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  • 标题:Frictional properties of anorthite (feldspar): implications for the lower boundary of the seismogenic zone
  • 本地全文:下载
  • 作者:Koji Masuda
  • 期刊名称:Earth, Planets and Space
  • 电子版ISSN:1880-5981
  • 出版年度:2020
  • 卷号:72
  • 期号:1
  • 页码:1-6
  • DOI:10.1186/s40623-020-01271-6
  • 出版社:Springer Verlag
  • 摘要:Earthquake magnitude is closely related to the depth extent of the seismogenic zone, and higher magnitude earthquakes occur where the seismogenic zone is thicker.The frictional properties of the dominant mineral constituents of the crust, such as feldspar-group minerals, control the depth extent of the seismogenic zone.Here, the velocity dependence of the steady-state friction of anorthite, the calcic endmember of the feldspar mineral series, was measured at temperatures from 20 to 600 °C, pore pressures of 0 (“dry”) and 50 MPa (“wet”), and an efective pressure of 150 MPa.The results support previous fndings that the frictional properties of feldspar play a dominant role in limiting the depth extent of the seismogenic zone.This evidence suggests that brittle deformation of anorthite may be responsible for brittle fault movements in the brittle–plastic transition zone.
  • 关键词:Fault friction; Feldspar; Anorthite; Albite; Quartz
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