The Protolith To A Marble Is Sandstone

Sandstone is sedimentary rock where the individual grains of sand that compose the rock are visible without magnification.

The protolith to a marble is sandstone.

Metamorphic rocks have protoliths and limestone or dolomite are the protoliths of marble. What is the protolith of amphibolite. Question 3 is the protolith for marble. What is the protolith of quartzite.

The sample is from estonia. Marble is extensively used as a dimension stone and it has been favored by architects since the antiquity. What is the protolith of gneiss. Sandstone shale granite limestone question 4 metamorphism may be initiated by.

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 under the conditions of metamorphism the calcite in the limestone recrystallizes to form a rock that is. Quartzite outcrops can be found in many mountain ranges all over the world. A protolith is the parent rock. Marble is made of calcite or some other carbonate and this mineral is common in only one possible protolith.

Width of sample 10 cm. Produces similarly quartzite is made only of quartz and only quartz sandstone has enough of that mineral and no others to be a reasonable protolith. What is the protolith of skarn. Quartzite is a common metamorphic rock because its protolith sandstone is very widespread.

Any rock type but often shale. However mostly because of marketing reasons some coarse grained limestones grainstones and dolomites are also sold as marble varieties. Sandstone is a protolith as it is so it does not have a protolith. Marble is a metamorphic rock.

Limestone or some other carbonate rock. Contact with an igneous intrusion contact with hot groundwater heat and pressure associated with deep burial all of the above are correct question 5 the minerals found in a metamorphic rock depend on. Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism.