orenatencim活动。（2017，<URL HREF =“https://doi.org/10.1002/2017JB014211”> https://doi.org/10.1002/2017JB01411 </ URL>）可以通过庞戈中间的海洋高点浏览来解释Tethyan海洋。显然，我们的提交是Ma等人的重要许可。工作和西藏高原地质以及及时意义在正确了解藏高原的演变史。因此，我们的论文可能对我们的国际同事感兴趣。 </ p> </ abstract> </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9期</span><b style="margin: 0 2px;">|</b><span>共5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 Wei‐Yan&option=202" target="_blank" rel="nofollow">Chen Wei‐Yan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hu Xiu‐Cheng&option=202" target="_blank" rel="nofollow">Hu Xiu‐Cheng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhong Yun&option=202" target="_blank" rel="nofollow">Zhong Yun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fu Yuan‐Bin&option=202" target="_blank" rel="nofollow">Fu Yuan‐Bin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Fang&option=202" target="_blank" rel="nofollow">Li Fang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Yu‐Guang&option=202" target="_blank" rel="nofollow">Wang Yu‐Guang;</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>School of Marine SciencesSun Yat‐sen UniversityGuangzhou China;</p> <p>School of Marine SciencesSun Yat‐sen UniversityGuangzhou China;</p> <p>School of Marine SciencesSun Yat‐sen UniversityGuangzhou China;</p> <p>Island Protection and Utilization Research CenterNational Marine Environmental Monitoring CenterDalian China;</p> <p>Island Protection and Utilization Research CenterNational Marine Environmental Monitoring CenterDalian China;</p> <p>Island Protection and Utilization Research CenterNational Marine Environmental Monitoring CenterDalian 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=Bangong suture zone&option=203" rel="nofollow">Bangong suture zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lhasa‐Qiangtang collision&option=203" rel="nofollow">Lhasa‐Qiangtang collision;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Meso‐Tethys&option=203" rel="nofollow">Meso‐Tethys;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tibetan Plateau&option=203" rel="nofollow">Tibetan Plateau;</a> </p> <div class="translation"> 机译：ban攻速途rezone;Lhasa‐Q Ian G糖collision;me so‐Tethys;Tibetan plateau; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025591112.html">Comment on “Sedimentary and Tectonic Evolution of the Southern Qiangtang Basin: Implications for the Lhasa‐Qiangtang Collision Timing” by A. 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