Depositional ages and characteristics of        <fc >M</fc>M        iddle–        <fc >U</fc>U        pper        <fc >J</fc>J        urassic and        <fc >L</fc>L        ower        <fc >C</fc>C        retaceous lacustrine deposits in southeastern        <fc >M</fc>M        ongolia

Hasegawa Hitoshi; Ando Hisao; Hasebe Noriko; Ichinnorov Niiden; Ohta Tohru; Hasegawa Takashi; Yamamoto Masanobu; Li Gang; Erdenetsogt Bat‐Orshikh; Heimhofer Ulrich; Murata Takayuki; Shinya Hironori; Enerel G.; Oyunjargal G.; Munkhtsetseg O.; Suzuki Noriyuki; Irino Tomohisa; Yamamoto Koshi

摘要

Abstract >Lower Cretaceous lacustrine oil shales are widely distributed in southeastern Mongolia. Due to the high organic carbon content of oil shale, many geochemical studies and petroleum exploration have been conducted. Although most of the oil shales are considered to be Early Cretaceous in age, a recent study reveals that some were deposited in the Middle Jurassic. The present study aims at establishing depositional ages and characteristics of the Jurassic and Cretaceous lacustrine deposits in Mongolia. The Lower Cretaceous Shinekhudag Formation is about 250?m thick and composed of alternating beds of shale and dolomite. The Middle Jurassic Eedemt Formation is about 150?m thick and composed of alternating beds of shale, dolomitic marl, and siltstone. The alternations of shale and dolomite in both formations were formed by lake level changes, reflecting precipitation changes. Shales were deposited in the center of a deep lake during highstand, while dolomites were formed by primary precipitation during lowstand. Based on the radiometric age dating, the Shinekhudag Formation was deposited between 123.8?±2.0 Ma and 118.5?±0.9 Ma of the early Aptian. The Eedemt Formation was deposited at around 165–158?Ma of Callovian–Oxfordian. The calculated sedimentation rate of the Shinekhudag Formation is between 4.7?±2.6 cm/ky and 10.0?±7.6 cm/ky. Shales in the Shinekhudag Formation show micrometer‐scale lamination, consisting of algal organic matter and detrital clay mineral couplets. Given the average thickness of micro‐laminae and calculated sedimentation rate, the micro‐lamination is most likely of varve origin. Both Middle–Upper Jurassic and Lower Cretaceous lacustrine oil shales were deposited in intracontinental basins in the paleo‐Asian continent. Tectonic processes and basin evolution basically controlled the deposition of these oil shales. In addition, enhanced precipitation </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”> <标题类型=“main”>抽象</标题> >下白垩纪湖泊石头广泛分布在蒙古东南部。由于油页岩的高有机碳含量，已经进行了许多地球化学研究和石油勘探。虽然大多数石油都被认为是年龄的早期白垩纪，但最近的一项研究表明，一些人沉积在侏罗纪中。本研究旨在建立蒙古侏罗纪和白垩纪湖泊沉积物的沉积年龄和特征。较低的白垩纪ShineKhudag形成约为250Ω米厚，由页岩和白云石的交替床组成。中间侏罗纪EEDEMT形成约150？米厚，由页岩，白云岩Marl和粉晶体的交替床组成。两种形成中的页岩和白云石的交替是通过湖泊水平变化形成的，反映降水变化。在高处理期间，Shales沉积在深湖中心，而Dolomites在低置期间通过初级沉淀形成。基于辐射尺年的约会，沉积在早期APTIAN的123.8±2.0 mA和118.5之间沉积在123.8？±2.0 mA之间。 EEDEMT形成沉积在115-158左右的Callovian-oxfordian。 ShineKhudag形成的计算沉降速率在4.7？±2.6cm / Ky和10.0？±7.6cm / ky之间。 Shinekhudag形成中的Shales显示米尺级层压，由藻类有机物和酥皮粘土矿物对联组成。鉴于微椎板的平均厚度和计算的沉降率，微层压最有可能变形。中上部侏罗纪和下白垩纪湖泊石头沉积在古亚洲大陆的肠道盆地。构造过程和盆地演化基本上控制了这些油页的沉积。此外，增强沉淀 </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3期</span><b style="margin: 0 2px;">|</b><span>共19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=Hasegawa Hitoshi&option=202" target="_blank" rel="nofollow">Hasegawa Hitoshi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ando Hisao&option=202" target="_blank" rel="nofollow">Ando Hisao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hasebe Noriko&option=202" target="_blank" rel="nofollow">Hasebe Noriko;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ichinnorov Niiden&option=202" target="_blank" rel="nofollow">Ichinnorov Niiden;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ohta Tohru&option=202" target="_blank" rel="nofollow">Ohta Tohru;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hasegawa Takashi&option=202" target="_blank" rel="nofollow">Hasegawa Takashi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yamamoto Masanobu&option=202" target="_blank" rel="nofollow">Yamamoto Masanobu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Gang&option=202" target="_blank" rel="nofollow">Li Gang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Erdenetsogt Bat‐Orshikh&option=202" target="_blank" rel="nofollow">Erdenetsogt Bat‐Orshikh;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heimhofer Ulrich&option=202" target="_blank" rel="nofollow">Heimhofer Ulrich;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Murata Takayuki&option=202" target="_blank" rel="nofollow">Murata Takayuki;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shinya Hironori&option=202" target="_blank" rel="nofollow">Shinya Hironori;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Enerel G.&option=202" target="_blank" rel="nofollow">Enerel G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Oyunjargal G.&option=202" target="_blank" rel="nofollow">Oyunjargal G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Munkhtsetseg O.&option=202" target="_blank" rel="nofollow">Munkhtsetseg O.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Suzuki Noriyuki&option=202" target="_blank" rel="nofollow">Suzuki Noriyuki;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Irino Tomohisa&option=202" target="_blank" rel="nofollow">Irino Tomohisa;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yamamoto Koshi&option=202" target="_blank" rel="nofollow">Yamamoto Koshi;</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 Global Environment and Disaster PreventionFaculty of Science and Technology Kochi UniversityKochi 780‐8520 Japan;</p> <p>Department of Earth Sciences Faculty of ScienceIbaraki UniversityBunkyo Mito 310‐8512 Japan;</p> <p>Institute of Nature and Environmental TechnologyKanazawa UniversityKakuma Kanazawa 920‐1192 Japan;</p> <p>Institute of Paleontology and GeologyMongolian Academy of SciencesP.O.B. 260 Ulaanbaatar 210351 Mongolia;</p> <p>Department of Earth Sciences Faculty of Education and Integrated Arts and SciencesWaseda UniversityNishiwaseda Shinjuku Tokyo 169‐8050 Japan;</p> <p>Department of Earth Sciences Faculty of ScienceKanazawa UniversityKakuma Kanazawa 920‐1192 Japan;</p> <p>Faculty of Environmental Earth ScienceHokkaido UniversityKita 8 Nishi 5 Kita‐ku Sapporo 060‐0810 Japan;</p> <p>Nanjing Institute of Geology and PalaeontologyChinese Academy of Science 39 East Beijing RoadNanjing 210008 China;</p> <p>Department of Geology and GeophysicsNational University of MongoliaKH Surguuliin Gudamj‐1 Ulaanbaatar 14200 Mongolia;</p> <p>Institute for GeologyLeibniz University HannoverWelfengarten 1 Hannover D‐30167 Germany;</p> <p>Department of Earth Sciences Faculty of ScienceIbaraki UniversityBunkyo Mito 310‐8512 Japan;</p> <p>Department of Earth Sciences Faculty of Education and Integrated Arts and SciencesWaseda UniversityNishiwaseda Shinjuku Tokyo 169‐8050 Japan;</p> <p>School of Geology and MiningMongolian University of Science and TechnologyBaga Toiruu34 Sukhbaatar Ulaanbaatar 210646 Mongolia;</p> <p>School of Geology and MiningMongolian University of Science and TechnologyBaga Toiruu34 Sukhbaatar Ulaanbaatar 210646 Mongolia;</p> <p>School of Geology and MiningMongolian University of Science and TechnologyBaga Toiruu34 Sukhbaatar Ulaanbaatar 210646 Mongolia;</p> <p>Department of Natural History ScienceHokkaido UniversityKita 8 Nishi 5 Kita‐ku Sapporo 060‐0810 Japan;</p> <p>Faculty of Environmental Earth ScienceHokkaido UniversityKita 8 Nishi 5 Kita‐ku Sapporo 060‐0810 Japan;</p> <p>Graduate School of Environmental StudiesNagoya UniversityFuro‐cho Chikusa‐ku Nagoya 464‐8601 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=C retaceous&option=203" rel="nofollow">C retaceous;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=humid climate&option=203" rel="nofollow">humid climate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=J urassic&option=203" rel="nofollow">J urassic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lake&option=203" rel="nofollow">lake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=M ongolia&option=203" rel="nofollow">M ongolia;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oil shale&option=203" rel="nofollow">oil shale;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=U–Pb age&option=203" rel="nofollow">U–Pb age;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=varve&option=203" rel="nofollow">varve;</a> </p> <div class="translation"> 机译：c Retaceous;潮湿的气候;J urassic;湖;M ongolia;油页岩;U-PB年龄;变形; </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/0704024846983.html">Depositional ages and characteristics of <fc >M</fc>M iddle– <fc >U</fc>U pper <fc >J</fc>J urassic and <fc >L</fc>L ower <fc >C</fc>C retaceous lacustrine deposits in southeastern <fc >M</fc>M ongolia</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hasegawa Hitoshi&option=202" target="_blank" rel="nofollow" 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Evidence of competition between Fc epsilonRI and Fc gammaRIII for limiting amounts of FcR beta and gamma chains.</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=D Dombrowicz&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">D Dombrowicz,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=V Flamand&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">V Flamand,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=I Miyajima&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">I Miyajima,</a> <span>1997</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 epsilonRIα链的缺失会导致FcγRIII依赖性肥大细胞脱颗粒和过敏反应的上调。 Fc epsilonRI和Fc gammaRIII在有限数量的FcR beta和γ链之间竞争的证据。</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/01000131158624.html">Moving the Undeployed TCP Extensions RFC 1072, RFC 1106, RFC 1110, RFC 1145, RFC 1146, RFC 1379, RFC 1644, and RFC 1693 to Historic Status</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=L. Eggert&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">L. Eggert </a> <span>2011</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：移动未处于TCP扩展RFC 1072，RFC 1106，RFC 1110，RFC 1145，RFC 1146，RFC 1379，RFC 1644和RFC 1693到历史状态</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_all-directions_thesis/0201287193020.html">BrieffComparisonfbetweenfWesternfandfChinesefteachinggmethods — —ReflectionsfoffoneflecturefinfInterculturalfCommunicationfcourse</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘庆&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 刘庆</a> <span> <a href="/journal-cn-54023/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 东西南北 </a> </span> <span> . 2017</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_process-industry_thesis/0201259162583.html">磷酸生产过程的FCS设计——基于FF总线技术的FCS系统减少了现场维护量</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=罗云邦&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 罗云邦</a> <span> <a href="/journal-cn-17781/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 流程工业 </a> </span> <span> . 2010</span><span>,第015期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201293376320.html">HFC32/HFC143a/HFC134a在空调/直接式蓄冷空调循环中替代HCFC22的研究</a> <b>[J]</b> <span> <a 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>4. </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>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_refrigeration-air-conditioning_thesis/0201286230969.html">非共沸混合工质HFC-32/HFC-125/HFC-134a在家用空调器中替代HCFC-22的实验研究</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘晓斌&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 刘晓斌</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=蒋能照&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,蒋能照</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=吴兆琳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,吴兆琳</a> <span> <a href="/journal-cn-7719/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 制冷与空调（北京） </a> </span> <span> . 1996</span><span>,第001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/020311995945.html">牛IgG Fc受体（FcγRⅡ，FcγRⅢ）的表达及其结合特性的鉴定</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王丽&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王丽</a> <span> . 2006</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> <ul 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Depositional ages and characteristics of MM iddle– UU pper JJ urassic and LL ower CC retaceous lacustrine deposits in southeastern MM ongolia

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