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Dynamic and thermal effects are combined in varying proportions and timescales and a wide range of P-T conditions may occur.

Burial metamorphism is a type of metamorphism, mostly of regional extent, which affects rocks deeply buried under a sedimentary-volcanic pile and is typically not associated with deformation or magmatism.

The resultant rocks are partially or completely recrystallised and generally lack schistosity. The recrystallisation, which is mostly incomplete, encompasses a wide range of temperatures.

The metamorphism is associated with circulating hot aqueous fluids with related metasomatism and typically shows an increasing temperature of metamorphism with depth.

Grain size reduction typically occurs in the rocks, and a range of rocks commonly referred to as mylonites and cataclasites is formed.

It includes melting and vaporisation of the target rock s. It is essentially caused by the heat transfer from the intruded magma body into the country rocks.

The range of metamorphic temperatures may be very wide. It may or may not be accompanied by significant deformation depending upon the dynamics of the intrusion.

It is most typically developed in xenoliths enclosed in such bodies. Pyrometamorphism may be accompanied by various degrees of partial melting to form, for example, fritted rocks, buchites.

It is typically of local extent in that it may be related to a specific setting or cause e. However, in a setting where igneous intrusion is repetitive e.

Metasomatism is commonly associated with this type of metamorphism. Lightning metamorphism is a type of metamorphism of local extent that is due to a strike of lightning.

The resulting rock is commonly a fulgurite, an almost entirely glassy rock. Depending on whether metamorphism is accompanied by increasing or decreasing temperature two types can be distinguished: As the pressure and temperature increase, a rock of a given chemical composition is expected to undergo a continuous series of chemical reactions between its constituent minerals and any fluid phase present to produce a series of new mineral assemblages that are stable at the higher pressures and temperatures.

Isograds represent mineral reactions not rock chemical composition. Metamorphic facies The concept of metamorphic facies was first proposed by Eskola who later gave the following definition: A metamorphic facies is "a group of rocks characterised by a definite set of minerals which, under the conditions obtaining during their formation, were at perfect equilibrium with each other.

The quantitative and qualitative mineral composition in the rocks of a given facies varies gradually in correspondence with variation in the chemical bulk composition of the rocks".

The Subcommission proposes the following definition of facies, which follows Eskola's writings and the commentaries of other workers.

More recently various authors have recognised distinctions in the assemblages containing prehnite and pumpellyite, and erected three facies or subfacies based on the assemblages prehnite-pumpellyite, prehnite-actinolite and pumpellyite-actinolite.

These facies or subfacies, involving prehnite and pumpellyite, may be collectively referred to as the subgreenschist facies.

Facies boundaries are defined by the appearance or disappearance of a mineral or group of minerals, and not a specific P and T.

Such variations in turn affect the P-T location of the boundary reactions. Defined by the occurrence of zeolites in mafic rocks, but not identifiable in metapelites.

Defined by the occurrence of prehnite and pumpellyite in metabasites. Defined by the occurrence of illite, chlorite and smectite in metapelites. Characterized by the lack of biotite in metasediments and metabasites phengite instead of Bt.

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Free casino bonus virginia casino boote - no deposit required for UK players. Lightning metamorphism is a type of metamorphism of local extent that is due to a strike of lightning.

The resulting rock is commonly a fulgurite, an almost entirely glassy rock. Depending on whether metamorphism is accompanied by increasing or decreasing temperature two types can be distinguished: As the pressure and temperature increase, a rock of a given chemical composition is expected to undergo a continuous series of chemical reactions between its constituent minerals and any fluid phase present to produce a series of new mineral assemblages that are stable at the higher pressures and temperatures.

Isograds represent mineral reactions not rock chemical composition. Metamorphic facies The concept of metamorphic facies was first proposed by Eskola who later gave the following definition: A metamorphic facies is "a group of rocks characterised by a definite set of minerals which, under the conditions obtaining during their formation, were at perfect equilibrium with each other.

The quantitative and qualitative mineral composition in the rocks of a given facies varies gradually in correspondence with variation in the chemical bulk composition of the rocks".

The Subcommission proposes the following definition of facies, which follows Eskola's writings and the commentaries of other workers.

More recently various authors have recognised distinctions in the assemblages containing prehnite and pumpellyite, and erected three facies or subfacies based on the assemblages prehnite-pumpellyite, prehnite-actinolite and pumpellyite-actinolite.

These facies or subfacies, involving prehnite and pumpellyite, may be collectively referred to as the subgreenschist facies. Facies boundaries are defined by the appearance or disappearance of a mineral or group of minerals, and not a specific P and T.

Such variations in turn affect the P-T location of the boundary reactions. Defined by the occurrence of zeolites in mafic rocks, but not identifiable in metapelites.

Defined by the occurrence of prehnite and pumpellyite in metabasites. Defined by the occurrence of illite, chlorite and smectite in metapelites.

Characterized by the lack of biotite in metasediments and metabasites phengite instead of Bt. No albite epidote or grossular garnet are the stable Ca Al silicates.

Eclogites can be subdivided into three groups: Eclogites that form in the mantle and are brought up to the surface with kimberlites in diatremes.

Garnets in these eclogites are rich in pyrope. Eclogites that form in the lower crust and are associated with gneiss terrains granulites and high grade amphibolites.

Garnets in this group are rich in grossular and almandine. Eclogites that form at relatively low temperatures in what are now known as subduction zones.

These eclogites contain almandine rich garnet and are associated with blueschists. Facies, Protolith and Mineral assemblage for different protolith.

Protolith refers to the original rock, prior to metamorphism. In low grade metamorphic rocks, original textures are often preserved allowing one to determine the likely protolith.

As the grade of metamorphism increases, original textures are replaced with metamorphic textures and other clues, such as bulk chemical composition of the rock, are used to determine the protolith: These rocks are derivatives of aluminous sedimentary rocks like shales and mudrocks.

Because of their high concentrations of alumina they are recognized by an abundance of aluminous minerals, like clay minerals, micas, kyanite, sillimanite, andalusite, and garnet.

Rocks that originally contained mostly quartz and feldspar like granitic rocks and arkosic sandstones will also contain an abundance of quartz and feldspar as metamorphic rocks, since these minerals are stable of a wide range of temperature and pressure.

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