The metamorphics rocks (1)

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•Cristian Galván Izquierdo •Íker Gil Fabregat •Llàtzer Miguel Valdès THE METAMORPHIC ROCKS

Transcript of The metamorphics rocks (1)

Page 1: The metamorphics rocks (1)

•Cristian Galván Izquierdo •Íker Gil Fabregat •Llàtzer Miguel Valdès

THE METAMORPHIC ROCKS

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ÍNDEX●What are the metamorphics rocks?●What are the regional and contact metamorphism?●Which are the metamorphics rocks?●Exemples: Slate, Gneiss, Schist, Marble, Micasquist, Quartzite, Micacita

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WHAT ARE THE METAMORPHIC ROCKS?The metamorphic rocks are subjected to metamorphism.Metamorphism is the set of solid state reactions affecting a rock (of any kind be sedimentary, igneous or metamorphic) subject to conditions of pressure and different to its origin temperature.

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WHAT ARE THE REGIONAL AND CONTACT METAMORPHISM?

Contact metamorphism is a type of metamorphism in which the change occurs in the rocks by the heat they receive when they are near a magma intrusion.

Regional metamorphism is a type of metamorphism in which the change occurs in conditions of high pressure and sometimes high temperatures.

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WHICH ARE THE METAMORPHIC ROCKS?

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SLATE (pissarra)It’s formed from metamorphisme of mudstone (argila)

Colour: Black

Fracture: Thin flat layers

Texture: Granular fine and homogeneous

Composition: Crystals not observable to the naked eye

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GNEISSIt’s a foliated rock with a banded appearance and granulars mineral grains. It’s formed from granit or clays. It has wavy layers, because of the grains of granit.

Colour: Dark and light stripes

Fracture: Strips

Texture: Planar rude

Composition: Quartz, feldspar and mica.

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MICASQUIST

Colour: Gray tones

Fracture: sheet

Texture: Schistose lepidoblastic

Composition: Mica, quartz and other minerals.

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SCHIST

Colour: Fairly homogeneous

Fracture: A wavy and irregular structure sheet (schistose structure)

Texture: Flaky

Composition: Muscovite, biotite, chlorite, quartz, plagioclase and chloritoid, staurolite, andalusite, kyanite, garnet, sillimanite

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MARBLE It’s formed by metamorphisme of calcareous, so it reacts with hydrochloric acid, and it makes effervescence.

Colour: white, pink, green, … it depends on the impurities.

Fracture: not foliated

Texture: fine to coarse grained,.

Composition: CaCO3, mica, magnesium silicates, graphite, iron oxides

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QUARTZITEIt’s formed by metamorphisme of sandstone.

Colour: usually white to gray

Fracture: conchoidal fracture

Texture: coarse texture

Composition: almost entirely of quartz

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MICA SCHIST (MICACITA)

Colour: green, grey, dark brown.

Fracture: medium grained.

Texture: foliated, platy.

Composition: quartz and mica (biotite or muscovite)