1.1 Introduction - Introduction to Mineralogy Introduction...

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Unformatted text preview: Introduction to Mineralogy Introduction to Mineralogy Mineralogy can be: Complex Difficult Boring Interesting Exciting Because… It’s a mix of complex/new ideas, with massive amounts of rote memorization. Objectives Objectives Three parts to class (originally three classes): Learn chemical properties of minerals 1. • • Crystallography – spatial arrangement of atoms Crystal chemistry – what atoms make up minerals and why Analytical methods: 1. 1. • • • 1. Physical properties (this week’s lab) – visual observations Polarizing microscope X­ray diffraction Identify, classify and organize minerals Why study mineralogy? Why study mineralogy? Minerals are chemical compounds that form from natural chemical/earth processes Minerals are basic building blocks of rocks Rocks provide record of earth history and are formed by earth processes Holistic Earth science: Earth history Earth processes Definition of Mineral Definition of Mineral A naturally occurring, homogeneous solid, with a defined (but generally not fixed) chemical composition and an ordered atomic arrangement 1. Naturally occurring 1. Naturally occurring Why not synthetic (man­made)? E.g. diamonds Corian countertops (quartz) Table salt (halite) Others? Salar de Uyuni, Bolivian Altiplano San Francisco Bay 2. Homogeneous solid 2. Homogeneous solid Minerals can not be PHYSICALLY broken into new compounds How about chemically “broken”? What would they break into? Why solid? Physical Reaction: Big Feldspar → Little Feldspar Chemical reaction: Albite → Na+ + Al3+ + SiO44- 3. Defined, but not fixed, 3. Defined, but not fixed, composition The compositions of minerals are strictly defined (stoichiometry), but can vary between compositions For example: Calcite is CaCO3 but will also contain much Mg, Sr, Fe, Mn etc. Olivine ­ (Fe,Mg)SiO4 ­ is a group of two main minerals: Fayalite (Fe2SiO4) Forsterite (Mg SiO ) 2 4 4. Ordered atomic arrangement 4. Ordered atomic arrangement Crystallography – how atoms are arranged in space. For example: Aragonite (CaCO3) and Calcite (CaCO3) are different minerals but have identical compositions This is why minerals are referred to by name rather than formula Mineral names include both composition (chemistry) and crystallography ...
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This note was uploaded on 09/19/2011 for the course GLY 3200 taught by Professor Staff during the Fall '10 term at University of Florida.

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