Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences
2017 Annual Meeting of Japan Association of Mineralogical Sciences
Session ID : S2-P04
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Host: Japan Association of Mineralogical Sciences

S2: Water Rock Interaction
Talc CPO formed by Si-metasomatism at the slab-mantle interfaces in subduction zones
*Takayoshi Nagaya, Atsushi Okamoto, Simon R Wallis, Ryosuke Oyanagi, Jun Muto, Masaoki Uno
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Keywords: Talc, Si-metasomatism, Crystallographic Preferred Orientation (CPO), EBSD
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Abstract
EBSD measurements using talc schists collected from the boundary between pelitic schist and antigorite serpentinite show talc CPO show the strong concentration of the normal direction of the (001) plane that is normal to the foliation. The strongest concentrations of the [100] and [010] directions of talc show the direction parallel to the lineation, and the direction parallel to the foliation and normal to the lineation, respectively.
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© 2017 Japan Association of Mineralogical Sciences
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