PARAGENESIS OF MINERALS Meaning and
Definition
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Paragenesis of minerals refers to the mineral assemblage or association that occurs together within a specific geological setting or environment. It describes the sequence and relationship in which various minerals crystallize and form together during the processes of mineralization.
When different minerals coexist in the same geological setting, their formation is influenced by various factors such as temperature, pressure, chemical composition of the surrounding fluids, and the time frame over which the mineralization occurs. These factors determine which minerals are stable and able to crystallize in a specific sequence.
The paragenesis of minerals provides valuable information about the conditions under which they formed and can be used to infer the geological history and processes that shaped a particular rock or mineral deposit. By analyzing the specific minerals present in a sample, geologists can gain insights into the temperature and pressure conditions at which the mineralization occurred, as well as the composition and evolution of the fluids involved.
The study of paragenesis is especially important in economic geology, where it helps in locating and understanding ore deposits and mineral resources. Certain minerals are indicative of specific processes or conditions, and their presence or absence can be used to identify the potential for economic mineralization in a given area.
Overall, the paragenesis of minerals provides a useful framework for understanding the relationships and interactions between different minerals within a geological context, contributing to our knowledge of Earth's processes and the formation of valuable mineral resources.
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A term in mineralogy applied to crystalline compounds whose mass is made up of crystals interblended in imperfect or irregular forms.
Etymological and pronouncing dictionary of the English language. By Stormonth, James, Phelp, P. H. Published 1874.
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