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This is a private module sandbox of Wyang, for their own experimentation. Items in this module may be added and removed at Wyang's discretion; do not rely on this module's stability.

of the metamorphic rock may be the list of all P-T problems experienced by a rock through its metamorphic background (Determine 1).

Crystals which have diverse regions with distinct compositions are zoned . A quite common zoning sample requires a change in composition of a mineral's Centre (core) when compared to its rim, and concentric rings of various compositions organized amongst the core as well as the rim (Fig. 5). Minerals that generally demonstrate this kind of zoning in the key or trace factors are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of such, garnet and plagioclase are suitable to research of metamorphic P-T paths, and zircon is relevant Click Here to determination of your timing of petrologic gatherings.

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