Protolith
 | This article needs additional citations for verification. (January 2021) |
A protolith (from Ancient Greek πρωτο (prōto) 'first' and λίθος (líthos) 'stone') is the original, unmetamorphosed rock from which a given metamorphic rock is formed.[1][2]
For example, the protolith of a slate is a shale or mudstone. Metamorphic rocks can be derived from any other kind of non-metamorphic rock and thus there is a wide variety of protoliths. Identifying a protolith is a major aim of metamorphic geology.
Protoliths are non-metamorphic rocks and have no protoliths themselves. The non-metamorphic rocks fall into two classes: sedimentary rocks, formed from sediment, and igneous rocks, formed from magma. The source of the sediment of a sedimentary rock is termed its provenance.
Magmatic protoliths can be further divided into three categories: ultramafic rock, mafic rock, and quartzo-feldspathic rock. Similarly, sedimentary protoliths can be classified as quartzo-feldspathic, pelitic, carbonate rocks, or some mixture of the three.[3]
On a geological time scale, the first protoliths were first formed[how?] shortly after the formation of the Earth during the Hadean eon.[citation needed]
References
[edit]- ^ "Basics--Rocks-Metamorphic". commons.wvc.edu. Retrieved 2022-10-17.
- ^ "protolith". The Free Dictionary. Farlex.
- ^ Hoinkes, G.; Hauzenberger, C. A.; Schmid, R. (2014-01-01), "Classification, Nomenclature, and Formation☆", Reference Module in Earth Systems and Environmental Sciences, Elsevier, doi:10.1016/b978-0-12-409548-9.09049-7, ISBN 978-0-12-409548-9, retrieved 2022-10-17
 | This article related to petrology is a stub. You can help Wikipedia by expanding it. |