Inland notches: lithological characteristics and climatic implications of subaerial cavernous landforms in Israel

Shtober‐Zisu Nurit; Amasha Hani; Frumkin Amos

摘要

Abstract >Inland notches, are elongated concave‐shape indentations that develop on the carbonate rocky cliffs of mountainous zones, down to the desert fringe. These rock shelters form as a result of the interaction between specific petrologic characteristics and climatic controls, emphasizing the importance of environment upon rock decay. Inland notches are shaped due to slight differences (1–15%) in the porosity of the visor and cavity bed: the cavity bed is more porous, so more likely to erode by exfoliation and dissolution. Thus, the cavity bed retreats at a faster rate compared to the slower subaerial dissolution of the visor bed, until a critical point is reached where the visor collapses. In Israel, inland notches inhabit the same lithostratigraphic units as do large caves. The vast majority (71%) of inland notches are formed in hard, dense, and crystalline limestone deposited throughout the Turonian age. Another 27% are cut into the dolomitic sequence of the upper Albian and lower Cenomanian. The rest (2%) are dispersed in the various formations of the Cenomanian and Eocene eras. Notches are most common in semi‐arid and in Mediterranean climates but mainly in areas with annual rainfall of between 400?mm and 850?mm. In more humid areas ( 900?mm/yr) notches are negligible or completely absent, due to the rapid rate of chemical dissolution of carbonate rocks. In the desert fringe (200–300?mm/yr), mechanical decay is accelerated and notches exhibit disintegration processes, visor collapse, and rock falls. In the desert area ( 200?mm/yr), salt decay replaces the chemical decay characteristic of inland notches, encouraging tafoni formation. In addition, notches form through fluvial activity or on account of greater petrophysical differences between consecutive beds; i.e. elongated cavities may form in soft rocks, shaded by harder visors or crusts. Copyright ? 2017 John Wiley & Sons, Ltd. </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”> <title type =“main”>抽象</ title> >内陆凹口，是细长的凹形缩进在山区岩石岩石悬崖上发展，向下到沙漠边缘。这些岩石避难所形成，由于特定探测性特征与气候控制之间的相互作用，强调环境对岩石衰变的重要性。由于遮阳板和腔床的孔隙率略微差异（1-15％），内陆凹口是由于孔隙率的轻微差异（1-15％）：腔床更加多孔，因此更有可能通过剥离和溶解而侵蚀。因此，与遮阳床的较慢的基底溶解相比，腔床以更快的速率退缩，直到达到遮阳板塌陷的临界点。在以色列，内陆陷入困境与大洞穴相同的岩石车身单位。绝大多数（71％）内陆凹口形成沉重，致密，晶体石灰岩中的沉重，沉积在整个接际年龄。另外27％被切成上尔米亚人和下尖曼诺曼的白云岩序列。其余的（2％）分散在临曼诺曼和何时代的各种地层中。凹口在半干旱和地中海气候中最常见，但主要在每年降雨量为400？mm和850？mm的区域。由于碳酸盐岩石的化学溶解速率的快速速率，在更潮湿的地区（＆ 900？mm / yr）凹口可忽略不计或完全不存在。在沙漠边缘（200-300？mm / yr）中，加速机械衰变，缺口展示崩解过程，遮阳板塌陷和岩石落下。在沙漠区域（＆ 200？mm / yr）中，盐腐烂取代内陆凹口的化学衰减特征，鼓励Tafoni形成。此外，通过氟血管活动或未考虑到连续床之间的更高的岩石物理差异的缺口;即，细长的空腔可以在软岩中形成，由更硬的遮阳板或外壳阴影。版权？ 2017年John Wiley＆amp; SONS，LTD。</ p> </ abstract> </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-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2017年第12期</span><b style="margin: 0 2px;">|</b><span>共13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=Shtober‐Zisu Nurit&option=202" target="_blank" rel="nofollow">Shtober‐Zisu Nurit;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Amasha Hani&option=202" target="_blank" rel="nofollow">Amasha Hani;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Frumkin Amos&option=202" target="_blank" rel="nofollow">Frumkin Amos;</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>University of Haifa Israel StudiesHaifa Israel;</p> <p>University of Haifa Israel StudiesHaifa Israel;</p> <p>Geography Institute of Earth ScienceHebrew University of JerusalemJerusalem Israel;</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=inland notch&option=203" rel="nofollow">inland notch;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rock shelter&option=203" rel="nofollow">rock shelter;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=exfoliation&option=203" rel="nofollow">exfoliation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rock decay&option=203" rel="nofollow">rock decay;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tafoni&option=203" rel="nofollow">tafoni;</a> </p> <div class="translation"> 机译：内陆槽口;岩雨层;去角质;岩石腐烂;Tafoni; </div> </li> </ul> </div> </div> <div class="literature cardcommon" id="literaturereference" style="display:none"> <div class="similarity "> <h3 class="all_title" id="enpatent111">引文网络</h3> <div class="referencetab clearfix"> <ul id="referencedaohang"> <li dataid="referenceul">参考文献</li> <li dataid="citationul">引证文献</li> <li dataid="commonreferenceul">共引文献</li> <li dataid="commoncitationul">同被引文献</li> <li dataid="tworeferenceul">二级参考文献</li> <li dataid="twocitationul">二级引证文献</li> </ul> </div> <div class="reference_details" id="referenceList"> <ul id="referenceul"></ul> <ul id="citationul"></ul> <ul id="commonreferenceul"></ul> <ul id="commoncitationul"></ul> <ul id="tworeferenceul"></ul> <ul id="twocitationul"></ul> </div> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023139072.html">Inland notches: lithological characteristics and climatic implications of subaerial cavernous landforms in Israel</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shtober‐Zisu Nurit&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Shtober‐Zisu Nurit,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Amasha Hani&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Amasha Hani,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Frumkin Amos&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Frumkin Amos </a> <a href="/journal-foreign-22319/" target="_blank" rel="nofollow" class="tuijian_authcolor">Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group .</a> <span>2017</span><span>,第12期</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：内陆缺口：以色列岩体海绵状地貌的岩性特征和气候影响</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_geomorphology_thesis/0204119703632.html">Slope retreat rates estimated from chronology of tufa deposits sheltered by inland notches on Mt. 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