(This assignment is currently being posted here in lieu of having a working team forum and will be posted there as soon as possible)
Dear team members,
The objective of this assignment is to define what an “End-Member Phase” is on a binary phase diagram and show how it relates to the subject of geology. I will be writing these definitions directed at an audience of board members or investors who may not have a lot of background geologic knowledge. The situation I have put myself in is that of writing a report about mineral formation and mineral properties, specifically to relate it to conditions of rock formation. In this report, these definitions and examples would be used to thoroughly explain “End-Member Phases”.
Thank you for taking the time to read and review my first work on definitions,
Kai Corley-Jory
Parenthetical Definition:
Forsterite and Fayalite are the two end-member phases (most pure extremes) of olivine.
Sentence Definition:
End-Member Phases are mineral formulas that showcase the most extreme versions of a mineral that has many possible configurations.
Extended Definition:
End Members of a Mineral Phase Diagram
Sentence Definition: End Member phases are mineral formulas that showcase the most extreme versions of a mineral that has many possible configurations. Etymology: The term “End-Member” is derived from the words “end”, which in reference to mineral phases means “The initial or the terminal point.”, and “member”, which means “A part of a whole.”
Description & Analysis: Many minerals do not have a static formula, and thus require complex phase diagrams to explain their constituents under different conditions of formation. End-Member phases showcase the extreme possibilities of mineral configuration. A binary phase diagram for the mineral Olivine (Fe, Mg)2SiO4 and its two end-members, Forsterite Mg2SiO4 and Fayalite Fe2SiO4 are shown in Figure 1.
FIGURE 1: Binary Phase Diagram for Olivine
History: Phase Diagrams are commonly used by scientists for the prediction of composition and state phase of substances (minerals) over a range of different conditions, commonly temperature and pressure. Figure 1 depicts a phase diagram for olivine with the variable conditions being temperature, in degrees Celsius, and the Magnesium to Iron content represented by the End Members, of a produced mineral at a constant pressure.
How it is used: End-Member phases are used in conjunction with phase diagrams to calculate possible percentages of mineral constituents that form in any one system. This principle is a useful tool for geologists and can be used in to back out the conditions of formation of rocks with a certain composition of minerals.
Bibliography:
“Endmember.” Ship Ahoy – Wiktionary, en.wiktionary.org/wiki/endmember.
“End.” Ship Ahoy – Wiktionary, en.wiktionary.org/wiki/end#English.
“Member.” Ship Ahoy – Wiktionary, en.wiktionary.org/wiki/member#English.
“Binary Phase Diagrams.” Examples, 10 Nov. 2016, serc.carleton.edu/research_education/equilibria/binary_diagrams.html.