Formation of the Iberian‐European Convergent Plate Boundary Fault and Its Effect on Intraplate Deformation in Central Europe

Dielforder Armin; Frasca Gianluca; Brune Sascha; Ford Mary

摘要

Abstract >With the Late Cretaceous onset of Africa‐Iberia‐Europe convergence Central Europe experienced a pulse of intraplate shortening lasting some 15–20 Myr. This deformation event documents area‐wide deviatoric compression of Europe and has been interpreted as a far‐field response to Africa‐Iberia‐Europe convergence. However, the factors that governed the compression of Europe and conditioned the transient character of the deformation event have remained unclear. Based on mechanical considerations, numerical simulations, and geological reconstructions, we examine how the dynamics of intraplate deformation were governed by the formation of a convergent plate boundary fault between Iberia and Europe. During the Late Cretaceous, plate convergence was accommodated by the inversion of a young hyperextended rift system separating Iberia from Europe. Our analysis shows that the strength of the lithosphere beneath this rift was initially sufficient to transmit large compressive stresses far into Europe, though the lithosphere beneath the rift was thinned and thermally weakened. Continued convergence forced the formation of the plate boundary fault between Iberia and Europe. The fault evolved progressively and constituted a lithospheric‐scale structure at the southern margin of Europe that weakened rheologically. This development caused a decrease in mechanical coupling between Iberia and Europe and a reduction of compressional far field stresses, which eventually terminated intraplate deformation in Central Europe. Taken together, our findings suggest that the Late Cretaceous intraplate deformation event records a high force transient that relates to the earliest strength evolution of a lithospheric‐scale plate boundary fault. </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> 与非洲 - 伊贝利亚 - 欧洲的后期白垩纪发作中央欧洲经历了持续约15-20元的血管内膜缩短的脉搏。这种变形事件文件的欧洲领域广泛的偏离压缩，并被解释为对非洲 - 伊比利亚欧洲融合的远地反应。然而，治理欧洲压缩和调节变形事件的瞬态特征的因素仍然不清楚。基于机械考虑，数值模拟和地质重建，我们研究了Intraink变形的动态如何通过形成伊比利亚和欧洲之间的收敛板边界断层来治理。在晚餐期间，通过欧洲伊比利亚分离伊比利亚的年轻过度伸展系统的反演，可以容纳板融合。我们的分析表明，这种裂谷下方的岩石圈的强度最初是足以将大型压缩应力传递到欧洲的大型压缩应力，尽管裂缝下方的岩石圈变薄并热削弱。持续的融合强制形成伊比利亚和欧洲之间的板边界断层。故障逐步演变，并构成了在欧洲南部的岩石尺度结构，在流变上削弱了流变。这一发展导致伊比利亚和欧洲之间的机械耦合减少，减少了压缩远场应力，最终终止了中欧的内衬变形。我们的研究结果表明，晚期白垩纪内部变形事件记录了高力瞬态，与岩石尺度板边界断层的最早的强度演变有关。</ 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5期</span><b style="margin: 0 2px;">|</b><span>共23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=Dielforder Armin&option=202" target="_blank" rel="nofollow">Dielforder Armin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Frasca Gianluca&option=202" target="_blank" rel="nofollow">Frasca Gianluca;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Brune Sascha&option=202" target="_blank" rel="nofollow">Brune Sascha;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ford Mary&option=202" target="_blank" rel="nofollow">Ford Mary;</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>Helmholtz Centre PotsdamGFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>Centre de Recherches Pétrographiques et GéochimiquesVand?uvre‐lès‐Nancy France;</p> <p>Helmholtz Centre PotsdamGFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>Centre de Recherches Pétrographiques et GéochimiquesVand?uvre‐lès‐Nancy France;</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=intraplate deformation&option=203" rel="nofollow">intraplate deformation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=orogeny&option=203" rel="nofollow">orogeny;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=plate boundary fault&option=203" rel="nofollow">plate boundary fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=plate coupling force&option=203" rel="nofollow">plate coupling force;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pyrenees&option=203" rel="nofollow">Pyrenees;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lithosphere dynamics&option=203" rel="nofollow">lithosphere dynamics;</a> </p> <div class="translation"> 机译：腔内变形;orogeny;板边界断层;板耦合力;比利牛斯;岩石圈动态; 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