The start‐up of the Dolomia Principale/Hauptdolomit carbonate platform (Upper Triassic) in the eastern Southern Alps

机译：在南部阿尔卑斯州东部的Dolomia Principale / Hauptdolomit碳酸盐平台（上三叠系）的启动

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Abstract >Wide carbonate platform environments developed on the western passive margin of the Tethys during the Late Triassic, after a major climate change (Carnian Pluvial Episode) that produced a crisis of high‐relief microbial carbonate platforms. The peritidal succession of this epicontinental platform (Dolomia Principale/Hauptdolomit, Dachstein Limestone) is widespread in the Mediterranean region. However, the start‐up stage is not fully understood. The original platform to basin depositional geometries of the system have been studied in the north‐eastern Southern Alps, close to the Italian/Slovenian boundary where they are exceptionally preserved. Sedimentological features have been investigated in detail by measuring several stratigraphic sections cropping out along an ideal depositional profile. The analysis of the facies architecture allowed reconstruction of the palaeoenvironments of the Dolomia Principale platform during its start‐up and early growth stages in the late Carnian. The carbonate platform was characterized by an outer platform area, connected northward to steep slopes facing a relatively deep basin. Southward, the outer platform was connected to inner sheltered environments by a narrow, often emerged shelf crest. Behind this zone, carbonate sedimentation occurred in shallow lagoons and tidal flats, passing inward to a siliciclastic mudflat. The Dolomia Principale platform was initially aggrading and able to keep pace with a concomitant sea‐level rise, and then prograding during the late Carnian. This stratigraphic interval was correlated with the Tuvalian succession of the Dolomites, allowing depiction of the depositional system on a wide scale of hundreds of kilometres. This large‐scale depositional system presents features in common with some Palaeozoic and Mesozoic carbonate build‐up </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 =“sed12416-abs-0001”xml：lang =“en”> <标题类型=“main” >摘要</ title> >在晚期三叠纪的Thethys西方被动边缘开发的宽碳平台环境，经过一系列重大的气候变化（卡尼亚普尔普利亚州），产生了高浮雕微生物碳酸盐平台的危机。这种综合体平台（Dolomia Principale / Hauptdolomit，Dachstein石灰石）的突出继承在地中海地区广泛普及。但是，启动阶段尚未完全理解。在南部的南部南部的南部阿尔卑斯州南部的盆地沉积几何形状的原始平台，靠近意大利/斯洛文尼亚边界，在这里尤其保留。已经通过测量沿理想的沉积轮廓造成的若干地层部分来详细研究了沉积物特征。在晚期Carnian的启动和早期生长阶段，对面部建筑的分析允许重建Dolomia Prinipale平台的古环境。碳酸盐平台的特征在于外平台面积，向北连接到陡峭的坡度面向相对深的盆地。向南，外部平台通过狭窄的，经常出现的架子嵴连接到内部遮蔽的环境。在该区域后面，碳酸盐沉降发生在浅泻湖和潮汐平面上，向内传递到硅砾泥浆。 Dolomia Principale平台最初致力于加剧，能够与伴随的海平面上升保持步伐，然后在晚期肉食中促进。该地层间隔与白云岩的三方大连连续相关，允许在宽度的数百公里上描绘沉积系统。这种大规模的沉积系统与某些古生物和中生代碳酸盐堆积有共同的特征 </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4期</span><b style="margin: 0 2px;">|</b><span>共35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=Caggiati Marcello&option=202" target="_blank" rel="nofollow">Caggiati Marcello;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gianolla Piero&option=202" target="_blank" rel="nofollow">Gianolla Piero;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Breda Anna&option=202" target="_blank" rel="nofollow">Breda Anna;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Celarc Bogomir&option=202" target="_blank" rel="nofollow">Celarc Bogomir;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Preto Nereo&option=202" target="_blank" rel="nofollow">Preto Nereo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Eberli Gregor&option=202" target="_blank" rel="nofollow">Eberli Gregor;</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>Physics and Earth Sciences DepartmentUniversity of FerraraVia Saragat 1 Ferrara 44100 Italy;</p> <p>Physics and Earth Sciences DepartmentUniversity of FerraraVia Saragat 1 Ferrara 44100 Italy;</p> <p>Geosciences DepartmentUniversity of PaduaVia Gradenigo 6 Padua 35131 Italy;</p> <p>Geological Survey of SloveniaDimi?eva ulica 14 Ljubljana SI‐1000 Slovenia;</p> <p>Geosciences DepartmentUniversity of PaduaVia Gradenigo 6 Padua 35131 Italy;</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=Carbonate factories&option=203" rel="nofollow">Carbonate factories;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=carbonate platforms&option=203" rel="nofollow">carbonate platforms;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=facies model&option=203" rel="nofollow">facies model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=microbialites&option=203" rel="nofollow">microbialites;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Triassic&option=203" rel="nofollow">Triassic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Western Tethys&option=203" rel="nofollow">Western Tethys;</a> </p> <div class="translation"> 机译：碳酸盐工厂;碳酸盐平台;相模型;微生物石;三叠纪;西部的特质; 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Parker </a> <span>2010</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：亚利桑那州石化森林国家公园南部的Sonsela岩层（上部三叠纪Chinle地层）的修订地层学</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/0100033488093.html ">Forward modelling of carbonate platforms:Sedimentological and diagenetic constraints from an application to a flat-topped greenhouse platform (Triassic, Southern Alps, Italy)</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Berra, F.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Berra, F.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lanfranchi, A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lanfranchi, A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Smart, P.L.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Smart, P.L.,</a> <span>2016</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：碳酸盐平台的正演模拟：从应用到平顶温室平台（三叠纪，南阿尔卑斯山，意大利）的沉积学和成岩学约束</span> </p> </li> <li> <div> <b>8. </b><a class="enjiyixqcontent" href="/ntis-science-report_ad_thesis/020711570056.html">Developing Carbonate Platforms: Southern Gulf of Suez, Northern Red Sea.</a> <b>[R] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Roberts, H. 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