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ERSC 2P12 Minerals 1 Minerals Background material essential in the description of rocks ERSC 2P17 - Brock University Greg Finn 2006 Minerals • This course is not a replacement or substitute for mineralogy (ERSC 2P21) • how to identify and recognize minerals that make up rocks • in excess of 3,000 minerals have been identified on Earth • however 90-95% of the Earth’s crust is composed of 8 minerals (these plus ~12 more you should be familiar with) ERSC 2P17 - Brock University Greg Finn 2006 What is a Mineral? • A homogeneous, naturally occurring, solid, inorganic substance, with a definable chemical composition, and an internal structure characterized by an orderly arrangement of atoms, ions and molecules in a lattice. ERSC 2P17 - Brock University Greg Finn 2006 1 ERSC 2P12 Minerals 1 What is a Mineral? Homogeneous ERSC 2P17 - Brock University Greg Finn 2006 What is a Mineral? Naturally Occurring ERSC 2P17 - Brock University Greg Finn 2006 What is a Mineral? Solid ERSC 2P17 - Brock University Greg Finn 2006 2 ERSC 2P12 Minerals 1 What is a Mineral? Inorganic Substance ERSC 2P17 - Brock University Greg Finn 2006 What is a Mineral? Definable Chemical Composition ERSC 2P17 - Brock University Greg Finn 2006 What is a Mineral? Orderly Arrangement of Atoms ERSC 2P17 - Brock University Greg Finn 2006 3 ERSC 2P12 Minerals 1 Naming Minerals • Each mineral has its own name, generally derived from: ERSC 2P17 - Brock University Greg Finn 2006 Naming Minerals (continued) ERSC 2P17 - Brock University Greg Finn 2006 Groups of Minerals • Different groups of minerals which are important to humans: ERSC 2P17 - Brock University Greg Finn 2006 4 ERSC 2P12 Minerals 1 Classes of Minerals • >3,000 minerals have been identified • can be separated into 7 groups or classes based on the chemical similarities and differences • silicates vs nonsilicates ERSC 2P17 - Brock University Greg Finn 2006 Classes of Minerals • Silicates comprise most of the minerals found on Earth • basic building block is the silica tetrahedron consisting of one silicon atom surrounded by 4 oxygen atoms • large number of silicate minerals identified and these differ in the way the silica tetrahedra are linked and the cations present ERSC 2P17 - Brock University Greg Finn 2006 Silica Tetrahedron • 4 oxygen surrounding 1 silicon Exploded view Schematic view ERSC 2P17 - Brock University Greg Finn 2006 5 ERSC 2P12 Minerals 1 Nonsilicates • Oxides • Sulphides • Sulfate ERSC 2P17 - Brock University Greg Finn 2006 Nonsilicates • Halides • Carbonates • Native elements ERSC 2P17 - Brock University Greg Finn 2006 Isolated/Independent Silicates • Si:O 1:4 ERSC 2P17 - Brock University Greg Finn 2006 6 ERSC 2P12 Minerals 1 Chain Silicates • Single-chain • Double-chain – Si:O 1:3 – Si:O 4:11 ERSC 2P17 - Brock University Greg Finn 2006 Phyllosilicates • Sheet silicates – Si:O 2:5 ERSC 2P17 - Brock University Greg Finn 2006 Tectosilicates Structure too complicated to show • Framework Silicates – Si:O 1:2 ERSC 2P17 - Brock University Greg Finn 2006 7