海底块状硫化物矿床的电、电磁勘探方法

R. Safipour, A. Swidinsky, S. Hölz, M. Jegen
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引用次数: 0

摘要

在第勒尼安海Palinuro海山的一个浅埋且热液不活跃的大型硫化物矿床上测试了两种海洋地球物理方法。在海底山上部署了一种新型电磁结构,该结构由船拖环发射机和远程偶极子接收器组成,远程接收器成功记录了瞬变电场。此外,还部署了一个SP系统,该系统由两对垂直的电极组成,并被拖曳到靠近海底的位置。在已知的块状硫化物矿化带上记录到异常高的电场强度,表明SP方法在探测不活跃的、埋藏的块状硫化物位点方面是有效的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Electrical and electromagnetic methods in exploring for seafloor massive sulfide deposits
Two marine geophysical methods are tested over a shallowly buried and hydrothermally inactive massive sulfide occurrence at the Palinuro Seamount in the Tyrrhenian Sea. A novel EM configuration consisting of a ship-towed loop transmitter and remote dipole receivers was deployed over the seamount, and electric field transients were successfully recorded by the remote receivers. An SP system consisting of two perpendicular pairs of electrodes towed close to the seafloor was also deployed. Anomalously high electric field strengths were recorded over the zone of known massive sulfide mineralization, demonstrating that the SP method is effective at detecting inactive, buried massive sulfide sites.
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