ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
假玄武玻璃的岩石磁学研究进展
  
关键词:pseudotachylyte  rock magnetism  magnetic fabric  seismic faulting
基金项目:由国家自然科学基金项目(编号: 42230312; 42172262; 42372266)、地球深部探测与矿产资源勘查国家科技重大专项(编号: 2024ZD1000500)和中国地质调查局地质调查项目(编号: DD20240041)联合资助。
作者单位E-mail
张蕾 中国地质科学院地质研究所, 自然资源部大陆动力学重点实验室
江苏东海大陆深孔地壳活动国家野外科学观测研究站 
zhanglei881102@126.com 
李海兵 中国地质科学院地质研究所, 自然资源部大陆动力学重点实验室
江苏东海大陆深孔地壳活动国家野外科学观测研究站 
lihaibing06@163.com 
孙知明 中国地质科学院地质力学研究所, 自然资源部古地磁与古构造重建重点实验室  
曹勇 中国地质科学院地质力学研究所, 自然资源部古地磁与古构造重建重点实验室  
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摘要:
A Review of Rock Magnetism of Pseudotachylyte
      Fault-related pseudotachylytes are critical for understanding seismic processes, as rock magnetic studies can elucidate the physicochemical properties and earthquake mechanisms of seismic faults. Building on recent advances in the rock magnetism of pseudotachylytes and incorporating findings from the Longmen Shan fault zone obtained by the author and their team, this study synthesizes recent advances in the rock magnetism of pseudotachylytes. The formation of magnetic materials in pseudotachylyte involves the transformation of paramagnetic minerals into ferromagnetic minerals (e.g., magnetite and maghemite) under frictional heating at temperatures ranging from 400 °C to 1 300 °C. Under high temperature (≥1 300 °C) and strongly reducing conditions, iron oxides and sulfides decompose to form metallic iron. At ultrahigh temperatures (≥1 500 °C), metallic iron further reacts with sulfur to produce monoclinic pyrrhotite. Analysis of magnetic fabric in pseudotachylytes provides valuable insights into paleoearthquakes mechanisms, paleostress orientation, and paleostrain characteristics. By integrating rock magnetism with paleomagnetism, geochemistry, numerical simulations, and microstructural analysis, key seismogenic parameters—such as coseismic frictional melting temperatures, seismogenic depths, redox conditions, and fluid interactions—can be constrained. A comprehensive approach combining rock magnetic analyses, nanoscale microscopy, microgeochemistry, high- to ultrahigh-temperature heating, and rapid shear experiments holds great promise for decoding the magnetic record of pseudotachylytes and retrieving direct physicochemical and stress information from seismic fault zones.
ZHANG Lei,LI Haibing,SUN Zhiming,CAO Yong.2026.A Review of Rock Magnetism of Pseudotachylyte[J].Acta Geoscientica Sinica,47(1):17-30.
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