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The Paleozoic Evolution of the Olga Basin Region, Northern Barents Sea: A Link to the Timanian Orogeny

机译：奥尔加盆地地区的古生代演变，北方的小人海洋：桃尾洋底山脉的联系

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Abstract >The evolution of the Olga Basin region in the northern Norwegian Barents Sea and its relation to the Caledonian and Timanian orogenies is poorly understood due to sparse geophysical data and the lack of well control. In 2015, the German Federal Institute for Geosciences and Natural Resources (BGR) acquired deep multichannel seismic lines as well as gravity and magnetic data. The new seismic data reveal that the Olga and S?rkapp Basins evolved as a W‐E striking half‐graben system along a major normal fault in the north and a smaller normal fault in the south, respectively. Deep crustal undulating high‐amplitude reflections below the Olga and S?rkapp Basins coincide with W‐E striking local magnetic maxima and may imply that the basins evolved on top of old collisional fabrics. The absence of major compressional deformation implies a post‐Caledonian onset of subsidence. The W‐E structural configuration of the sedimentary basins is difficult to reconcile with an earlier proposed NE striking Caledonian branch in the northern Barents Sea. Instead, the orientation of the Olga and S?rkapp Basins lines up with Timanian structural trends from the Pechora Basin. We propose that the Olga and S?rkapp Basins experienced transtensional deformation during the late Devonian/early Carboniferous NE‐SW regional extension phase whereby inherited Timanian lineaments controlled the final W‐E basin configuration. A salient pre‐Caledonian Olga‐S?rkapp crustal block in the central Barents Sea would also explain the recently proposed NNW rotation of Caledonian nappes and thrust sheets in the southwestern Barents Sea. </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> >北部挪威人的奥尔加盆地区域的演变及其与喀里多尼亚人和仙山洋洋的关系由于稀疏地球物理数据和缺乏良好的控制而难以理解。 2015年，德国联邦地球科学研究所和自然资源研究所（BGR）获得了深度多通道地震线以及重力和磁数据。新的地震数据揭示了Olga和S？Rkapp盆地沿着北方的主要正常断层和南部的较小普通断层，分别演变为一个W-E醒目的半重争夺系统。奥尔加和S以下的深层地壳起伏的高振幅反射率与局部磁性最大值相一致，局部可能意味着盆地在旧碰撞织物的顶部进化。没有重大压缩变形意味着后喀里多尼亚人的沉降发作。沉积盆地的W-E结构配置难以与北方小人海上的早期提出的尼斯尖头喀里多尼亚分支协调。相反，Olga和S的取向与Pechora盆地的蒂纳尼亚结构趋势引进了奥尔格和S？rkapp盆地。我们提出了Olga和S？Rkapp盆地在晚德文/早期石炭纪的Ne-SW区域延伸阶段经历了悲剧性变形，从而继承了蒂纳尼亚队列控制了最终的W-E盆地配置。突出的喀尔德·奥尔加尔（Rkapp Chartal Block）在中央小理海地中也将解释最近提出的Caledonian Nappes和Shortusth Marents海的推力板的NNW旋转。</ 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16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=Klitzke P.&option=202" target="_blank" rel="nofollow">Klitzke P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Franke D.&option=202" target="_blank" rel="nofollow">Franke D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ehrhardt A.&option=202" target="_blank" rel="nofollow">Ehrhardt A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lutz R.&option=202" target="_blank" rel="nofollow">Lutz R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Reinhardt L.&option=202" target="_blank" rel="nofollow">Reinhardt L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heyde I.&option=202" target="_blank" rel="nofollow">Heyde I.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Faleide J. I.&option=202" target="_blank" rel="nofollow">Faleide J. I.;</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>Federal Institute for Geosciences and Natural Resources (BGR)Hannover Germany;</p> <p>Federal Institute for Geosciences and Natural Resources (BGR)Hannover Germany;</p> <p>Federal Institute for Geosciences and Natural Resources (BGR)Hannover Germany;</p> <p>Federal Institute for Geosciences and Natural Resources (BGR)Hannover Germany;</p> <p>Federal Institute for Geosciences and Natural Resources (BGR)Hannover Germany;</p> <p>Federal Institute for Geosciences and Natural Resources (BGR)Hannover Germany;</p> <p>Research Centre for Arctic Petroleum Exploration (ARCEx)UiT ‐ The Arctic University of NorwayTroms? Norway;</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=Barents Sea&option=203" rel="nofollow">Barents Sea;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Timanian orogeny&option=203" rel="nofollow">Timanian orogeny;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Caledonian orogeny&option=203" rel="nofollow">Caledonian orogeny;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismic reflection data&option=203" rel="nofollow">seismic reflection data;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=gravity data&option=203" rel="nofollow">gravity data;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magnetic data&option=203" rel="nofollow">magnetic data;</a> </p> <div class="translation"> 机译：野生海洋;蒂纳尼亚orenogy;喀里多尼亚山脉;地震反射数据;重力数据;磁数据; </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 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