Interaction of an antecedent fluvial system with early normal fault growth: Implications for syn‐rift stratigraphy, western Corinth rift (Greece)

Hemelsda?l Romain; Ford Mary; Malartre Fabrice; Gawthorpe Rob; Marzo Mariano

摘要

Abstract >Continental ‘overfilled’ conditions during rift initiation are conventionally explained as due to low creation of accommodation compared with sediment supply. Alternatively, sediment supply can be relatively high from the onset of rifting due to an antecedent drainage system. The alluvial Lower Group of the western Plio–Pleistocene Corinth rift is used to investigate the interaction of fluvial sedimentation with early rifting. This rift was obliquely superimposed on the Hellenide mountain belt from which it inherited a significant palaeorelief. Detailed sedimentary logging and mapping of the well‐exposed syn‐rift succession document the facies distributions, palaeocurrents and stratigraphic architecture. Magnetostratigraphy and biostratigraphy are used to date and correlate the alluvial succession across and between fault blocks. From 3·2 to 1·8?Ma, a transverse low sinuosity braided river system flowed north/north‐east to east across east–west‐striking active fault blocks (4 to 7?km in width). Deposits evolved downstream from coarse alluvial conglomerates to fine‐grained lacustrine deposits over 15 to 30?km. The length scale of facies belts is much greater than, and thus not directly controlled by, the width of the fault blocks. At its termination, the distributive river system built small, stacked deltas into a shallow lake margin. The presence of a major antecedent drainage system is supported by: (i) a single major sediment entry point; (ii) persistence of a main channel belt axis; (iii) downstream fining at the scale of the rift basin. The zones of maximum subsidence on individual faults are aligned with the persistent fluvial axis, suggesting that sediment supply influenced normal fault growth. Instead of low accommodation rate during the early rift phase, this study proposes that facies progradation can be controlled by continuous and high sediment supply from antecedent rivers. </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 xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”xml：id =“sed12381-abs-0001”> <标题类型=“main”>抽象</ title> < P>欧陆风格“过满”条件在裂谷启动期间是传统的解释为与沉积物供应相比的低廉的创造。或者，由于前一种引流系统，沉积物供应可以从脱发的开始相对较高。激烈的较低组西部Plio-eNleistocene Corinth Rift用于探讨河流沉降与早期河流的相互作用。这种裂缝倾斜叠加在地狱化的山腰上，它从中遗传了一个重要的古猿。详细的沉积测井和映射曝光良好的Syn-rift连续文件，文档文件分布，古吞并和地层架构。磁通数据和生物数据库迄今为止迄今为止，与故障块之间的冲积连续和相关联。从3·2到1·8？MA，横向低圆润编织河系统流动北/向东向东流过东西，横向撞击活性断层块（宽度为4至7 km）。将沉积物从粗糙的冲积结块中进化到下游，以超过15至30μm的细粒涂层沉积物。面部带的长度尺度远大于故障块的宽度而不是直接控制。在其终止时，分布式河流系统建造了小型，堆积的饮水店进入浅湖边缘。主要的前一种排水系统的存在得到支持：（i）单个主要沉积物入口点; （ii）主沟道带轴的持久性; （iii）在裂缝盆地的等级下澄清的下游罚款。最大沉降区对单个故障的沉降区与持久性氟轴对齐，表明沉积物供应影响了正常的故障增长。本研究提出了在早期裂口期间在早期的裂口阶段期间的住宿率低，而是可以通过来自前所未有的河流的连续和高沉的供应来控制各个进一步。</ 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-28547/'>《Sedimentology: Journal of the International Association of Sedimentologists 》</a> <b style="margin: 0 2px;">|</b><span>2017年第7期</span><b style="margin: 0 2px;">|</b> <span>共41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=Hemelsda?l Romain&option=202" target="_blank" rel="nofollow">Hemelsda?l Romain;</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> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Malartre Fabrice&option=202" target="_blank" rel="nofollow">Malartre Fabrice;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gawthorpe Rob&option=202" target="_blank" rel="nofollow">Gawthorpe Rob;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marzo Mariano&option=202" target="_blank" rel="nofollow">Marzo Mariano;</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>UMR 7358 CNRS‐ULCentre de Recherches Pétrographiques et Géochimiques15 rue Notre Dame des Pauvres BP 20 Vand?uvre les Nancy Cedex 54501 France;</p> <p>UMR 7358 CNRS‐ULCentre de Recherches Pétrographiques et Géochimiques15 rue Notre Dame des Pauvres BP 20 Vand?uvre les Nancy Cedex 54501 France;</p> <p>GeoRessourcesUMR 7359 CNRS‐Université de LorraineVand?uvre‐lès‐Nancy Cedex 54505 France;</p> <p>Basin and Reservoir Studies GroupUniversity of BergenAllegater 41 Bergen 5020 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/165.html" title="地质学">地质学 ;</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=Antecedent river&option=203" rel="nofollow">Antecedent river;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=conglomerate&option=203" rel="nofollow">conglomerate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fault migration&option=203" rel="nofollow">fault migration;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluvial system&option=203" rel="nofollow">fluvial system;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rift basin&option=203" rel="nofollow">rift basin;</a> </p> <div class="translation"> 机译：前河;集团;故障迁移;河流系统;裂缝盆; 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