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Olivines also occur in metamorphic environments.
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Although it is difficult to single out the seismogenic mechanism from a number of proposed models, more detailed discussions of the relationship between hypocenter locations, fault segmentation and the material structure contrast around the plate boundary, are important for considering the seismogenic mechanism in terms of metamorphic environments (e.g., Hyndman and Peacock, 2003).
In this vein, it is not surprising that our phenotype-environment correlations found that divergence in metamorphic mass is most closely related to pond pH, whereas divergence in larval period is most closely related to latitude, and larval growth to predator density, respectively.
Jadeite is found only in metamorphic rocks.
It can also occur in metamorphic rocks.
The rock-forming garnets are most common in metamorphic rocks.
Hornblende occurs widely in metamorphic and igneous rocks.
Amphiboles are found principally in metamorphic and igneous rocks.
Quartz-bearing strata are abundant in metamorphic terrains.
Muscovite is particularly common in metamorphic gneisses, schists, and phyllites.
Thus, the study of porphyroblast fabrics in metamorphic rocks can be complex but has the potential to yield important information on the structural history of metamorphic regions.
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