Proterozoic tectonothermal processes imaged with magnetotellurics and seismic reflection in southern Australia
Proterozoic tectonothermal processes imaged with magnetotellurics and seismic reflection in southern Australia作者机构:Geological Survey of South AustraliaDepartment for Energy and MiningAdelaideSA5005Australia School of Earth and Environmental SciencesUniversity of AdelaideAdelaideSA5005Australia
出 版 物:《Geoscience Frontiers》 (地学前缘(英文版))
年 卷 期:2020年第11卷第3期
页 面:885-893页
核心收录:
学科分类:070904[理学-构造地质学] 081801[工学-矿产普查与勘探] 081802[工学-地球探测与信息技术] 070903[理学-古生物学与地层学(含:古人类学)] 0709[理学-地质学] 07[理学] 08[工学] 0708[理学-地球物理学] 0818[工学-地质资源与地质工程] 0704[理学-天文学]
基 金:Eucla Gawler MT data Geological Survey of South Australia
主 题:Magnetotellurics Seismic reflection Resistivity
摘 要:Over the last two decades,co-located seismic and magnetotelluric(MT) profiles provided fundamental geophysical data sets to image the Australian *** their complimentary nature,the data are processed and often interpreted separately without common processes in *** here qualitatively compare 2 D resistivity inversion models derived from MT and seismic reflection profiles across a region of Archean-Proterozoic Australia to address the causes of variations in seismic response and anomalous conductivity in the *** find that there exists a spatial association between regions of low reflectivity in seismic sections and low resistivity in co-located2 D MT modelled *** relationships elucidate possible signatures of past magmatic and fluid-related *** on their diffuse or discrete character,we hypothesize these signatures signify fossil melting of the crust due to mafic underplating,magma movement or hydrothermal fluid flow through the *** approach discussed herein is a process-oriented approach to interpretation of geophysical images and a significant extension to traditional geophysical methods which are primarily sensitive to a singular bulk rock property or state.