Predicting Sediment Thickness on Vanished Ocean Crust Since 200 Ma

Dutkiewicz A.; Müller R. D.; Wang X.; OCallaghan S.; Cannon J.; Wright N. M.

摘要

Abstract >Tracing sedimentation through time on existing and vanished seafloor is imperative for constraining long‐term eustasy and for calculating volumes of subducted deep‐sea sediments that contribute to global geochemical cycles. We present regression algorithms that incorporate the age of the ocean crust and the mean distance to the nearest passive margin to predict sediment thicknesses and long‐term decompacted sedimentation rates since 200 Ma. The mean sediment thickness decreases from ～220 m at 200 Ma to a minimum of ～140 m at 130 Ma, reflecting the replacement of old Panthalassic ocean floor with young sediment‐poor mid‐ocean ridges, followed by an increase to ～365 m at present‐day. This increase reflects the accumulation of sediments on ageing abyssal plains proximal to passive margins, coupled with a decrease in the mean distance of any parcel of ocean crust to the nearest passive margin by over 700 km, and a doubling of the total passive margin length at present‐day. Mean long‐term sedimentation rates increase from ～0.5 cm/ky at 160 Ma to over 0.8 cm/ky today, caused by enhanced terrigenous sediment influx along lengthened passive margins, superimposed by the onset of ocean‐wide carbonate sedimentation. Our predictive algorithms, coupled to a plate tectonic model, provide a framework for constraining the seafloor sediment‐driven eustatic sea‐level component, which has grown from ～80 to 210 m since 120 Ma. This implies a long‐term sea‐level rise component of 130 m, partly counteracting the contemporaneous increase in ocean basin depth due to progressive crustal ageing. </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> >通过现有和消失的海底的时间追踪沉积，对于限制长期果汁和计算促进全球地球化学循环的低压深海沉积物的诱导。我们将回归算法纳入海底的年龄，与最近的被动边际的平均距离预测自200 mA以来预测沉积物厚度和长期分解沉降率。平均沉积物厚度从200 mA的〜220米降低至最低约140米的130 mA，反映了用幼砂贫瘠的中海山脊的旧诗歌海洋地板，然后增加到365米今天。这种增加反映了沉积物沉积物对被动边缘的衰老深度平原的沉积物，同时加上任何海洋地壳到最近的被动边距的平均距离减少到超过700公里，以及总被动边缘长度的加倍今天。根据延长的被动边距，由延长的被动边距增加，平均长期沉降率从160 mA达到超过0.8厘米/ ky增加到超过0.8厘米/ ky。我们的预测算法耦合到板构造模型，提供了一种限制海底沉积物驱动的突出部分量的框架，其自120 mA以来从〜80至210米生长。这意味着长期的海平面上升组分为130米，部分地抵消了由于进步的地壳老化导致的海洋盆地深度的同时增加。</ 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12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=Dutkiewicz A.&option=202" target="_blank" rel="nofollow">Dutkiewicz A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Müller R. D.&option=202" target="_blank" rel="nofollow">Müller R. D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang X.&option=202" target="_blank" rel="nofollow">Wang X.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=OCallaghan S.&option=202" target="_blank" rel="nofollow">OCallaghan S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cannon J.&option=202" target="_blank" rel="nofollow">Cannon J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wright N. M.&option=202" target="_blank" rel="nofollow">Wright N. M.;</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>EarthByte Group School of GeosciencesUniversity of SydneySydney NSW Australia;</p> <p>EarthByte Group School of GeosciencesUniversity of SydneySydney NSW Australia;</p> <p>Data61 CSIRO Australian Technology ParkEveleigh NSW Australia;</p> <p>Data61 CSIRO Australian Technology ParkEveleigh NSW Australia;</p> <p>EarthByte Group School of GeosciencesUniversity of SydneySydney NSW Australia;</p> <p>EarthByte Group School of GeosciencesUniversity of SydneySydney NSW Australia;</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=sediment thickness&option=203" rel="nofollow">sediment thickness;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sedimentation rate&option=203" rel="nofollow">sedimentation rate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=eustasy&option=203" rel="nofollow">eustasy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=plate tectonics&option=203" rel="nofollow">plate tectonics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=machine learning&option=203" rel="nofollow">machine learning;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ocean basin evolution&option=203" rel="nofollow">ocean basin evolution;</a> </p> <div class="translation"> 机译：沉积物厚度;沉降率;南瓜;板构造;机器学习;海洋盆地进化; </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/0704023360772.html">Predicting Sediment Thickness on Vanished Ocean Crust Since 200 Ma</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dutkiewicz A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Dutkiewicz A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Müller R. 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Dutkiewicz&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">A. Dutkiewicz,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=R. D. Müller&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">R. D. Müller,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=X. Wang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">X. Wang,</a> <span>2017</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：预测自200 mA以来消失的海洋地壳上的沉积物厚度</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-oceanologica-sinica_thesis/0201253881896.html">由东海、黄海沉积物中有机碳含量及稳定同位素组成重建200 a以来初级生产力历史记录</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=蔡德陵&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 蔡德陵</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙耀&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,孙耀</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张小勇&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张小勇</a> <span> <a href="/journal-cn-4977/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋学报（中文版） </a> </span> <span> . 2014</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201296457668.html">赤道西太平洋暖池区更新世以来的生源沉积物沉积特征及其古海洋学意义</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王汝建&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王汝建</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=成鑫荣&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,成鑫荣</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘传联&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘传联</a> <span> <a href="/journal-cn-56825/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋地质与第四纪地质 </a> </span> <span> . 2001</span><span>,第4期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_chinese-journal-polar-research_thesis/0201253932358.html">南极15ka以来海洋沉积物的环境磁学研究</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=侯红明&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 侯红明</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王保贵&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王保贵</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=汤贤赞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,汤贤赞</a> <span> <a href="/journal-cn-4982/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 极地研究 </a> </span> <span> . 1997</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_chinese-journal-geophysics_thesis/0201253037126.html">20Ma以来Mohns洋中脊的非对称扩张速率与地壳结构</a> <b>[J]</b> <span> <a 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