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首页> 外文期刊>The island arc >Spatial distribution of the apatite fission‐track ages in the TT oki granite, central JJ apan: EE xhumation rate of a CC retaceous pluton emplaced in the EE ast AA sian continental margin
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Spatial distribution of the apatite fission‐track ages in the TT oki granite, central JJ apan: EE xhumation rate of a CC retaceous pluton emplaced in the EE ast AA sian continental margin

机译： T T OKI花岗岩中的磷灰石裂变轨道时代的空间分布，中央 J J APAN： E E Xhumation率的 C C RETACE富柱在 E E AST A A AIS Continental Margin中

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Abstract > The <fc>C</fc> retaceous <fc>T</fc> oki granitic pluton of the <fc>T</fc> ono district, central <fc>J</fc> apan was emplaced in the <fc>E</fc> ast <fc>A</fc> sian continental margin at about 70?Ma. The <fc>T</fc> oki granite has apatite fission‐track ( <fc>AFT</fc> ) ages ranging from 52.1 ±2.8?Ma to 37.1 ±3.6?Ma (number of measurements, n?=?33); this indicates the three‐dimensional thermal evolution during the pluton's low‐temperature history (temperature in the <fc>AFT</fc> partial annealing zone: 60–120?°C). The majority of the <fc>T</fc> oki granite has a spatial distribution of older ages in the shallower parts and younger ages in the deeper parts, representing that the shallower regions arrived (were exhumed) at the <fc>AFT</fc> closure depth earlier than the deeper regions. Such a cooling pattern was predominantly constrained by the exhumation of the <fc>T</fc> oki granitic pluton and was related to the regional denudation of the <fc>T</fc> ono district. The age–elevation relationships ( <fc>AER</fc> s) of the <fc>T</fc> oki granite indicate a fast exhumation rate of about 0.16 ±0.04?mm/year between 50?Ma and 40?Ma. The <fc>AFT</fc> inverse calculation using <fc>HeFT</fc> y program gives time‐temperature paths ( <fi>t</fi> – <fi>T</fi> paths), suggesting that the pluton experienced continuous slow cooling without massive reheating since about 40?Ma until the present day. A combination of the <fc>AER</fc> s and <fc>AFT</fc> inverse calculations represents the following exhumation history of th </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> > <FC> C </ FC> RETACE <FC> T </ FC> OKI花岗岩型富弦> <FC> T </ FC> ONO区，中央<FC> J </ FC> APAN在<FC> E </ FC> AST <FC> A A ASIAN Continental Margin中被置于约70？MA。 <FC> T </ FC> OKI花岗岩具有磷灰石裂变轨道（<FC> AFT </ FC>），范围从52.1±2.8？mA到37.1±3.6？mA（测量次数，n？= 33 ）;这表明了钢板低温历史中的三维热演变（<FC> AFT </ FC>部分退火区：60-120Ω·°C）。大多数<FC> T </ FC> OKI花岗岩在较深部分中的较浅零件和较小的零件中具有较大年龄的空间分布，代表较浅的区域（在<FC> AFT < / fc>比深层区域更早的封闭深度。这种冷却模式主要受到<Fc> T </ Fc> OKI花岗岩钚的辐射，并且与<FC> T </ FC> ONO区的区域剥蚀有关。 <Fc> T </ Fc> OKI花岗岩的年龄升高关系（<FC> AER </ FC> S）表示快速送达速率约为0.16±0.04？mm /岁50？mA和40？ma 。使用<FC> HEFT </ FC> Y程序的逆计算逆计算提供时间温度路径（<FI> T </ FI> - <FI> T </ FI>路径），表明这一点芦苇经历了连续缓慢的冷却，而不会大约40？马马直到现在。 <FC> AER </ FC> S和<FC> AFT </ FC>逆计算的组合代表了以下送达历史 </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6期</span><b style="margin: 0 2px;">|</b><span>共15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=Yuguchi Takashi&option=202" target="_blank" rel="nofollow">Yuguchi Takashi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sueoka Shigeru&option=202" target="_blank" rel="nofollow">Sueoka Shigeru;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Iwano Hideki&option=202" target="_blank" rel="nofollow">Iwano Hideki;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Danhara Tohru&option=202" target="_blank" rel="nofollow">Danhara Tohru;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ishibashi Masayuki&option=202" target="_blank" rel="nofollow">Ishibashi Masayuki;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sasao Eiji&option=202" target="_blank" rel="nofollow">Sasao Eiji;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nishiyama Tadao&option=202" target="_blank" rel="nofollow">Nishiyama Tadao;</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>Mizunami Underground Research Laboratory Geoscientific Research Department Tono Geoscience Center Sector of Decommissioning and Radioactive Waste ManagementJapan Atomic Energy Agency 1‐64 Yamanouchi AkiyoMizunami 509‐6132 Japan;</p> <p>Natural Hazard Evaluation Group Plant Technology Development Department Monju Project Management and Engineering CenterJapan Atomic Energy Agency 1 ShirakiTsuruga 919‐1279 Japan;</p> <p>Kyoto Fission‐Track Co. Ltd 44‐4 Minamitajiri OmiyaKita‐ku 603‐8832 Japan;</p> <p>Kyoto Fission‐Track Co. Ltd 44‐4 Minamitajiri OmiyaKita‐ku 603‐8832 Japan;</p> <p>Mizunami Underground Research Laboratory Geoscientific Research Department Tono Geoscience Center Sector of Decommissioning and Radioactive Waste ManagementJapan Atomic Energy Agency 1‐64 Yamanouchi AkiyoMizunami 509‐6132 Japan;</p> <p>Mizunami Underground Research Laboratory Geoscientific Research Department Tono Geoscience Center Sector of Decommissioning and Radioactive Waste ManagementJapan Atomic Energy Agency 1‐64 Yamanouchi AkiyoMizunami 509‐6132 Japan;</p> <p>Department of Earth and Environmental Sciences School of Science Graduate School of Science and TechnologyKumamoto University 2‐39‐1 Kurokami Chuo‐kuKumamoto 860‐8555 Japan;</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=apatite fission‐track age&option=203" rel="nofollow">apatite fission‐track age;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=chronological distribution in the pluton&option=203" rel="nofollow">chronological distribution in the pluton;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=E ast A sian continental margin&option=203" rel="nofollow">E ast A sian continental margin;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=exhumation history&option=203" rel="nofollow">exhumation history;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=HeFT y analysis&option=203" rel="nofollow">HeFT y analysis;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T oki granite&option=203" rel="nofollow">T oki granite;</a> </p> <div class="translation"> 机译：磷灰石裂变轨道时代;芦苇的时间顺序分布;E AST A AIR Continental Margin;挖掘历史;HEFT Y分析;T OKI花岗岩; </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> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024846853.html">Spatial distribution of the apatite fission‐track ages in the <fc >T</fc>T oki granite, central <fc >J</fc>J apan: <fc >E</fc>E xhumation rate of a <fc >C</fc>C retaceous pluton emplaced in the <fc >E</fc>E ast <fc >A</fc>A sian continental margin</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yuguchi Takashi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yuguchi Takashi,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sueoka Shigeru&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sueoka Shigeru,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Iwano Hideki&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Iwano Hideki,</a> <a href="/journal-foreign-30952/" target="_blank" rel="nofollow" class="tuijian_authcolor">The island arc .</a> <span>2017</span><span>,第6期</span> </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：<FC> T </ FC> T OKI花岗岩中的磷灰石裂变轨道时代的空间分布，中央<FC> J </ FC> J APAN：<FC> E </ FC> E Xhumation率的<FC > C </ FC> C RETACE富柱在<FC> E </ FC> E AST <FC> A </ FC> A AIS Continental Margin中</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_detail_thesis/0204121887849.html">Demand Side Management Strategy for Distribution Networks Volt/Var Control: A FCS-Model Predictive Control Approach</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rafael A. 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王怀信&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王怀信</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙军英&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,孙军英</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=付里&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,付里</a> <span> <a href="/journal-cn-57116/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 工程热物理学报 </a> </span> <span> . 2000</span><span>,第2期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-refrigeration_thesis/0201213987102.html">制冷剂CFC12的一种新三元替代工质HFC152a/HFC125/HFC134a</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈凌珊&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 陈凌珊</a> <span> <a href="/journal-cn-7716/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 制冷学报 </a> </span> <span> . 1998</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-28957_thesis/020222108751.html">FCS与后FCS时代</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王启志&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王启志</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王晓霞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王晓霞</a> <span> <a href="/conference-cn-28957/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 现场总线与智能仪表专题研讨会 </a> <span> <span> . 2003</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/02031651840.html">CFCl、CFCl和CFCl分子外价轨道电子动量谱的研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=尹晓峰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 尹晓峰</a> <span> . 2003</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120104161833.html">浅层电气保护器件(GFCI、AFCI和AFCI/GFCI)系统和方法</a> <b>[P]</b> . <span> 中国专利： CN111492540A </span> <span> . 2020-08-04</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/061201972078.html">PFC信号生成电路、使用PFC信号生成电路的PFC控制系统以及PFC控制方法</a> <b>[P]</b> . <span> 中国专利： CN103503295B </span> <span> . 2016.03.09</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130415182869.html">"process for separating a mixture comprising hf and hfc-1234ze, process for separating an e-hfc-1234ze from a mixture including hydrogen fluoride and said e-hfc-1234ze, process for separating" of hydrogen fluoride from a mixture containing hydrogen fluoride and e-hfc-1234ze, process for purifying an e-hfc-1234ze from a mixture of e-hfc-1234ze and hf, process for purifying hf from a mixture comprising e-hfc-1234ze and hf, process for separating e-hfc-1234ze from a mixture of e-hfc-1234ze, hf and at least one of hfc-245fa or hfc-245eb and process for hfc-1234yf separation from hfc-1234ze "</a> <b>[P]</b> . <span> 外国专利： <!-- --> BRPI0906015A2 </span> <span> . 2015-06-30</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：从包含氟化氢的混合物中分离氟化氢的“分离包含hf和hfc-1234ze的混合物的方法，从包含氟化氢和所述e-hfc-1234ze的混合物中分离e-hfc-1234ze的过程，分离方法”。 e-hfc-1234ze，从e-hfc-1234ze和hf的混合物中纯化e-hfc-1234ze的方法，从包含e-hfc-1234ze和hf的混合物中纯化hf的方法，分离e-hfc-从e-hfc-1234ze，hf和hfc-245fa或hfc-245eb中至少一种的混合物中提取1234ze，以及从hfc-1234ze中分离hfc-1234yf的方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130415182870.html">Separation process of a mixture comprising HF and HFC - 1234yf, separation process of HFC - 1234yf a mixture comprising hydrogen fluoride and the mentioned this 1234yf, separation process of hydrogen fluoride in a mixture comprising hydrogen fluoride and HF. C - 1234yf, purification process of HFC - 1234yf from a mixture comprising HFCS - 1234yf and HF.Purification process of HF from a mixture comprising an HFC - 1234yf and HF, separation of a mixture of HFC - 1234yf HFC - 1234yf, HF and at least one of HFC - 245cb or HFCS - 245eb and separation process of a mixture comprising HF HFC - 1234yf, HF and at least u M of HFC - 245cb or HFCS - 245eb</a> <b>[P]</b> . <span> 外国专利： <!-- --> BRPI0906014A2 </span> <span> . 2015-06-30</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：包含HF和HFC的混合物的分离过程-1234yf，HFC-1234yf的分离过程，包含氟化氢和上述的1234yf的混合物，包含氟化氢和HF的混合物中的氟化氢的分离过程。 C-1234yf，从包含HFCS-1234yf和HF的混合物中纯化HFC-1234yf的过程。从HFC-1234yf和HF的混合物中纯化HF，分离HFC-1234yf的混合物HFC-1234yf，HF和HFC-245cb或HFCS-245eb中的至少一种以及包含HF HFC-1234yf，HF和至少1 M的HFC-245cb或HFCS-245eb的混合物的分离方法 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130446818066.html">n - acetyl - (l) - (4) - tsu00fcanofenu00fcu00fclalaniini ac - (l) - (4 - ((cn) phe - oh and n - acetyl - (l) - p - amidinofenu00fcu00fclalaniintsu00fckloheksu00fcu00fclglu00fctsiin - beta - (3) - n - metu00fcu00fclpu00fcridiinium) alanine ac - (l) - paph - chg - palme (3) - nh2 valmistamismeetod</a> <b>[P]</b> . <span> 外国专利： <!-- --> EE03698B1 </span> <span> . 2002-04-15</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：n-乙酰-（l）-（4）-ts u00fcanofen u00fc u00fclalaniini ac-（l）-（4-（（cn）phe-oh和n-乙酰-（l）-p-amidinofen u00fc u00fclalaniints u00fckloheks u00fc u00fclgl u00fctsiin-beta-（3）-n-met u00fc u00fclp u00fcridiinium）丙氨酸ac-（l）-paph-chg-palme（3）-nh2 valmistamism </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> 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