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首页> 外文期刊>Geochemistry, geophysics, geosystems >Reconstructing the Evolution of the Submarine Monterey Canyon System From Os, Nd, and Pb Isotopes in Hydrogenetic Fe‐Mn Crusts
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Reconstructing the Evolution of the Submarine Monterey Canyon System From Os, Nd, and Pb Isotopes in Hydrogenetic Fe‐Mn Crusts

机译：在氢气Fe-Mn外壳中重建来自OS，Nd和Pb同位素的潜艇蒙特尼峡谷系统的演变

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Abstract > The sources of terrestrial material delivered to the California margin over the past 7 Myr were assessed using 187 Os/ 188 Os, Nd, and Pb isotopes in hydrogenetic ferromanganese crusts from three seamounts along the central and southern California margin. From 6.8 to 4.5 (±0.5) Ma, all three isotope systems show more radiogenic values at Davidson Seamount, located near the base of the Monterey Canyon System, than in Fe‐Mn crusts from the more remote Taney and Hoss Seamounts. At the Taney Seamounts, approximately 225 km farther offshore from Davidson Seamount, 187 Os/ 188 Os values, but not Pb and Nd isotope ratios, also deviate from the Cenozoic seawater curve toward more radiogenic values from 6.8 to 4.5 (±0.5) Ma. However, none of the isotope systems in Fe‐Mn crusts deviate from seawater at Hoss Seamount located approximately 450 km to the south. The regional gradients in isotope ratios indicate that substantial input of dissolved and particulate terrestrial material into the Monterey Canyon System is responsible for the local deviations in the seawater Nd, Pb, and Os isotope compositions from 6.8 to 4.5 (±0.5) Ma. The isotope ratios recorded in Fe‐Mn crusts are consistent with a southern Sierra Nevada or western Basin and Range provenance of the terrestrial material which was delivered by rivers to the canyon. The exhumation of the modern Monterey Canyon must have begun between 10 and 6.8?±?0.5 Ma, as indicated by our data, the age of incised strata, and paleo‐location of the Monterey Canyon relative to the paleo‐coastline. </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> > 使用过去7 MYR的陆地材料的来源进行了评估 187 </ sup> OS / 188 </ sup> OS，ND和PB同位素在沿着中央和南加州边缘的三个海山的氢化铁锰料壳。从6.8到4.5（±0.5）mA，所有三个同位素系统都会在Davidson Seamount上显示更多位于蒙特利峡谷系统的底部的辐射性值，而不是来自遥远的Taney和Hoss Seamounts的Fe-Mn Crusts。在Taney Seamounts，从Davidson Seamount远离海上大约225公里， 187 </ sup> OS / 188 </ sup> OS值，但不是PB和ND同位素比率，也偏离新生代海水曲线，从6.8到4.5（±0.5）mA的更多辐射值。然而，Fe-Mn Crust中的同位素系统都没有偏离Hoss Seamount的海水，位于南部约450公里。同位素率的区域梯度表明，将溶解和颗粒状陆地材料进入蒙特里峡谷系统的大量输入负责海水Nd，Pb和Os同位素组合物的局部偏差为6.8至4.5（±0.5）mA。在Fe-Mn外壳中记录的同位素比与南部的南部塞拉涅达或西部盆地和陆地材料的范围来源一致，该地面材料由河流送到峡谷。现代蒙特雷峡谷的挖掘必须已经开始在10到6.8之间？±0.5 mA，如我们的数据所示，所在地层的年龄，蒙特利峡谷的古地区相对于古海岸线。 </ 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>2017年第11期</span><b style="margin: 0 2px;">|</b><span>共18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=Conrad T. A.&option=202" target="_blank" rel="nofollow">Conrad T. A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nielsen S. G.&option=202" target="_blank" rel="nofollow">Nielsen S. G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Peucker‐Ehrenbrink B.&option=202" target="_blank" rel="nofollow">Peucker‐Ehrenbrink B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Blusztajn J.&option=202" target="_blank" rel="nofollow">Blusztajn J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Winslow D.&option=202" target="_blank" rel="nofollow">Winslow D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hein J. R.&option=202" target="_blank" rel="nofollow">Hein J. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Paytan A.&option=202" target="_blank" rel="nofollow">Paytan A.;</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>University California Santa CruzE&</p> <p>PS Santa Cruz CA USA;</p> <p>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>University California Santa CruzE&</p> <p>PS Santa Cruz CA USA;</p> <p>U.S. Geological Survey PCMSCSanta Cruz CA USA;</p> <p>University California Santa Cruz Institute of Marine SciencesSanta Cruz CA 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=ferromanganese crusts&option=203" rel="nofollow">ferromanganese crusts;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=osmium isotopes&option=203" rel="nofollow">osmium isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=neodymium isotopes&option=203" rel="nofollow">neodymium isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lead isotopes&option=203" rel="nofollow">lead isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Monterey Canyon System&option=203" rel="nofollow">Monterey Canyon System;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Seawater&option=203" rel="nofollow">Seawater;</a> </p> <div class="translation"> 机译：铁曼喃甲板;锇同位素;钕同位素;铅同位素;蒙特雷峡谷系统;海水; </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/0704023360495.html">Reconstructing the Evolution of the Submarine Monterey Canyon System From Os, Nd, and Pb Isotopes in Hydrogenetic Fe‐Mn Crusts</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Conrad T. 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