权益分类	功能权益	普通用户	{{item.name}}会员
{{category.name}}	{{benefitItem.name}}

Rock magnetic properties and their anisotropy from the Outokumpu assemblage in the Outokumpu deep drilling, Finland

芬兰奥托昆普深钻奥托昆普组合的岩石磁特性及其各向异性

基本信息

批准号：
65103356
负责人：
Privatdozentin Dr. Agnes Kontny
金额：
--
依托单位：
Abteilung Strukturgeologie und Tektonophysik
依托单位国家：
德国
项目类别：
Infrastructure Priority Programmes
财政年份：
2008
资助国家：
德国
起止时间：
2007-12-31 至 2012-12-31
项目状态：
已结题

来源：
https://gepris.dfg.de/gepris/projekt/65103356?language=en
关键词：
Rock magnetic properties their anisotropy

项目摘要

The aim of this project is to provide rock and paleomagnetic data under consideration of paleomagnetic field vectors (inclination) and of the directional dependence of magnetic susceptibility and magnetic remanence for the interpretation of the magnetic logging data (see proposal by Hördt and Leuven). We focus in our study on the Outokumpu assemblage between 1314 and 1515 m of the Outokumpu deep drilling. This assemblage is characterized by several geophysical anomalies including both very high magnetic susceptibilities and remanent magnetizations and is the host rock of the Outokumpu-type Cu-Co-Zn-Ni(-Ag-Au) deposits. The remanent magnetization in the serpentinites is carried by magnetite and pyrrhotite. Different degrees of silica-carbonate alteration of serpentinite caused a decomposition of magnetite and a transformation of ferrimagnetic into antiferromagnetic pyrrhotite along with Ni-sulfide formation, which is seen in strong susceptibility variation in the serpentinite unit. Although we found no correlation between rock magnetic properties and chemical composition, we observed a clear relationship between mineralogy and magnetic properties in relation to the silica-carbonate alteration. This finding also explains the strong magnetic field variation within the investigated Outokumpu assemblage measured by Hördt and co-workers.

该项目的目的是提供考虑到古磁场矢量（倾角）以及磁化率和剩磁的方向依赖性的岩石和古地磁数据，以便解释磁测井数据（见Hördt和Leuven提出的建议）。我们重点研究了Outokumpu深钻1314 ~ 1515 m之间的Outokumpu组合。该组合具有高磁化率和剩余磁化率等地球物理异常特征，是乌托昆普型Cu-Co-Zn-Ni（-Ag-Au）矿床的寄主岩。蛇纹岩中的残余磁化由磁铁矿和磁黄铁矿携带。蛇纹岩不同程度的硅碳酸盐蚀变导致磁铁矿分解，铁磁性磁黄铁矿转变为反铁磁性磁黄铁矿，并形成镍硫化物，在蛇纹岩单元中表现出强烈的磁化率变化。虽然我们没有发现岩石磁性与化学成分之间的相关性，但我们观察到与硅碳酸盐蚀变有关的矿物学和磁性之间存在明确的关系。这一发现也解释了Hördt及其同事测量的Outokumpu组合中强磁场的变化。