Thermal structure beneath Far Eastern Russia inferred from geothermobarometric analyses of mantle xenoliths: Direct evidence for high geothermal gradient in backarc lithosphere

Journal

  • Tectonophysics

    Tectonophysics (554-557), 74-82, 2012-07-25

    Elsevier B.V.

Cited by:  1

Codes

  • NII Article ID (NAID)
    120004689043
  • Text Lang
    ENG
  • Article Type
    Journal Article
  • ISSN
    0040-1951
  • Data Source
    CJPref  IR 
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