EPIDOTIZATION Meaning and
Definition
-
Epidotization is a geological process characterized by the alteration and transformation of a rock or mineral into epidosite, a type of metamorphic rock containing the mineral epidote. This process typically occurs as a result of regional metamorphism, in which high pressures and temperatures lead to the recrystallization of pre-existing minerals into new ones.
During epidotization, the original mineralogy and texture of the rock are progressively modified. The mineral epidote, a calcium aluminum iron silicate, is commonly formed as a result of the process. This mineral often replaces other minerals such as plagioclase feldspar, pyroxene, hornblende, or other ferromagnesian minerals in the original rock, resulting in the distinctive characteristics of epidosite.
Epidotization usually takes place in the presence of fluids, such as hot water or hydrothermal solutions, that facilitate the movement of ions and the exchange of elements between minerals. These fluids play a vital role in the chemical reactions involved in the alteration process, allowing the components of the original rock to be dissolved or reprecipitated in the form of epidote.
The transformation of rocks through epidotization can provide a wealth of information about the geological conditions and history of a particular region. The resulting epidosite may exhibit specific textures and mineral assemblages that help geologists understand past tectonic events, thermal gradients, fluid flow patterns, and other geological processes that have influenced the area.
Common Misspellings for EPIDOTIZATION
- wpidotization
- spidotization
- dpidotization
- rpidotization
- 4pidotization
- 3pidotization
- eoidotization
- elidotization
- e0idotization
- epudotization
- epjdotization
- epkdotization
- epodotization
- ep9dotization
- ep8dotization
- episotization
- epixotization
- epicotization
- epifotization
- epirotization
Etymology of EPIDOTIZATION
The word "epidotization" is derived from the noun "epidote" and the suffix "-ization".
The term "epidotization" is associated with the mineral "epidote", which is a silicate mineral commonly found in metamorphic rocks. It forms as a result of the metamorphic alteration of pre-existing minerals during the process known as "epidotization".
The suffix "-ization" is derived from Latin and is often used to form nouns that indicate a process or result. In this case, "epidotization" refers to the process of metamorphic alteration leading to the formation of the mineral epidote.
Infographic
Add the infographic to your website:
