The fractal properties of topography as controlled by the interactions of tectonic, lithological, and geomorphological processes

机译：构造，岩性和地貌过程的相互作用控制的地形分形特征

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Abstract >Landscape topography widely exhibits fractal structure. Because of the complexity of relief geometry this structure is not homogeneous in space, and the study of its spatial characteristics represents a powerful method for investigating the interrelationships between landforms and underlying processes. We explore these interrelationships using the digital elevation model (DEM) of an area located in central Italy, where landscape topography is strongly linked to its geological evolution, being characterized by alternating intermountain basins and mountain ranges trending NW–SE. A modified version of the method based on the standard deviation of relief elevations is used to evaluate the fractal parameters of relief after tiling the DEM in spatial units characterized by homogeneous fractal geometry, and statistical methods in conjunction with spatial analysis techniques are applied to the resulting terrain datasets. Both the lowest and (to a lesser extent) the highest values of fractal dimension are found to follow the ridge‐and‐valley trend. Low fractal dimension is observed in the mountain ranges characterized by massive strata of limestone, and along the fault scarps defining the contact between the intermountain basins and the surrounding slopes, where sediment deposition prevails. High fractal dimension is observed in regions characterized by highly erodible terrigenous lithology, and in areas where tectonic activity favors erosional processes mainly by rivers. The analysis of the (fractal) power law parameters also suggests that each major lithological complex has its own characteristic fractal signature. These results provide new insights into the link between the fractal properties of topography and the tectonic, lithological, and geomorphological features of the area, and show that the analysis approach proposed is useful t </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> >横向形貌广泛表现出分形结构。由于浮雕几何形状的复杂性，这种结构在空间中不是均匀的，并且其空间特征的研究代表了调查地形和底层过程之间的相互关系的强大方法。我们探讨了使用位于意大利中部地区的地区的数字高度模型（DEM）的这些相互关系，其中景观地形与其地质演变有关，其特征在于交替的中间盆地和山脉趋势趋势NW-SE。基于浮雕凸起的标准偏差的方法的修改版本用于评估削减由均匀分形几何形状的空间单元中的DEM后的释放的分形参数，以及与空间分析技术结合的统计方法应用于所得的地形数据集。最低和（在较小程度上），发现分形维数的最高值遵循脊和谷趋势。在山脉中观察到低分形尺寸，其特征在于石灰石的大规模地层，沿着故障围巾，限定了层罩盆地和周围斜坡之间的接触，其中沉积物沉积普遍存在。在具有高度可易于侵蚀的人颅岩的区域中观察到高分形尺寸，以及在构造活动主要由河流的侵蚀过程的领域。（分形）电力法参数的分析还表明每个主要岩性复合物具有自己的特征分形签名。这些结果对地形分形性质与该地区的构造，岩性和地貌特征之间的联系提供了新的见解，并表明提出的分析方法是有用的 </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15期</span><b style="margin: 0 2px;">|</b><span>共14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=Liucci Luisa&option=202" target="_blank" rel="nofollow">Liucci Luisa;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Melelli Laura&option=202" target="_blank" rel="nofollow">Melelli Laura;</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 Physics and GeologyUniversity of Perugia06123 Perugia Italy;</p> <p>Department of Physics and GeologyUniversity of Perugia06123 Perugia 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/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=topography&option=203" rel="nofollow">topography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fractal&option=203" rel="nofollow">fractal;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=spatial analysis&option=203" rel="nofollow">spatial analysis;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geomorphological processes&option=203" rel="nofollow">geomorphological processes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=roughness&option=203" rel="nofollow">roughness;</a> </p> <div class="translation"> 机译：地形;分形;空间分析;地貌过程;粗糙度; 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