Geomorphic response to late Quaternary tectonics in the axial portion of the Southern Apennines (Italy): A case study from the Calore River valley

Amato V.; Aucelli P.P.C.; Cesarano M.; Filocamo F.; Leone N.; Petrosino P.; Rosskopf C.M.; Valente E.; Casciello E.; Giralt S.; Jicha B.R.

摘要

Abstract > The present study focuses on the morphotectonic evolution of the axial portion of the Southern Apennine chain between the lower Calore River valley and the northern Camposauro mountain front (Campania Region). A multidisciplinary approach was used, including geomorphological, field‐geology, stratigraphical, morphotectonic, structural, 40 Ar/ 39 Ar and tephrostratigraphical data. Results indicate that, from the Lower Pleistocene onwards, this sector of the chain was affected by extensional tectonics responsible for the onset of the sedimentation of Quaternary fluvial, alluvial fan and slope deposits. Fault systems are mainly composed of NW‐SE, NE–SW and W‐E trending strike‐slip and normal faults, associated to NW‐SE and NE–SW oriented extensions. Fault scarps, stratigraphical and structural data and morphotectonic indicators suggest that these faults affected the wide piedmont area of the northern Camposauro mountain front in the Lower Pleistocene–Upper Pleistocene time span. Faults affected both the oldest Quaternary slope deposits (Laiano Synthem, Lower Pleistocene) and the overlying alluvial fan system deposits constrained between the late Middle Pleistocene and the Holocene. The latter are geomorphologically and chrono‐stratigraphically grouped into four generations, I generation: late Middle Pleistocene–early Upper Pleistocene, with tephra layers 40 Ar/ 39 Ar dated to 158±6 and 113±7 ka; II generation: Upper Pleistocene, with tephra layers correlated with the Campanian Ignimbrite (39?ka) and with the slightly older Campi Flegrei activity ( 40 Ar/ 39 Ar age 48±7 ka); III generation: late Upper Pleistocene–Lower Holocene, with tephra la </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：lang =“en”> <title type =“main”>抽象</ title> >当前研究重点研究了下葫芦河谷和北坎普拉山前沿（坎帕尼亚地区）南部赤峰链条轴向部分的连续性演变。使用多学科方法，包括地貌，现场地质，地层，图解性，结构，结构， 40 </ sup> Ar / 39 </ sup> Ar和tephroStrataphical数据。结果表明，从较低的更优先岛开始，该链条的该部门受到季术河流，冲积扇和坡沉积物沉降的扩展构造的影响。故障系统主要由NW-SE，NE-SW和W-E趋势触摸滑动和正常故障组成，与NW-SE和NE-SW定向延伸有关。故障稀稀硅，地质和结构数据和Morphoteccection指标表明，这些断层影响了北方坎普罗山前面的宽山麓地区，在较低的中新生上升山脉时间跨度。缺陷影响最古老的四元坡沉积物（Laiano Synthem，较低），覆盖的冲积风扇系统沉积物受到后期中间人烯和全新世之间的约束。后者在整岩上和计时分层分为四代，我生成：晚期渗透介质 - 早期上层烯丙烯，用Tephra层 40 </ sup> Ar / 39 </ sup> Ar日期为158± 6和113±7 ka; II代：上部更新世，Tephra层与Campanian Ignimbrite（39 ka）相关，并且略大较旧的坎皮羊毛活动（ 40 </ sup> Ar / 39 </ sup> AR Age 48± 7 ka）; iii生成：晚熟较低的全新世，用Tephra La </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>2018年第11期</span><b style="margin: 0 2px;">|</b><span>共18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=Amato V.&option=202" target="_blank" rel="nofollow">Amato V.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Aucelli P.P.C.&option=202" target="_blank" rel="nofollow">Aucelli P.P.C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cesarano M.&option=202" target="_blank" rel="nofollow">Cesarano M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Filocamo F.&option=202" target="_blank" rel="nofollow">Filocamo F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leone N.&option=202" target="_blank" rel="nofollow">Leone N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Petrosino P.&option=202" target="_blank" rel="nofollow">Petrosino P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rosskopf C.M.&option=202" target="_blank" rel="nofollow">Rosskopf C.M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Valente E.&option=202" target="_blank" rel="nofollow">Valente E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Casciello E.&option=202" target="_blank" rel="nofollow">Casciello E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Giralt S.&option=202" target="_blank" rel="nofollow">Giralt S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jicha B.R.&option=202" target="_blank" rel="nofollow">Jicha B.R.;</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 Biosciences and TerritoryUniversity of MolisePesche (IS) Italy;</p> <p>Department of Science and TechonologyParthenope UniversityNaples Italy;</p> <p>Institute of Environmental Geology and Geoengineering IGAG‐CNRRome Italy;</p> <p>Department of Biosciences and TerritoryUniversity of MolisePesche (IS) Italy;</p> <p>Department of Biosciences and TerritoryUniversity of MolisePesche (IS) Italy;</p> <p>Department of Earth Environment and Resources SciencesUniversity of Naples Federico IINaples Italy;</p> <p>Department of Biosciences and TerritoryUniversity of MolisePesche (IS) Italy;</p> <p>Department of Earth Environment and Resources SciencesUniversity of Naples Federico IINaples Italy;</p> <p>Institute of Earth Sciences Jaume Almera ICTJA‐CISCBarcelona Spain;</p> <p>Institute of Earth Sciences Jaume Almera ICTJA‐CISCBarcelona Spain;</p> <p>University of Wisconsin‐MadisonMadison Wisconsin;</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=geomorphology&option=203" rel="nofollow">geomorphology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=extensional tectonics&option=203" rel="nofollow">extensional tectonics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=alluvial fans&option=203" rel="nofollow">alluvial fans;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tephrostratigraphy&option=203" rel="nofollow">tephrostratigraphy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=southern Italy&option=203" rel="nofollow">southern Italy;</a> </p> <div class="translation"> 机译：地貌;扩展构造;冲积球迷;tephroStratigraphy;意大利南部; </div> </li> </ul> </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023138985.html">Geomorphic response to late Quaternary tectonics in the axial portion of the Southern Apennines (Italy): A case study from the Calore River valley</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Amato V.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Amato V.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Aucelli P.P.C.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Aucelli P.P.C.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cesarano M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Cesarano M.,</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>2018</span><span>,第11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：南部亚平宁南部轴向部分（意大利）的后季度构造的地貌响应：Calore River Valley的案例研究</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_geomorphology_thesis/0204112224837.html">Geomorphic evidence of Quaternary tectonics within an underlap fault zone of southern Apennines, Italy</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Giano Salvatore Ivo&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Giano Salvatore Ivo,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pescatore Eva&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Pescatore Eva,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Agosta Fabrizio&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Agosta Fabrizio,</a> <a href="/journal-foreign-841/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geomorphology .</a> <span>2018</span><span>,第FEBa15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：意大利亚平宁山脉下缘断层带内第四纪构造的地貌证据</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_journal-geodynamics_thesis/0204112260071.html">Late Quaternary tectonics in the inner Northern Apennines (Siena Basin, southern Tuscany, Italy) and their seismotectonic implication</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Andrea Brogi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Andrea Brogi,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Enrico Capezzuoli&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Enrico Capezzuoli,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ivan Martini&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ivan Martini,</a> <a href="/journal-foreign-852/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geodynamics .</a> <span>2014</span><span>,第may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：北部亚平宁山脉（锡耶纳盆地，意大利托斯卡纳南部）的晚第四纪构造及其地震构造意义</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_meeting-255497_thesis/0705010377609.html">Structural, Morphotectonic and Thermo- chronological Constraints to the Late Miocene- quaternary Tectonic Evolution and Exhumation in the Southern Apennines, Italy</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=S. 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