Three‐Dimensional Seismic Imaging of Ancient Submarine Lava Flows: An Example From the Southern Australian Margin

Reynolds P.; Holford S.; Schofield N.; Ross A.

摘要

Abstract >Submarine lava flows are the most common surficial igneous rock on the Earth. However, they are inherently more difficult to study than their subaerial counterparts due to their inaccessibility. In this study, we use newly acquired 3‐D (three‐dimensional) seismic reflection data to document the distribution and morphology of 26 ancient, buried lava flows within the middle Eocene‐aged Bight Basin Igneous Complex, offshore southern Australia. Many of these lava flows are associated with volcanoes that vary from 60 to 625 m in height and 0.3 to 10 km in diameter. Well data and seismic‐stratigraphic relationships suggest that the lava flows and volcanoes were emplaced offshore in water depths of 300 m. The lava flows range from 0.5 to 34 km in length and 1 to 15 km in width and are typified by tabular and dendritic forms. This morphological variation may result from differing lava effusion rates and/or the volumes of lava erupted. We demonstrate that: (1) the dendritic flows contain complex lava distribution systems and kipukas, features never‐before observed from seismic data; and (2) the distribution and morphology of the lava flows was strongly controlled by the emplacement of magmatic intrusion‐induced forced folds. This suggests that magmatic intrusions may play an important role in controlling the distribution of lava flows elsewhere. Our study highlights the usefulness of seismic data in studying the manifestation of submarine volcanism, and provides quantitative data on the extent and distribution of an ancient submarine volcanic province along the southern Australian margin. </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”> <标题类型=“main”>抽象</ title> 潜艇熔岩流是地球上最常见的曲线岩石。然而，由于其无法访问，它们本质上更难以研究比其子宫人对应物。在这项研究中，我们使用新收购的3-D（三维）地震反射数据来记录26岁的古代埋藏盆地中的26个古代埋藏的熔岩流动，澳大利亚海上南部南部南部南部。这些熔岩流中的许多流量与火山有关，火山高于60至625米，直径0.3至10千米。井数据和地震 - 地层关系表明，熔岩流量和火山在水深的海上被置于300米。熔岩流量范围为0.5至34千米，宽度为1至15千米，用表格和树突形式典型。这种形态变异可能是不同于不同的熔岩积液率和/或熔岩体积爆发的熔岩。我们证明：（1）树突流量含有复杂的熔岩分布系统和KIPUKAS，从地震数据观察到之前从未出发; （2）熔岩流的分布和形态受到岩浆入侵诱导的强制折叠的施加强烈控制。这表明岩浆侵入可能在控制其他地方的熔岩分布方面发挥重要作用。我们的研究突出了地震数据在研究潜艇火山主义的表现方面的有用性，并提供了关于澳大利亚南部南部南部潜艇火山省的定量数据。</ 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>2017年第11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=Reynolds P.&option=202" target="_blank" rel="nofollow">Reynolds P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Holford S.&option=202" target="_blank" rel="nofollow">Holford S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schofield N.&option=202" target="_blank" rel="nofollow">Schofield N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ross A.&option=202" target="_blank" rel="nofollow">Ross 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>Centre for Tectonics Resources and Exploration Australian School of PetroleumUniversity of AdelaideAdelaide SA Australia;</p> <p>Centre for Tectonics Resources and Exploration Australian School of PetroleumUniversity of AdelaideAdelaide SA Australia;</p> <p>Department of Geology &</p> <p>Petroleum GeologyUniversity of AberdeenAberdeen UK;</p> <p>CSIRO Energy Australian Resources Research CentreKensington WA Australia;</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=submarine lava flow&option=203" rel="nofollow">submarine lava flow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismic attributes&option=203" rel="nofollow">seismic attributes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=forced folds&option=203" rel="nofollow">forced folds;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lava distribution system&option=203" rel="nofollow">lava distribution system;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=intraplate volcanism&option=203" rel="nofollow">intraplate volcanism;</a> </p> <div class="translation"> 机译：潜艇熔岩流;地震属性;强制褶皱;熔岩分配系统;血液膜火山; 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Douglas</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=R.A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,R.A.</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fraser1&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Fraser1</a> <span> <a href="/journal-cn-39438/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋地质 </a> </span> <span> . 2016</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_foreign-geology-beijing_thesis/0201262950822.html">晚太古代会聚边缘构造运动和金的矿作用：对西澳大利亚...</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barl.ME&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . Barl.ME</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵建&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,赵建</a> <span> <a href="/journal-cn-42495/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 国外地质（北京） </a> </span> <span> . 1991</span><span>,第004期</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120103876691.html">生成一个或多个亮度边缘以形成物体的三维模型</a> <b>[P]</b> . <span> 中国专利： CN111164375A </span> <span> . 2020-05-15</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130411974046.html">ancient carvings on metals, stones and other mineralioggi incomprehensible being bulinate art such as cryptograms where entering flows of light will effect a reflection outside which oloprogramme provides a three-dimensional image is well defined and understood as the same predetermined engraver</a> <b>[P]</b> . <span> 外国专利：  ITCT20150008U1 </span> <span> . 2016-09-02</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：金属，石头和其他矿物ioogigi上的古代雕刻是难以理解的艺术，例如密码术，其中进入的光流将产生反射，在其中，oloprogramme提供了三维图像，并被很好地定义并理解为相同的预定雕刻师 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130402603761.html">SEISMIC THREE-DIMENSIONAL MEASUREMENT METHOD FOR SMALL OBJECTS, SUBMARINE CABLES AND THE LIKE IN THE SEA BED, SEA SWELL INDEPENDENT TOWED BODY FOR THE ULTRA-HIGH RESOLUTION 3D MEASUREMENT OF SMALL STRUCTURES IN THE SEA BED AND MODULAR DEVICE CARRIER FOR THE THREE-DIMENSIONAL MEASUREMENT OF SMALL OBJECTS IN THE SEA BED</a> <b>[P]</b> . <span> 外国专利：  EP3717940A1 </span> <span> . 2020-10-07</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：地震床中的小物体，海底电缆和类似物的地震三维测量方法，海底独立形状的拖曳体对于海底床和模块式载体中的小结构的超高分辨率3D测量海床上的小物体 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130403482531.html">SEISMIC THREE-DIMENSIONAL MEASUREMENT METHOD FOR SMALL OBJECTS, SUBMARINE CABLES AND THE LIKE IN THE SEA BED, SEA SWELL INDEPENDENT TOWED BODY FOR THE ULTRA-HIGH RESOLUTION 3D MEASUREMENT OF SMALL STRUCTURES IN THE SEA BED AND MODULAR DEVICE CARRIER FOR THE THREE-DIMENSIONAL MEASUREMENT OF SMALL OBJECTS IN THE SEA BED</a> <b>[P]</b> . <span> 外国专利：  WO2019105510A1 </span> <span> . 2019-06-06</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：地震床中的小物体，海底电缆和类似物的地震三维测量方法，海底独立形状的拖曳体对于海底床和模块式载体中的小结构的超高分辨率3D测量海床上的小物体 </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 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