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antigorite    
叶蛇纹石

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  • Antigorite - Wikipedia
    Antigorite is a lamellated, monoclinic mineral in the phyllosilicate serpentine subgroup with the ideal chemical formula of (Mg,Fe 2+) 3 Si 2 O 5 (OH) 4 [2] It is the high-pressure polymorph of serpentine and is commonly found in metamorphosed serpentinites
  • Antigorite: Mineral information, data and localities.
    Antigorite is a higher temperature serpentine mineral, forming only above 250°C (Wenner Taylor, 1974; Evans, 1977); chrysotile and lizardite are lower temperature polymorphs Antigorite is not the most common serpentine mineral, although it is a common member of the group
  • Antigorite Mineral Data
    Antigorite Comments: Yellowish green, fibrous antigorite Location: East Broughon, Quebec, Canada Scale: 22x10 cm © Dave Barthelmy
  • Antigorite (Mg 2+ 3 2 5 4 - Handbook of Mineralogy
    Occurrence: Commonly replaces ultrama ̄c rocks, pervasively or in crosscutting veinlets As a replacement of siliceous dolostone along contacts with diabase sills Chromite, magnetite, chrysotile, olivine Distribution: Widespread; less common however than lizardite
  • Antigorite - ALEX STREKEISEN
    Antigorite is a mineral belonging to the serpentine group of minerals Antigorite forms during low-grade metamorphism of olivine-rich rocks (peridotite and other ultrabasic rocks, gabbros, lamprophyres, etc ); is a major component in serpentinites
  • Antigorite - Rock Identifier
    Antigorite is a lamellated, monoclinic mineral in the phylosilicate serpentine subgroup with the ideal chemical formula of (Mg,Fe)3Si2O5(OH)4 It is the high-pressure polymorph of serpentine and is commonly found in metamorphosed serpentinites
  • Antigorite | mineral | Britannica
    Serpentine generally occurs in three polymorphs: chrysotile, a fibrous variety used as asbestos; antigorite, a variety occurring in either corrugated plates or fibres; and lizardite, a very fine-grained, platy variety





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