U–Pb zircon ages of the Nakanogawa Group in the Hidaka Belt, northern Japan: Implications for its provenance and the protolith of the Hidaka metamorphic rocks

Nanayama Futoshi; Takahashi Yutaka; Yamasaki Toru; Nakagawa Mitsuru; Iwano Hideki; Danhara Tohru; Hirata Takafumi

摘要

Abstract >Zircon U–Pb ages of two acidic tuff and two turbidite sandstone samples from the Nakanogawa Group, Hidaka Belt, were measured to estimate its depositional age and the development of the Hokkaido Central Belt, northeast Japan. In the northern unit, homogeneous zircons from pelagic acidic tuff from a basal horizon dated to 58–57?Ma, zircons from sandstone from the upper part of the unit dated to 56–54?Ma, and zircons from acidic tuff from the uppermost part dated to 60–56?Ma and 69–63?Ma. Both of the tuff U–Pb ages are significantly older than the youngest radiolarian fossil age (66–48?Ma). Therefore, the maximum depositional age of the turbidite facies in the northern unit is 58?Ma and the younger age limit, estimated from the fossil age, is 48?Ma. In the southern unit, homogeneous zircons from turbidite sandstone dated to 58–57?Ma. Thus the depositional age of this turbidite facies was interpreted to be 66–56?Ma from the fossil age, probably close to 57?Ma. Most of the zircon U–Pb ages from the Nakanogawa Group are younger than 80?Ma, with a major peak at 60?Ma. This result implies that around Hokkaido volcanic activity occurred mainly after 80?Ma. Older zircon ages (120–80?Ma, 180–140?Ma, 340–220?Ma, 1.9?Ga, 2.2?Ga, and 2.7?Ga) give information about the provenance of other rocks in the Hidaka Belt. It is inferred that the Nakanogawa Group comprises protoliths of the upper sequence of the Hidaka Metamorphic Zone, which therefore has the same depositional age as the Nakanogawa Group (66–48?Ma). The depositional ages of the lower sequence of the Hidaka Metamorphic Zone and the Nakanogawa Group are probably the same. </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> > zircon u-pb ages两个酸性凝灰岩和来自Nakanogawa组的两个浊砂岩样品，目瞪口带，被测量估算其沉积年龄和日本东北地区北海道中央腰带的发展。在北方单位中，从基部地平线到58-57？MA，从砂岩的Zircons从单元的上部到56-54？ma，以及从最上部的酸性凝灰岩的氧化锆日期为60-56？MA和69-63？马。 Tuff U-PB年龄均比最小的放射性化化石年龄（66-48〜ma）明显大。因此，北部单位的浊度相的最大沉积年龄为58？ma和年轻的年龄限制，从化石年龄估计，是48？ma。在南部单位，浊度砂岩的均质锆石日期为58-57？马。因此，这种浊度相的沉积年龄被解释为来自化石年龄的66-56〜ma，可能接近57？ma。来自Nakanogawa集团的大多数锆石U-PB年龄小于80？MA，60米的主要峰值。这一结果意味着北海道火山活度主要发生在80次以后发生。较旧的锆石年龄（120-80？ma，180-140？ma，340-220？ma，1.9？ga，2.2？ga和2.7？ga）给出了有关Hidaka皮带中其他岩石的出处的信息。推断Nakanogawa组包括Hidaka变质区的上序的促果实，因此与Nakanogawa组（66-48 ma）具有与沉积年龄相同的沉积年龄。 Hidaka变质区和Nakanogawa组的下序列的沉积年龄可能是相同的。</ 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>2018年第2期</span><b style="margin: 0 2px;">|</b><span>共20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=Nanayama Futoshi&option=202" target="_blank" rel="nofollow">Nanayama Futoshi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Takahashi Yutaka&option=202" target="_blank" rel="nofollow">Takahashi Yutaka;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yamasaki Toru&option=202" target="_blank" rel="nofollow">Yamasaki Toru;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakagawa Mitsuru&option=202" target="_blank" rel="nofollow">Nakagawa Mitsuru;</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=Hirata Takafumi&option=202" target="_blank" rel="nofollow">Hirata Takafumi;</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>Geological Survey of JapanAIST1‐1‐1 Higashi Tsukuba 305‐8567 Japan;</p> <p>Geological Survey of JapanAIST1‐1‐1 Higashi Tsukuba 305‐8567 Japan;</p> <p>Geological Survey of JapanAIST1‐1‐1 Higashi Tsukuba 305‐8567 Japan;</p> <p>Geological Survey of JapanAIST1‐1‐1 Higashi Tsukuba 305‐8567 Japan;</p> <p>Kyoto Fission‐Track Co. LtdOmiya Kita‐Ku Kyoto 603‐8832 Japan;</p> <p>Kyoto Fission‐Track Co. LtdOmiya Kita‐Ku Kyoto 603‐8832 Japan;</p> <p>Geochemical Research Center Graduate School of ScienceThe University of TokyoBunkyo‐Ku Tokyo 113‐0033 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=depositional age&option=203" rel="nofollow">depositional age;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=early Eocene&option=203" rel="nofollow">early Eocene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hidaka Belt&option=203" rel="nofollow">Hidaka Belt;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hidaka metamorphic zone&option=203" rel="nofollow">Hidaka metamorphic zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=LA–ICP–MS&option=203" rel="nofollow">LA–ICP–MS;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakanogawa Group&option=203" rel="nofollow">Nakanogawa Group;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Paleocene&option=203" rel="nofollow">Paleocene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=U–Pb dating&option=203" rel="nofollow">U–Pb dating;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=zircon&option=203" rel="nofollow">zircon;</a> </p> <div class="translation"> 机译：沉积年龄;早期的eocene;海达拉腰带;Hidaka变质区;La-ICP-MS;Nakanogawa Group;古世纪;U-PB约会;锆石; </div> </li> </ul> </div> </div> <div class="literature cardcommon" id="literaturereference" style="display:none"> <div class="similarity "> <h3 class="all_title" id="enpatent111">引文网络</h3> <div class="referencetab clearfix"> <ul id="referencedaohang"> <li dataid="referenceul">参考文献</li> <li dataid="citationul">引证文献</li> <li dataid="commonreferenceul">共引文献</li> <li dataid="commoncitationul">同被引文献</li> <li dataid="tworeferenceul">二级参考文献</li> <li dataid="twocitationul">二级引证文献</li> </ul> </div> <div class="reference_details" id="referenceList"> <ul id="referenceul"></ul> <ul id="citationul"></ul> <ul id="commonreferenceul"></ul> <ul id="commoncitationul"></ul> <ul id="tworeferenceul"></ul> <ul id="twocitationul"></ul> </div> </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/0704024846973.html">U–Pb zircon ages of the Nakanogawa Group in the Hidaka Belt, northern Japan: Implications for its provenance and the protolith of the Hidaka metamorphic rocks</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nanayama Futoshi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Nanayama Futoshi,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Takahashi Yutaka&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Takahashi Yutaka,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yamasaki Toru&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yamasaki Toru,</a> <a href="/journal-foreign-30952/" target="_blank" rel="nofollow" class="tuijian_authcolor">The island arc .</a> <span>2018</span><span>,第2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：日本北部的Hidaka腰带的U-PB Zircon年龄段：对其出处的影响和Hidaka变质岩的促果</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070405623256.html">Linking granulites, silicic magmatism, and crustal growth in arcs: Ion microprobe (zircon) U-Pb ages from the Hidaka metamorphic belt, Japan</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kemp AIS&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kemp AIS,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shimura T&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Shimura T,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hawkesworth CJ&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hawkesworth CJ </a> <a href="/journal-foreign-23447/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geology .</a> <span>2007</span><span>,第9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：连接粒岩，硅质岩浆作用和弧形地壳生长：日本日高变质带的离子微探针（锆石）U-Pb年龄</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_detail_thesis/0204115550059.html">Pseudotachylytes, related fault rocks, asperities, and crustal structures in the Hidaka metamorphic belt, Hokkaido, northern Japan</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T. Toyoshima&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">T. Toyoshima,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T. Obara&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">T. Obara,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T. Niizato&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">T. Niizato,</a> <a href="/journal-foreign-22384/" target="_blank" rel="nofollow" class="tuijian_authcolor">Earth, planets and space: EPS .</a> <span>2004</span><span>,第12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：日本北部北海道日高变质带中的假速溶质，相关断层岩石，凹凸不平和地壳结构</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_meeting--1_thesis/020515089383.html">Fluid and melt inclusions in rock-forming minerals and zircons from high grade polymetamorphic rocks:origin of protoliths, characteristics of the superimposed metamorphic events and zircon age interpretation</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> </a> <a href="/conference-foreign--1/" target="_blank" rel="nofollow" class="tuijian_authcolor"> .</a> <span>2006</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：高品位多变质岩中成岩矿物和锆石中的流体和熔体包裹体：原石起源，叠加变质事件的特征和锆石年龄解释</span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-degree-foreign_mphd_thesis/02061562106.html">Geochemistry, Nd, Pb and Sr Isotope Systematics, and U-Pb zircon ages of the Neoarchean Bad Vermilion Lake Greenstone Belt and Spatially Associated Granitic rocks, Western Superior Province, Canada.</a> <b>[D] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wu, Tuoyu.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wu, Tuoyu. </a> <span>2015</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：新西伯利亚Bad Vermilion湖绿石带和空间相关的花岗岩岩石的地球化学，Nd，Pb和Sr同位素系统学以及U-Pb锆石年龄，加拿大西部上级省。</span> </p> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-journal-foreign-pmc_elsevier-sponsored-documents_thesis/040004946429.html">Single crystal U–Pb zircon age and Sr–Nd isotopic composition of impactites from the Bosumtwi impact structure Ghana: Comparison with country rocks and Ivory Coast tektites</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ludovic Ferrière&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ludovic Ferrière,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Christian Koeberl&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Christian Koeberl,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Martin Thöni&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Martin Thöni,</a> <span>-1</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：加纳Bosumtwi撞击结构的撞击岩单晶U–Pb锆石年龄和Sr–Nd同位素组成：与乡村岩石和象牙海岸陨石的比较</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/0100025906215.html">Pseudotachylytes, related fault rocks, asperities, and crustal structures in the Hidaka metamorphic belt, Hokkaido, northern Japan</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T. Toyoshima&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">T. Toyoshima,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T. Obara&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">T. Obara,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T. Niizato&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">T. Niizato,</a> <span>2014</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：日本北部北海道日高变质带中的假速溶质，相关断层岩石，凹凸不平和地壳结构</span> </p> </li> <li> <div> <b>8. </b><a class="enjiyixqcontent" href="/ntis-science-report_de_thesis/020711747725.html">Morphology and U-Pb Ages of Zircons from the High-Grade Metamorphic Precambrian in the Sirdal-Oersdal Area, SW Norway</a> <b>[R] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wielens, J. B. W.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wielens, J. B. W. </a> <span>1979</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：来自挪威西南部sirdal-Oersdal地区高级变质前寒武纪的锆石形态和U-pb年龄</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_oil-gas-storage-transportation_thesis/020125121666.html">日本甜柿保花促果技术</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . </a> <span> <a href="/journal-cn-7333/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 农业知识（瓜果菜） </a> </span> <span> . 2004</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_fruit-growers-friend_thesis/0201259841430.html">日本甜柿保花促果技术要点</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王其广&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王其广</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈延智&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,陈延智</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=付方元&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,付方元</a> <span> <a href="/journal-cn-6936/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 果农之友 </a> </span> <span> . 2004</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_anhui-forestry-science-technology_thesis/0201260267978.html">日本甜柿的促花促果技术</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=黄武&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 黄武</a> <span> <a href="/journal-cn-6974/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 安徽林业科技 </a> </span> <span> . 2002</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-jinling-institute-technology_thesis/0201272760457.html">不同处理方法对陀螺果扦插促根的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵子荀&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵子荀</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=沈子雅&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,沈子雅</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=牛曼婷&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,牛曼婷</a> <span> <a href="/journal-cn-4677/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 金陵科技学院学报 </a> </span> <span> . 2019</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201295847311.html">花期促果措施对冬枣内源激素和坐果率的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=马庆华&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 马庆华</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=续九如&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,续九如</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王贵禧&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王贵禧</a> <span> <a href="/journal-cn-56720/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国农学通报 </a> </span> <span> . 2010</span><span>,第9期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-14201_thesis/020221093498.html">退变质流体对超高压变质岩石Rb-Sr，Sm-Nd，U-Pb和Lu-Hf同位素体系的影响——以苏鲁超高压变质带南部青龙山地区为例</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李红艳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李红艳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王栋&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王栋</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=程湘&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,程湘</a> <span> <a href="/conference-cn-14201/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2010年全国岩石学与地球动力学研讨会 </a> <span> <span> . 2010</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020315645214.html">生长调节剂对环江县引种薄壳山核桃‘绍兴’控梢促果影响初探</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李莹&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李莹</a> <span> . 2020</span> </span> </div> </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> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704024846973','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="关闭" onclick="$('.journalsub-pop-up').hide()"> <p class="pardon">抱歉，该期刊暂不可订阅，敬请期待！</p> <p class="current">目前支持订阅全部北京大学中文核心（2020）期刊目录。</p> <div style="display: flex;margin-top: 69px;justify-content: space-between;"> <div class="no-sub" onclick="$('.journalsub-pop-up').hide()">暂不订阅</div> <div class="other-sub" onclick="continueSub('from=pc-detail')">继续订阅其他期刊</div> </div> </div> </div> <div class="right_btn"> <ul> <li class="gouwuche">  </li> <li class="yijian"> <a href="javascript:void(0);" onclick="link_analysis('/mycenter/auth/complaint.html',this)" title="意见反馈">意见反馈</a> </li> <li class="top"> <a href="javascript:scrollTo(0,0);" title="回到顶部">回到顶部</a> </li> <li class="shouye"> <a href="/" title="首页">回到首页</a> </li> </ul> </div> <div class="xllindexfooter"> <div class="xllindexfootercenter"> <div class="xllindexfooterleft left" > <div class="xllindexfooterleftli"> <ul> <li><a href="/about.html" title="关于掌桥">关于掌桥</a></li> <li><a href="/help/helpmap.html" title="资源导航">资源导航</a></li> <li><a href="/help/helpguide.html" title="新手指南">新手指南</a></li> <li><a href="/help/helpcenter.html" title="常见问题">常见问题</a></li> <li><a href="/sitemap.html" title="网站地图">网站地图</a></li> <li><a href="/help/helpcenter.html?type=9" title="版权声明">版权声明</a></li> </ul> </div> <div class="xllindexfooterleft"> <p class="xllindexfooterlefteamil">客服邮箱：kefu@zhangqiaokeyan.com</p> <div class="xllindexfooterlefttcp"> <div class="xllindexfooterpoliceiimg"></div> <div class="xllindexfooterpoliceispan"> <span>京公网安备：11010802029741号 </span> <span>ICP备案号：<a href="https://beian.miit.gov.cn" rel="nofollow" target="_blank" title="ICP备案号">京ICP备15016152号-6</a></span> <span>六维联合信息科技 (北京) 有限公司©版权所有</span> </div> </div> </div> </div> <div class="xllindexfooterright left"> <ul> <li> <p style="font-weight: bold;">客服微信</p> <div></div> </li> <li> <p style="font-weight: bold;">服务号</p> <div></div> </li> </ul> </div> </div> </div> <span id="0704024846973down" data-source="7," data-out-id="EtlVyfvRVvUkgmgu+xrGYKgZnRlhW/cEHMJ1Ri/lMzhhFzo8NrQ64x/9JQ10Q5cd," data-f-source-id="7" data-title="U–Pb zircon ages of the Nakanogawa Group in the Hidaka Belt, northern Japan: Implications for its provenance and the protolith of the Hidaka metamorphic rocks" data-price="20" data-site-name="" data-transnum="24" style="display:none;"></span> <input type="hidden" value="4" id="sourcetype"> <input type="hidden" value="0704024846973" id="docid"> <input type="hidden" value="30952" id="journalid"> <input type="hidden" value="1" id="inyn_provide_service_level"> <input type="hidden" value="https://cdn.zhangqiaokeyan.com" id="imgcdn"> <input type="hidden" value="1" id="isdeatail"> <input type="hidden" value="" id="syyn_indexed_database"> <input type="hidden" value="" id="servicetype"> <input type="hidden" id="pagename" value="U–Pb zircon ages of the Nakanogawa Group in the Hidaka Belt, northern Japan: Implications for its provenance and the protolith of the Hidaka metamorphic rocks"/> <input type="hidden" value="thesis_get_original" id="pageIdentification"> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery-1.12.4.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/lwlh_ajax.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zq.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/common.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery.cookie.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/top.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/tip.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/login.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/down.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/search.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/newmail.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/page.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/searchtype.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/user/regist.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zxs_solor/detail.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zxs_solor/reference.js?v=5.8.7"></script> <script type="text/javascript" src="https://www.zhangqiaokeyan.com/statistics/static/pagecollection.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/tj.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/sse.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/pushbaidu.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/history.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/util/cookie.js?v=5.8.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/weipu/weipu.js?v=5.8.7"></script> </body> <script> function kefu(customization) { var from = GetQueryString("from"); if (from == null || from == "") { from = "other"; } var url = getWxWorkQrCode(73, from, customization); if (url == "" || typeof url == 'undefined') { url = "https://wework.qpic.cn/wwpic/994838_0LUTS-VqR0quT1N_1675665967/0"; } tipDocGuidance(url, '人工辅助获取外文期刊材料'); } $(function(){ var weiPuStatus = getCookie('WeiPuStatus'); if(weiPuStatus){ tipWeiPuStatus(weiPuStatus); delCookie('WeiPuStatus'); } getFacetKeywordVoInId(); var sourcetype = $("#sourcetype").val(); var inyn_provide_service_level = $("#inyn_provide_service_level").val(); if((sourcetype ==1||sourcetype==4)&&inyn_provide_service_level!=4){ getJournal(); } }) function toCoverPage(){ var sourcetype=$("#sourcetype").val var fromStr=""; if(sourcetype==0){ fromStr="pc-wwoaxiangqing"; } if(sourcetype==4){ fromStr="pc-wwdetail-title"; } if(sourcetype==5){ fromStr="pc-wwhuiyixiangqing"; } window.location.href=url+"/zhichengpingshenlunwen.html?from="+fromStr; } </script> </html>