Rapid cooling and geospeedometry of granitic rocks exhumation within a volcanic arc: A case study from the Central Slovakian Neovolcanic Field (Western Carpathians)

Kohút Milan; Dani?ík Martin

摘要

Abstract > U–Pb Sensitive High‐Resolution Ion MicroProbe ( <fc>SHRIMP</fc> ) dating of zircon in combination with (U–Th)/He dating of zircon and apatite is applied to constrain the emplacement and exhumation history of the youngest granitic rocks in the Western Carpathians collected in the Central Slovakian Neovolcanic Field. Two samples of diorite from the locality Banky, and granodiorite from Banská Hodru?a yield the U–Pb zircon concordia ages of 15.21 ±0.19 Ma and 12.92 ±0.27?Ma, respectively, recording the time of zircon crystallization and the intrusions’ emplacement. Zircon (U–Th)/He ages of 14.70 ±0.94 (Banky) and 12.65 ±0.61?Ma (Banská Hodru?a), and apatite (U–Th)/He ages of 14.45 ±0.70?Ma (diorite) and 12.26 ±0.77?Ma (granodiorite) are less than 1?Myr younger than the corresponding zircon U–Pb ages. For both diorite and granodiorite rocks their chronological data thus document a simple cooling process from magmatic crystallization/solidification temperatures to near‐surface temperatures in the Middle Miocene, without subsequent reheating. Geospeedometry data suggest for rapid cooling at an average rate of 678 ±158 °C/Myr, and the exhumation rate of 5?mm/year corresponding to active tectonic‐forced exhumation. The quick cooling is interpreted to record the exhumation of the studied granitic rocks complex that closely followed its emplacement, and was likely accompanied by a drop in the paleo‐geothermal gradient due to cessation of volcanic activity in the area. </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”> <标题类型=“main”>抽象</ title> > U-Pb敏感的高分辨率离子微探测（<FC> ShRIMP </ FC>）ZIRCON与（ u-th）/ zircon和磷灰石的约会适用于限制在中央斯洛伐克Neovolcanic田野中喀尔巴阡山脉最年轻的花岗岩岩石的施加和挖掘历史。来自地区私人的两种模具，以及来自BanskáHodru的Granodiorite，分别为15.21±0.19 mA和12.92±0.27Ω的U-PB锆石康科氏菌和12.92±0.27Ω。锆石（U-TH）/何年14.70±0.94（银行）和12.65±0.61？MA（鲍氏霍尔鲁？A），磷灰石（U-TH）/他年龄14.45±0.70？MA（Diorite）和12.26岁±0.77？ma（granodiorite）小于1？myr比相应的锆石U-Pb年龄较小。对于Diorite和Granodiorite岩石的岩石，它们的时间顺序数据从岩浆结晶/凝固温度下记录了简单的冷却过程，在中间内烯中的近表面温度下，无需随后再加热。地理化测量数据表明，平均速率为678±158°C / MYR的平均速率，以及对应于有源构造强制挖掘的5？mm /年的呼口速率。快速冷却被解释为记录所研究的花岗岩复合物的散发，紧密遵循其施加，并且由于该地区的火山活性的停止，古地热梯度可能伴随着古地热梯度。 </ 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-30952/'>《The island arc》</a> <b style="margin: 0 2px;">|</b><span>2017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=Kohút Milan&option=202" target="_blank" rel="nofollow">Kohút Milan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dani?ík Martin&option=202" target="_blank" rel="nofollow">Dani?ík Martin;</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 Geology Earth Science InstituteSlovak Academy of SciencesDúbravská cesta 9 840 05 Bratislava Slovakia;</p> <p>Faculty of Science and Engineering Department of Earth and Ocean SciencesThe University of WaikatoPrivate Bag 3105 Hamilton 3240 New Zealand;</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=Central Slovakian Neovolcanic Field&option=203" rel="nofollow">Central Slovakian Neovolcanic Field;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geospeedometry&option=203" rel="nofollow">geospeedometry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=granitic rocks&option=203" rel="nofollow">granitic rocks;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Western Carpathians&option=203" rel="nofollow">Western Carpathians;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=zircon and apatite (U–Th)/He dating&option=203" rel="nofollow">zircon and apatite (U–Th)/He dating;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=zircon U–Pb dating&option=203" rel="nofollow">zircon U–Pb dating;</a> </p> <div class="translation"> 机译：中央斯洛伐克Neovolcanic田地;地理化测量;花岗岩;西喀尔巴阡山脉;锆石和磷灰石（U-TH）/他约会;Zircon U-Pb约会; </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/0704024846999.html">Rapid cooling and geospeedometry of granitic rocks exhumation within a volcanic arc: A case study from the Central Slovakian Neovolcanic Field (Western Carpathians)</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kohút Milan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kohút Milan,</a> <a 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