The two main influences are the kind of limestone that makes up the parent rock and the kind and degree of metamorphism.
Limestone marble parent rock.
The parent rock of gneiss can be.
The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals.
Is marble and limestone an example of a metamorphic rock and its parent rock.
Start studying parent rocks of metamorphic rocks.
It can be virtually any color from white to black to red to green etc and sometimes it will contain metamorphosed fossils or other components.
Parent rock of marble.
Shale granite hornblende garnet muscovite schist.
It can be most any color including white black reds greens and more.
Parent rock of gneiss.
Generally high amounts of magnesium in limestone give a greenish tint to the marble.
Are slate phyllite garnet muscovite schist regional or contact.
Both regional and contact.
Since it is composed of calcite it can be tested with dilute hydrochloric acid.
It is composed primarily of the mineral calcite caco 3 and usually contains other minerals such as clay minerals micas quartz pyrite iron oxides and graphite.
The parent rock of marble is.
Marble both limestone and dolomitic is an extremely variable rock in appearance since it depends on what rock was the parent and the degree of metamorphism it underwent.
Marble is most commonly used for sculpture and as construction material.
Limestone is a carbonate sedimentary rock that is often composed of the skeletal fragments of marine organisms such as coral foraminifera and molluscs its major materials are the minerals calcite and aragonite which are different crystal forms of calcium carbonate caco 3 a closely related rock is dolomite which contains a high percentage of the mineral dolomite camg co 3 2.
The parent rock of hornblende schist is.
Marble is a rock resulting from metamorphism of sedimentary carbonate rocks most commonly limestone or dolomite rock.
Limestone is considered to be the most common parent rock of marble.
If it bubbles it is composed of calcite and.
It is usually course grained though fine grained marble is found in some places and is highly prized for creating sculptures.
Parent rock of athracite coal.
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Metamorphism causes variable recrystallization of the original carbonate mineral grains.
Limestone can be the parent rock of skarn and marble.