The Toarcian–Bajocian deltaic system in the North German Basin: Subsurface mapping of ancient deltas‐morphology, evolution and controls

Zimmermann Jens; Franz Matthias; Schaller Astrid; Wolfgramm Markus

摘要

Abstract >Research focussing on the morphology and morphodynamics of modern river deltas has contributed much to the understanding of reservoir geometry and prediction of hydrocarbon splays and deep geothermal aquifers. The interplay of allogenic and autogenic controls results in complex histories of modern river deltas comprising subsequent regressive and transgressive stages of delta formation. The application to ancient examples is still ambiguous and in particular the detailed morphological description of ancient deltas is often hampered by limited subsurface data. This basin‐scale study employs a data set of 15 cored wells and more than 450 logged wells in combination with lithofacies, biofacies and architectural analysis to reconstruct high‐resolution subsurface facies and sand thickness maps of the Toarcian–Bajocian deltaic system in the North German Basin. The results of this study show the evolution from smaller elongate river‐dominated delta types in the Lower and Upper Toarcian (15?000 to 20?000?km2), and a larger lobate river‐dominated delta in the Upper Aalenian (40?000?km2) to a cuspate mixed river‐dominated?and wave‐modified delta in the Upper Bajocian (25?000?km2). River‐dominated deltas are formed of distributary deltaic channel belts and associated sheetsands of the delta plain and distributary‐mouth bar complexes with bar‐finger sand architectures of the delta front. Increasing marine processes in the Bajocian resulted in modification of delta complexes forming a shoreface setting with foreshoals, arc‐like chains of ooid‐bearing barrier shoals and back barrier lagoons. The complex history of the Toarcian–Bajocian?deltaic system was mainly controlled by allogenic sea‐level fluctuations that triggered the delta progradation and subordinately by allogenic basin reorganization. Autogenic </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 =“sed12410-abs-0001”xml：lang =“en”> <标题类型=“main” >摘要</标题> >对现代河三角洲的形态学和形态学性的研究贡献了对储层几何形状和碳氢化合物展和深层地热含水层的预测。同种异体和容易对照的相互作用导致复杂历史的现代河δ，包括随后的δ形成的回归和近级阶段。在古代的例子中的应用仍然是含糊不清的，特别是古代斯特拓的详细形态学描述经常受到限制地下数据的阻碍。该盆地研究采用了15个芯片井的数据集和450多井，与岩散，生物缩探和建筑分析组合，以重建北德国Toarcian-Bajocian Deltaic系统的高分辨率地下相和砂厚度图盆地。该研究的结果表明，下部和上部和上部和上部到20〜000？KM2）中较小的细长河主导的三角洲类型的演变（15？000到20？KM2），并且在Aalenian上部的较大裂片河主导的三角洲（40？000当尖锐的河流主导的尖瓣KM2）？和上部Bajocian（25 000？KM2）中的波改进的三角洲。河主导的斯特拓是由分销日期通道带形成的三角洲平原和分销嘴巴复合物的相关板条，带有三角形前面的拨打砂架构。增加了Bajocian中的海洋过程导致δ配合物的改变，形成具有预示物的横向设置的横向设置，壳体屏障浅滩和后屏障泻湖的弧形链。 Toarcian-Bajocian的复杂历史主要由同种异体海平面波动来控制，以引发三角洲盆地促成并通过同种异体盆地重组来制止。自动化 </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>2018年第3期</span><b style="margin: 0 2px;">|</b><span>共34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=Zimmermann Jens&option=202" target="_blank" rel="nofollow">Zimmermann Jens;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Franz Matthias&option=202" target="_blank" rel="nofollow">Franz Matthias;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schaller Astrid&option=202" target="_blank" rel="nofollow">Schaller Astrid;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wolfgramm Markus&option=202" target="_blank" rel="nofollow">Wolfgramm Markus;</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>Department of GeologyTU Bergakademie FreibergBernhard‐von‐Cotta‐Stra?e 2 09599 Freiberg Germany;</p> <p>Geowissenschaftliches Zentrum der Universit?t G?ttingenGoldschmidtstra?e 3 37077 G?ttingen Germany;</p> <p>Federal Institute for Geosciences and Natural ResourcesWilhelmstr. 25‐30 13593 Berlin Germany;</p> <p>Geothermie Neubrandenburg GmbHSeestrasse 7a 17033 Neubrandenburg Germany;</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=Allogenic deltaic process change&option=203" rel="nofollow">Allogenic deltaic process change;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=autogenic deltaic process change&option=203" rel="nofollow">autogenic deltaic process change;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=elongate river‐dominated delta&option=203" rel="nofollow">elongate river‐dominated delta;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lithofacies analysis&option=203" rel="nofollow">lithofacies analysis;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lobate river‐dominated delta&option=203" rel="nofollow">lobate river‐dominated delta;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lobe abandonment&option=203" rel="nofollow">lobe abandonment;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lobe shifting&option=203" rel="nofollow">lobe shifting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subsidence&option=203" rel="nofollow">subsidence;</a> </p> <div class="translation"> 机译：同种异体的Deltaic工艺变化;自闭虫过程变化;细长河主导的三角洲;锂外分析;裂片河主导的三角洲;叶遗弃;叶片移位;沉降; 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</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：在源代码控制系统中确定函数调用图的空间局部性中的增量 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704024308599','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="关闭" onclick="$('.journalsub-pop-up').hide()"> <p 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