Integrated Radiolaria, benthic foraminifera and conodont biochronology of the pelagic Permian blocks/tectonic slices and geochemistry of associated volcanic rocks from the Mersin Mélange, southern Turkey: Implications for the Permian evolution of the northern Neotethys

Tekin Ugur Kagan; Okuyucu Cengiz; Sayit Kaan; Bedi Yavuz; Noble Paula J.; Krystyn Leopold; G?ncüoglu Mehmet Cemal

摘要

Abstract >Blocks and tectonic slices within the Mersin Mélange (southern Turkey), which are of Northern Neotethyan origin (Izmir–Ankara–Erzincan Ocean (IAE)), were studied in detail by using radiolarian, conodont, and foraminiferal assemblages on six different stratigraphic sections with well‐preserved Permian succesions. The basal part of the Permian sequence, composed of alternating chert and mudstone with basic volcanics, is assigned to the late Asselian (Early Permian) based on radiolarians. The next basaltic interval in the sequence is dated as Kungurian. The highly alkaline basic volcanics in the sequence are extremely enriched, similar to kimberlitic/lamprophyric magmas generated at continental intraplate settings. Trace element systematics suggest that these lavas were generated in a continental margin involving a metasomatized subcontinental lithospheric mantle source (SCLM). The middle part of the Permian sequences, dated by benthic foraminifera and conodont assemblages, includes detrital limestones with chert interlayers and neptunian dykes of middle Wordian to earliest Wuchiapingian age. Higher in the sequence, detrital limestones are overlain by alternating chert and mudstone with intermittent microbrecciated beds of early Wuchiapingian to middle Changhsingian (Late Permian) age based on the radiolarians. A large negative shift at the base of the Lopingian at the upper part of section is correlated to negative shifts at the Guadalupian/Lopingian boundary associated with the end‐Guadalupian mass extinction event. All these findings indicate that a continental rift system associated with a possible mantle plume existed during the late Early to Late Permian period. This event was responsible for the rupturing of the northern Gondwanan margin related to the opening of the IAE Ocean. When the deep basinal features of the Early Permian volcano‐sedimentary sequence are consi </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> > MersinMélange（南部土耳其）内的块和构造片，北尼科斯北部北部（Izmir-Ankara-Erzincan Ocean（IAE））通过使用Radiolarian，Conodont和Forminiferal组装在六个不同的地层部分上进行详细研究，具有保存完全的二叠件果实。双序列的基础部分，由交替的燧石和泥岩与基本火山岩组成，被分配到基于放射性的较晚的陈述（早期二叠纪）。序列中的下一个玄武岩间隔被称为kungurian。序列中的高度碱性碱性火山岩是极其富集的，类似于在欧陆内部内部产生的Kimberlitic / Lamprophyic Magmas。痕量元素系统表明，这些熔岩是在涉及弥漫的亚型岩石岩石地幔源（SCLM）的大陆边缘中产生的。由Benthic Foraminifera和Conodont组合日期的二叠腔序列的中间部分包括滴乳石灰石，中间德语和中间德国的Neptunian Dykes至最早的武伍坡时代。序列中较高，滴乳石灰石通过交替的燧石和泥岩与间歇性微生物的床，武家市早期的常春藤（晚二叠纪）年龄基于放射性岩。在部分上部的梯田基地的底座上的大负偏移与与末端 - 瓜达卢普群众灭绝事件相关的瓜达卢普/洛杭人边界的负换档相关。所有这些调查结果表明，在早期久经济期间的早期患者期间存在与可能的地幔羽流相关的大陆裂缝系统。该事件负责与IAE海洋开放有关的北方阁楼利润率破裂。当早期的二叠膜火山沉积序列的深层间隙是Consi时 </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-30952/'>《The island arc》</a> <b style="margin: 0 2px;">|</b><span>2019年第2期</span><b style="margin: 0 2px;">|</b><span>共37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=Tekin Ugur Kagan&option=202" target="_blank" rel="nofollow">Tekin Ugur Kagan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Okuyucu Cengiz&option=202" target="_blank" rel="nofollow">Okuyucu Cengiz;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sayit Kaan&option=202" target="_blank" rel="nofollow">Sayit Kaan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bedi Yavuz&option=202" target="_blank" rel="nofollow">Bedi Yavuz;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Noble Paula J.&option=202" target="_blank" rel="nofollow">Noble Paula J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Krystyn Leopold&option=202" target="_blank" rel="nofollow">Krystyn Leopold;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=G?ncüoglu Mehmet Cemal&option=202" target="_blank" rel="nofollow">G?ncüoglu Mehmet Cemal;</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 Geological EngineeringHacettepe UniversityBeytepe 06800 Ankara;</p> <p>Department of Geological EngineeringSelcuk UniversityKonya 42075 Turkey;</p> <p>Department of Geological EngineeringMiddle East Technical UniversityAnkara 06800 Turkey;</p> <p>Department of Geological InvestigationGeneral Directorate of Mineral Research and ExplorationAnkara 06800 Turkey;</p> <p>Department of Geological Sciences and EngineeringMS 172 University of Nevada RenoReno Nevada 89557‐0138 USA;</p> <p>Department of PalaeontologyVienna University Geozentrum Althanstra?e 9Vienna 1090 Austria;</p> <p>Department of Geological EngineeringMiddle East Technical UniversityAnkara 06800 Turkey;</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>P313.7; </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=biochronology&option=203" rel="nofollow">biochronology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fossil assemblages&option=203" rel="nofollow">fossil assemblages;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magmatic geochemistry&option=203" rel="nofollow">magmatic geochemistry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Permian&option=203" rel="nofollow">Permian;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tethyan evolution&option=203" rel="nofollow">Tethyan evolution;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Turkey&option=203" rel="nofollow">Turkey;</a> </p> <div class="translation"> 机译：生物学;化石组合;魔法地球化学;二叠纪;Tethyan演变;土耳其; 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