Geophysical correlation: global versus local perspectives

Kvamme Kenneth L.

摘要

Abstract > Robust anomalies that point to the same buried features frequently occur in diverse data sets from multi‐method surveys [e.g. ground penetrating radar (GPR), magnetic gradiometry, electrical resistivity]. Relationships between such corresponding anomalies traditionally have been noted subjectively, through visual comparisons of mappings or overlays of geophysical results. These circumstances create a paradox because theory and correlational studies generally suggest largely independent dimensions, while mappings of geophysical results often illustrate parallel anomalies which suggest that robust correlations should exist. Through application of <fi>local</fi> Pearson's <fi>r</fi> in small neighbourhoods, with radii ranging from 0.71 to 1.6?m, a means is offered, and demonstrated, to quantify and map local correlations between two geophysical data sets. A case study examines relationships between apparent electrical resistivity, a GPR depth‐slice, and magnetic susceptibility data acquired at Army City, a Great War troop support town in Kansas, now obliterated except for subsurface remains. Intricate spatial patterns of positive and negative correlations between these modalities are illustrated that vary in complexity with neighbourhood size. Neighbourhoods of moderate size seem preferable because the spatial patterning of correlations is enhanced locally and region‐wide. With focus given to positive correlations that point to parallel anomalies, overlays of high correlation frequently correspond with robust anomalies observed in each data set and offer objective criteria for assessments of correlation. However, it is also demonstrated that mutually robust anomalies do not necessarily exhibit high correlation and that high correlations frequently exist in regions devoid of apparent anomalies. The issue of assessing jointly parallel correlations between three or more geophysical data sets is also confronted using a form of local principal components analysis. It is shown that high eigenvalues associated with first principal components that exhibit loadings in the same direction point to zones of mutually high parallel correlation. </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：lang =“en”> <标题类型=“main”>抽象</ title> > 指向相同埋地特征的强大异常经常发生在多种方法调查中的不同数据集中[例如地面穿透雷达（GPR），磁谱仪，电阻率]。传统上已经通过地球物理结果的映射或覆盖的视觉比较来主观地注意到这种相应的异常之间的关系。这些情况创造了一个悖论，因为理论和相关研究通常表明了很大程度上的尺寸，而地球物理结果的映射通常是说明平行异常，这表明应该存在强大的相关性。通过应用 <fi>本地</ fi> Pearson的 <fi> r </ fi> 在小区中，RADII范围为0.71至1.6？m，提供了一种手段，并演示，以量化和映射两个地球物理数据集之间的局部相关性。案例研究检查了在堪萨斯州克拉斯的伟大战争部队支援镇在军队城市中获得的表观电阻率，GPR深度切片和磁性敏感性数据之间的关系。示出了这些方式之间的正面和负相关性的复杂空间模式，其复杂性与邻域大小不同。中等大小的邻居似乎是优选的，因为相关性的空间图案化在本地和区域宽地增强。对于指向平行异常的阳性相关的焦点，高相关覆盖通常对应于每个数据集中观察到的鲁棒异常，并提供有关相关性评估的客观标准。然而，还证明了相互稳健的异常不一定表现出高相关性，并且在没有表观异常的区域中经常存在高的相关性。评估三个或更多个地球物理数据集之间的共同并行相关性的问题也使用一种局部主成分分析来面对。结果表明，与第一主成分相关的高特征值，其在与相互高平行相关区的相同方向上的加载中表现出负载。 </ 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-19488/'>《Archaeological prospection》</a> <b style="margin: 0 2px;">|</b><span>2018年第2期</span><b style="margin: 0 2px;">|</b><span>共10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=Kvamme Kenneth L.&option=202" target="_blank" rel="nofollow">Kvamme Kenneth L.;</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 Anthropology &</p> <p>Archeo‐Imaging LabUniversity of ArkansasFayetteville AR USA;</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/140.html" title="文物考古">文物考古;</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=data integration&option=203" rel="nofollow">data integration;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geophysical correlation&option=203" rel="nofollow">geophysical correlation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Great War&option=203" rel="nofollow">Great War;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=local correlation&option=203" rel="nofollow">local correlation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=local PCA&option=203" rel="nofollow">local PCA;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=multi‐method surveys&option=203" rel="nofollow">multi‐method surveys;</a> </p> <div class="translation"> 机译：数据集成;地球物理相关;伟大的战争;局部相关;本地PCA;多方法调查; 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