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首页> 外文期刊>Geochemistry, geophysics, geosystems >Dating Clinopyroxene Phenocrysts in Submarine Basalts Using 4040 Ar/ 3939 Ar Geochronology
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Dating Clinopyroxene Phenocrysts in Submarine Basalts Using 4040 Ar/ 3939 Ar Geochronology

机译:使用潜艇玄武岩的延迟临床异癸酯 40 40 ar / 39 39 AR地理学

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摘要

Abstract > Dating submarine basalts using 40 Ar/ 39 Ar geochronology is often hindered by a lack of potassium‐bearing phenocrystic phases and severe alteration in the groundmass. Clinopyroxene is a common phenocrystic phase in seafloor basalts and is highly resistive to low‐temperature alteration. Here we show that clinopyroxene phenocrysts separated from marine basalts are a viable phase for 40 Ar/ 39 Ar incremental heating age determinations. We provide results from a pilot study comprising 16 age experiments from nine clinopyroxene separates, five of which from samples with dated coeval phases. The clinopyroxene ages range from 11.5 to 112?Ma with relatively high uncertainties (ranging from 0.8% to 7.1%; median of 1.9%) compared to more traditional phases. The clinopyroxene age plateaus form at low to moderate temperature steps and are characterized by relatively elevated K/Ca of 0.002–0.4, suggesting that other K‐bearing phases hosted within the clinopyroxene are likely degassing to yield the 40 Ar/ 39 Ar age information. There are three possible origins for the K and corresponding 40 Ar* including films of trapped melt/nanomineral inclusions along grain defects, secondary melt inclusion bands, or variations in degassing behaviors between lower and higher crystalline Ca pyroxene phases. Regardless of the source of the K, the age determinations are successful with 75% of the experiments producing long plateaus (60% 39 Ar released) with mean square of the weighted deviations ranging from 0.6 to 1.5 and probability of fit values 0.05. We conclude that clinopyroxene dating by the 40 Ar/ 39 Ar method has the potential to provide a wealth of information for previously undated, altered seafloor lithologies and continental equivalents. </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”> <标题类型=“main”>抽象</ title> > 使用潜艇基础使用 40 </ sup> ar / 39 </ sup> AR地质族学通常受到含钾的苯杂交阶段和造型中的严重改变的阻碍。 Clinocogoxene是海底底部常见的苯杂交相,对低温改变具有高阻电性。在这里,我们表明,与海洋沼气分离的Clinopogoxene PhenCrysts是一种可行的阶段 40 </ sup> ar / 39 </ sup> AR增量加热时代测定。我们提供的试点研究结果包括来自九个临床分离的16岁的年龄实验,其中5个来自患有患有群阶段的样品。与更多传统阶段相比,临床的临床增长的范围为11.5至112·mA,相对高的不确定性(范围为0.8%至7.1%;中位数为1.9%)。在低至中等温度阶段的临床成功率在低至中等温度阶段,其特征在于0.002-0.4的k / ca相对升高,表明在临床内宿主的其他k轴承阶段可能脱气以产生脱气 40 </ sup> ar / 39 </ sup> AR年龄信息。 K和相应有三种可能的起源 40 </ sup> ar *包括沿谷物缺陷,次级熔体包合物或脱气行为的血液熔体/纳米型夹杂物的薄膜,或在下晶的Ca聚烯相之间脱气行为的变化。无论k的来源如何,年龄测定都是成功的75%的实验,生产长期强韧(& 60% 39 </ sup> AR释放)加权偏差的平均方形,范围为0.6至1.5,拟合值的概率& 0.05。我们得出结论,Clinoceoxene由此约会 40 </ sup> ar / 39 </ sup> AR方法有可能为先前未结过的,改变的海底岩性和大陆当量提供丰富的信息。 </ p> </摘要> </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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2019年第2期</span><b style="margin: 0 2px;">|</b><span>共13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=Konrad Kevin&option=202" target="_blank" rel="nofollow">Konrad Kevin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Koppers Anthony A. P.&option=202" target="_blank" rel="nofollow">Koppers Anthony A. P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Balbas Andrea M.&option=202" target="_blank" rel="nofollow">Balbas Andrea M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Miggins Daniel P.&option=202" target="_blank" rel="nofollow">Miggins Daniel P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heaton Daniel E.&option=202" target="_blank" rel="nofollow">Heaton Daniel E.;</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>College of Earth Ocean and Atmospheric ScienceOregon State UniversityCorvallis OR USA;</p> <p>College of Earth Ocean and Atmospheric ScienceOregon State UniversityCorvallis OR USA;</p> <p>College of Earth Ocean and Atmospheric ScienceOregon State UniversityCorvallis OR USA;</p> <p>College of Earth Ocean and Atmospheric ScienceOregon State UniversityCorvallis OR USA;</p> <p>College of Earth Ocean and Atmospheric ScienceOregon State UniversityCorvallis OR USA;</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><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></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=40 Ar/ 39 Ar geochronology&option=203" rel="nofollow">40 Ar/ 39 Ar geochronology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=clinopyroxene&option=203" rel="nofollow">clinopyroxene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=basalts&option=203" rel="nofollow">basalts;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=melt inclusions&option=203" rel="nofollow">melt inclusions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=submarine alteration&option=203" rel="nofollow">submarine alteration;</a> </p> <div class="translation"> 机译:40 AR / 39 AR地理学;Clinococoxene;沼泽;熔体夹杂物;潜艇改变; </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/0704023360747.html">Dating Clinopyroxene Phenocrysts in Submarine Basalts Using <sup >4040 Ar/ <sup >3939 Ar Geochronology</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Konrad Kevin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Konrad Kevin,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Koppers Anthony A. 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</li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_geology-in-china_thesis/0201252104988.html">云南个旧卡房蚀变玄武岩金云母40Ar-39Ar同位素年龄研究及意义</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张娟&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张娟</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=毛景文&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,毛景文</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=程彦博&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,程彦博</a> <span> <a href="/journal-cn-4800/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国地质 </a> </span> <span> . 2012</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-petrologica-sinica_thesis/0201252026799.html">地幔包体金云母~(40)Ar/~(39)Ar年龄对玄武岩浆喷发结束时间的约束</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杜世俊&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 杜世俊</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=徐兴旺&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,徐兴旺</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨列坤&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨列坤</a> <span> <a href="/journal-cn-4795/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 岩石学报 </a> </span> <span> . 2009</span><span>,第012期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_earth-science-frontiers_thesis/0201253156034.html">藏北双湖鄂柔地区变质岩和玄武岩的40Ar/39Ar年龄及其意义</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王立全&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 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