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首页> 外文期刊>Sedimentology: Journal of the International Association of Sedimentologists >Flow dynamics at the origin of thin clayey sand lacustrine turbidites: Examples from Lake Hazar, Turkey
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Flow dynamics at the origin of thin clayey sand lacustrine turbidites: Examples from Lake Hazar, Turkey

机译：薄粘土砂湖浑浊浊度起源的流动动力学：来自土耳其湖的实例

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Abstract >Turbidity currents and their deposits can be investigated using several methods, i.e. direct monitoring, physical and numerical modelling, sediment cores and outcrops. The present study focused on thin clayey sand turbidites found in Lake Hazar (Turkey) occurring in eleven clusters of closely spaced thin beds. Depositional processes and sources for three of those eleven clusters are studied at three coring sites. Bathymetrical data and seismic reflection profiles are used to understand the specific geomorphology of each site. X‐ray, thin sections and CT scan imagery combined with grain‐size, geochemical and mineralogical measurements on the cores allow characterization of the turbidites. Turbidites included in each cluster were produced by remobilization of surficial slope sediment, a process identified in very few studies worldwide. Three types of turbidites are distinguished and compared with deposits obtained in flume studies published in the literature. Type 1 is made of an ungraded clayey silt layer issued from a cohesive flow. Type 2 is composed of a partially graded clayey sand layer overlain by a mud cap, attributed to a transitional flow. Type 3 corresponds to a graded clayey sand layer overlain by a mud cap issued from a turbulence‐dominated flow. While the published experimental studies show that turbulence is damped by cohesion for low clay content, type 3 deposits of this study show evidence for a turbulence‐dominated mechanism despite their high clay content. This divergence may in part relate to input variables, such as water chemistry and clay mineralogy, that are not routinely considered in experimental studies. Furthermore, the large sedimentological variety observed in the turbidites from one coring site to another is related to the evolution of a sediment flow within a field‐scale basin made of a complex physiography that cannot be tackled by flume experiments. </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 =“sed12380-abs-0001”> <标题类型=“main”>抽象</ title> < P>可以使用几种方法来研究浊度和它们的沉积物，即直接监测，物理和数值建模，沉积物核和露头。目前的研究重点是薄粘土砂浊，在苏必拉湖（土耳其）中发生的薄膜薄薄的薄床。在三个取纱部位研究了三个簇中的三种群中的沉积过程和来源。浴多种数据和地震反射型材用于了解每个站点的特定地貌。 X射线，薄剖面和CT扫描图像与芯上的晶粒尺寸，地球化学和矿物学测量相结合，允许浊度表征。通过重新染色表层斜率沉积物，产生了每个簇中包含的浊度，在全世界少数研究中发现的过程。区分三种类型的浊度，并与文献中发表的水槽研究中获得的沉积物进行比较。类型1由从粘性流动发出的未非粘土淤泥层制成。类型2由泥帽覆盖的部分分级夹层砂层组成，归因于过渡流程。类型3对应于由湍流主导流的泥浆帽覆盖的分级粘土砂层。虽然已发表的实验研究表明，湍流被用于低粘土含量的粘合，但这项研究的3型沉积物显示出湍流主导机制的证据，尽管它们具有高粘土含量。这种分歧部分可以部分地涉及输入变量，例如水化学和粘土矿物学，其在实验研究中不常规考虑。此外，从一个取牙部位到另一个牙齿位点的浊度观察到的大型沉积学变化与泥沙流量的沉积物流动的演变有关，该粪便盆腔内不能被水槽实验所缠结的复杂的物理图。</ 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28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=Hage Sophie&option=202" target="_blank" rel="nofollow">Hage Sophie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hubert‐Ferrari Aurélia&option=202" target="_blank" rel="nofollow">Hubert‐Ferrari Aurélia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lamair Laura&option=202" target="_blank" rel="nofollow">Lamair Laura;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Av?ar Ula?&option=202" target="_blank" rel="nofollow">Av?ar Ula?;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=El Ouahabi Meriam&option=202" target="_blank" rel="nofollow">El Ouahabi Meriam;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Van Daele Maarten&option=202" target="_blank" rel="nofollow">Van Daele Maarten;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Boulvain Frédéric&option=202" target="_blank" rel="nofollow">Boulvain Frédéric;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ali Bahri Mohamed&option=202" target="_blank" rel="nofollow">Ali Bahri Mohamed;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Seret Alain&option=202" target="_blank" rel="nofollow">Seret Alain;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Plenevaux Alain&option=202" target="_blank" rel="nofollow">Plenevaux Alain;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Baas Jaco&option=202" target="_blank" rel="nofollow">Baas Jaco;</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 GeographyUnivsersity of LiegeQuartier Village 4 Clos Mercator 3 4000 Liege Belgium;</p> <p>Department of GeographyUnivsersity of LiegeQuartier Village 4 Clos Mercator 3 4000 Liege Belgium;</p> <p>Department of GeographyUnivsersity of LiegeQuartier Village 4 Clos Mercator 3 4000 Liege Belgium;</p> <p>King Abdullah University of Science and TechnologyThuwal 23955 Saudi Arabia;</p> <p>Geographisches InstitutAlbertus‐Magnus‐Platz23955 K?ln Germany;</p> <p>Renard Centre of Marine GeologyGeological Institute Ghent UniversityKrijgslaan 281 s.8 B‐9000 Gent Belgium;</p> <p>Department of GeologyUniversity of LiegeQuartier Agora Batiment B18. Allée du six ao?t 14 4000 Liège Belgium;</p> <p>GIGA‐Cyclotron Research centreInstitut de Physique B5a Quartier AgoraAllée du six AoutLiège 194000 Belgium;</p> <p>GIGA‐Cyclotron Research centreInstitut de Physique B5a Quartier AgoraAllée du six AoutLiège 194000 Belgium;</p> <p>GIGA‐Cyclotron Research centreInstitut de Physique B5a Quartier AgoraAllée du six AoutLiège 194000 Belgium;</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=Clayey sand turbidites&option=203" rel="nofollow">Clayey sand turbidites;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=cohesion&option=203" rel="nofollow">cohesion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=shallow slope failure&option=203" rel="nofollow">shallow slope failure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subaqueous sediment density flows&option=203" rel="nofollow">subaqueous sediment density flows;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=turbulence&option=203" rel="nofollow">turbulence;</a> </p> <div class="translation"> 机译：Clayey砂浊;凝聚力;浅边坡衰竭;亚水沉积物密度流动;湍流; 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