The Alpine Fault Hangingwall Viewed From Within: Structural Analysis of Ultrasonic Image Logs in the DFDP‐2B Borehole, New Zealand

Massiot Cécile; Célérier Bernard; Doan Mai‐Linh; Little Tim A.; Townend John; McNamara David D.; Williams Jack; Schmitt Douglas R.; Toy Virginia G.; Sutherland Rupert; Janku‐Capova Lucie; Upton Phaedra; Pezard Philippe A.

摘要

Abstract >Ultrasonic image logs acquired in the DFDP‐2B borehole yield the first continuous, subsurface description of the transition from schist to mylonite in the hangingwall of the Alpine Fault, New Zealand, to a depth of 818 m below surface. Three feature sets are delineated. One set, comprising foliation and foliation‐parallel veins and fractures, has a constant orientation. The average dip direction of 145° is subparallel to the dip direction of the Alpine Fault, and the average dip magnitude of 60° is similar to nearby outcrop observations of foliation in the Alpine mylonites that occur immediately above the Alpine Fault. We suggest that this foliation orientation is similar to the Alpine Fault plane at ～1 km depth in the Whataroa valley. The other two auxiliary feature sets are interpreted as joints based on their morphology and orientation. Subvertical joints with NW‐SE (137°) strike occurring dominantly above ～500 m are interpreted as being formed during the exhumation and unloading of the Alpine Fault's hangingwall. Gently dipping joints, predominantly observed below ～500 m, are interpreted as inherited hydrofractures exhumed from their depth of formation. These three fracture sets, combined with subsidiary brecciated fault zones, define the fluid pathways and anisotropic permeability directions. In addition, high topographic relief, which perturbs the stress tensor, likely enhances the slip potential and thus permeability of subvertical fractures below the ridges, and of gently dipping fractures below the valleys. Thus, DFDP‐2B borehole observations support the inference of a large zone of enhanced permeability in the hangingwall of the Alpine Fault. </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 Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >在DFDP-2B钻孔中获取的超声图像日志产生的第一个连续，地下表面的过渡到高山故障，新西兰的悬挂空间，深度为818米。三个特征集被删除。包含叶片和叶状平行静脉和骨折的一组具有恒定的取向。 145°的平均倾向方向与高山故障的倾角相同，平均倾角为60°类似于附近的卵巢囊肿中叶片的脱裂观察，其在高山断层上方立即发生。我们认为这种叶面取向类似于在Whatearoa谷的〜1公里深处的高山断层平面。另外两个辅助特征集根据其形态和方向被解释为关节。具有高于〜500μm的NW-SE（137°）击球的剧本关节被解释为在高山故障悬挂壁的挖掘和卸载过程中形成。轻轻地浸入关节，主要观察到〜500米以下，被解释为从其形成深度挖掘的遗传水下裂缝。这三种骨折组合与辅助封闭断层区结合，定义了流体途径和各向异性渗透方向。此外，扰动应力张量的高地形浮雕，可能提高了脊下方的逆变骨折，并且在谷底下轻轻浸渍骨折的渗透性。因此，DFDP-2B钻孔观察支持在高山故障的悬挂壁中的大区域增强渗透性的推断。</ 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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2018年第8期</span><b style="margin: 0 2px;">|</b><span>共24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=Massiot Cécile&option=202" target="_blank" rel="nofollow">Massiot Cécile;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Célérier Bernard&option=202" target="_blank" rel="nofollow">Célérier Bernard;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Doan Mai‐Linh&option=202" target="_blank" rel="nofollow">Doan Mai‐Linh;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Little Tim A.&option=202" target="_blank" rel="nofollow">Little Tim A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Townend John&option=202" target="_blank" rel="nofollow">Townend John;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McNamara David D.&option=202" target="_blank" rel="nofollow">McNamara David D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Williams Jack&option=202" target="_blank" rel="nofollow">Williams Jack;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schmitt Douglas R.&option=202" target="_blank" rel="nofollow">Schmitt Douglas R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Toy Virginia G.&option=202" target="_blank" rel="nofollow">Toy Virginia G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sutherland Rupert&option=202" target="_blank" rel="nofollow">Sutherland Rupert;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Janku‐Capova Lucie&option=202" target="_blank" rel="nofollow">Janku‐Capova Lucie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Upton Phaedra&option=202" target="_blank" rel="nofollow">Upton Phaedra;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pezard Philippe A.&option=202" target="_blank" rel="nofollow">Pezard Philippe A.;</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>GNS Science AvalonLower Hutt New Zealand;</p> <p>Géosciences MontpellierUniversité de Montpellier CNRSMontpellier France;</p> <p>Univ. Grenoble Alpes Univ. Savoie Mont Blanc CNRS IRD IFSTTARISTerre Grenoble France;</p> <p>SGEES Victoria University of WellingtonWellington New Zealand;</p> <p>SGEES Victoria University of WellingtonWellington New Zealand;</p> <p>School of Natural Sciences University of IrelandGalway Ireland;</p> <p>Department of Geology University of OtagoDunedin New Zealand;</p> <p>Department of PhysicsUniversity of AlbertaEdmonton AB Canada;</p> <p>Department of Geology University of OtagoDunedin New Zealand;</p> <p>SGEES Victoria University of WellingtonWellington New Zealand;</p> <p>SGEES Victoria University of WellingtonWellington New Zealand;</p> <p>GNS Science AvalonLower Hutt New Zealand;</p> <p>Géosciences MontpellierUniversité de Montpellier CNRSMontpellier France;</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=Alpine Fault&option=203" rel="nofollow">Alpine Fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ultrasonic image log&option=203" rel="nofollow">ultrasonic image log;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=foliation&option=203" rel="nofollow">foliation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fractures&option=203" rel="nofollow">fractures;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=anisotropy&option=203" rel="nofollow">anisotropy;</a> </p> <div class="translation"> 机译：高山故障;超声图像原;叶子;骨折;各向异性; </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> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360847.html">The Alpine Fault Hangingwall Viewed From Within: Structural Analysis of Ultrasonic Image Logs in the DFDP‐2B Borehole, New Zealand</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Massiot Cécile&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Massiot Cécile,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Célérier Bernard&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Célérier Bernard,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Doan Mai‐Linh&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Doan Mai‐Linh,</a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2018</span><span>,第8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：从内部观察的高山故障悬挂壁：在DFDP-2B钻孔，新西兰的超声图像日志的结构分析</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025591663.html">Seismic P Wave Velocity Model From 3-D Surface and Borehole Seismic Data at the Alpine Fault DFDP-2 Drill Site (Whataroa, New Zealand)</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lay V&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lay V,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Buske S.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Buske S.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bodenburg S. 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href="/patent-detail/06120204717851.html">变压器内部固体绝缘故障超声波探测装置</a> <b>[P]</b> . <span> 中国专利： CN204719182U </span> <span> . 2015.10.21</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130463108867.html">Borehole logging methods for detection and imaging of formation structural features</a> <b>[P]</b> . <span> 外国专利：  EP0296987B1 </span> <span> . 1992-07-22</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：地层结构特征检测和成像的井眼测井方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130465947833.html">Borehole logging methods for detection and imaging of formation structural features</a> <b>[P]</b> . <span> 外国专利：  EP0296987A3 </span> <span> . 1990-05-16</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：地层结构特征检测和成像的井眼测井方法 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130466930064.html">Borehole logging methods for detection and imaging of formation structural features</a> <b>[P]</b> . <span> 外国专利：  US4817059A </span> <span> . 1989-03-28</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：地层结构特征检测和成像的井眼测井方法 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" 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