An unzoned mineral that is often zoned at lower-medium metamorphic grades has both experienced large temperature problems or was in no way zoned (owing to a simple reaction historical past at restricted P-T or to development solely at high-T). Response textures Some metamorphic rocks consist of evidence for incomplete reactions or other textural evidence for part of the P-T path. An easy case in point would be the partial replacement of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural evidence may also be handy in situations the place the reactants are actually completely eaten if The form of one or more reactants are preserved; by way of example, pseudomorphs (Figs. 6b-d). An example of a more advanced reaction texture includes the development of coronas , which include a number of shells (rims, moats) of a mineral or minerals all around a central (reactant) period (Fig. 6e). In many scenarios, coronas also include the high-quality-scale intergrowth of minerals inside a texture often known as symplectite (Figs. 6e-f).
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For many rocks, the only A part of the P-T path recorded while in the mineral assemblage and texture of your rock is the 'peak' of metamorphism -- the situations on the thermal utmost (i.e., the most here temperature as well as pressure at the maximum temperature). In the event the rock had a sedimentary or volcanic protolith, it is possible to infer which the rock begun at the surface, attained peak situations at some temperature and depth inside the Earth, and returned on the floor (where by the rock was gathered).
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