
Nguồn ngoài
Mineralogy
Minerals are our planet. They form the Earth and the bedrock that we live on, making up all of Earth’s rocks and sediments, and they are important components in soils. So, they literally are the foundations for our lives. Perhaps because they are ubiquitous, most people don’t even notice them or consider that all rock is made of minerals.
- Tác giả
- Dexter Perkins et al.
- Nhà xuất bản
- University of North Dakota
- Nguồn
- LibreTexts
- Giấy phép
- CC BY-NC-SA
- Ngôn ngữ
- EN
- Danh mục
- Khoa học cơ bản
Mục lục· 324 mục
- 01: Introduction
- 1.01: The Importance of Minerals
- 1.1.01: Mineral Commodities
- 1.1.02: Ore Minerals
- 1.1.03: The Importance of Crystallography
- 1.02: Definition of a Mineral
- 1.2.01: Traditional Definition
- 1.2.02: Matter and Minerals
- 1.2.03: Minerals and Mineral Varieties
- 1.2.04: Synthetic Minerals and Simulants
- 1.2.05: Crystalline and Non-Crystalline Mineral Materials
- 1.2.06: Biominerals
- 1.2.07: Anthropogenic Minerals
- 1.03: Elements Minerals and Rocks
- 1.04: Classifying Minerals
- 1.4.01: Subclasses Groups and Smaller Divisions
- 1.4.02: An Example- Pyroxenes
- 02: Mineral Chemistry
- 2.01: Elements and Minerals
- 2.02: Elements and the Periodic Table
- 2.2.01: Groups
- 2.2.02: Atomic Number and Mass
- 2.2.03: Moles
- 2.2.04: Radioactive Minerals
- 2.2.05: Periods
- 2.03: Ions
- 2.3.01: Typical Valences
- 2.04: Bonding in Minerals
- 2.4.01: Ionic Bonds
- 2.4.1.01: Common Cations and Anions
- 2.4.02: Covalent Bonds
- 2.4.03: Metallic Bonds
- 2.4.04: Other Kinds of Bonds
- 2.4.05: Ionic Covalent and Metallic Crystals
- 2.4.5.01: Bonding and Mineral Properties
- 2.05: Compositional Variation in Minerals
- 2.5.01: How to Normalize a Mineral Analysis
- 2.06: Common Minerals
- 2.6.01: Common Elements Make Up the Common Minerals
- 03: Mineral Properties
- 3.01: Naming Minerals
- 3.02: Mineral Identification
- 3.03: Crystal Shape
- 3.3.01: Crystal Forms
- 3.3.02: Mineral Habit
- 3.04: Mineral Appearance
- 3.4.01: Luster
- 3.4.02: Diaphaneity
- 3.4.03: Color
- 3.4.04: Streak
- 3.4.05: Luminescence
- 3.4.06: Play of Colors
- 3.05: Strength and Breaking
- 3.5.01: Tenacity
- 3.5.02: Cleavage Fracture and Parting
- 3.5.03: Hardness
- 3.06: Density and Specific Gravity
- 3.07: Magnetism
- 3.08: Electrical Properties
- 3.09: Reaction to Dilute Hydrochloric Acid
- 3.10: Additional Properties
- 04: Crystals and Crystallization
- 4.01: Crystalline and Noncrystalline Solids
- 4.02: Forming Crystals
- 4.2.01: Igneous Minerals
- 4.2.02: Aqueous Minerals
- 4.2.03: Hydrothermal Minerals
- 4.2.04: Metamorphic Minerals
- 4.2.05: Weathering and Diagenesis
- 4.03: Mineral Stability and Polymorphs
- 4.04: Factors Controlling Crystal Size and Perfection
- 4.4.01: Time and Temperature
- 4.4.02: Ostwald Ripening
- 4.4.03: Organized Atomic Arrangements
- 4.4.04: Crystal Defects
- 4.4.05: Crystal Zoning
- 4.4.06: Crystal Twinning
- 4.05: Life Spans of Minerals
- 05: Optical Mineralogy
- 5.01: Introduction to Mineral Optics
- 5.02: Light and the Properties of Light
- 5.2.01: Interference
- 5.2.02: The Velocity of Light in Crystals and the Refractive Index
- 5.03: Polarization of Light
- 5.3.01: Polarized Light
- 5.3.02: Crossed Polars
- 5.3.03: Polarized Light Vibrating at an Angle to a Polarizing Filter
- 5.04: Petrographic Microscopes
- 5.4.01: The Components of a Microscope
- 5.4.02: Plane (PP) Polarized Light and Cross Polarized (XP)Light
- 5.05: More About Uniaxial and Biaxial Minerals
- 5.5.01: Extinction Angles
- 5.5.02: Accessory Plates and the Sign of Elongation
- 5.06: Interference Figures
- 5.6.01: Uniaxial Interference Figures
- 5.6.02: Biaxial Interference Figures
- 5.07: Identifying Minerals and Mineral Properties in Thin Section
- 06: Igneous Rocks and Silicate Minerals
- 6.01: Magmas and Igneous Rocks
- 6.1.01: Where Do Igneous Rocks Occur
- 6.02: Compositions of Igneous Rocks
- 6.2.01: Mafic and Silicic Magmas
- 6.2.02: Volatiles
- 6.03: Crystallization of Magmas
- 6.3.01: Equilibrium Between Crystals and Melt
- 6.3.02: Bowens Reaction Series
- 6.3.03: Disequilibrium
- 6.04: Silicate Minerals
- 6.4.01: Summary - Silicate Minerals and Igneous Rocks
- 6.4.02: SiO2 Polymorphs
- 6.4.03: Feldspars
- 6.4.04: Feldspathoids
- 6.4.05: Micas
- 6.4.06: Chain Silicates
- 6.4.07: Pyroxenes
- 6.4.08: Amphiboles
- 6.4.09: Ring Silicates and Paired Tetrahedral Silicates
- 6.4.10: Olivine Group Minerals
- 6.05: Naming Igneous Rocks
- 6.06: Mineral Modes
- 6.07: Common Types of Igneous Rock
- 6.7.01: Silicic Igneous Rocks (20 Quartz)
- 6.7.02: Mafic and Intermediate Igneous Rocks (0 to 20 Quartz)
- 6.7.03: Ultramafic Igneous Rocks
- 07: Sedimentary Minerals and Sedimentary Rocks
- 7.01: Weathering
- 7.1.01: Two Kinds of Weathering
- 7.1.02: Results of Weathering
- 7.1.03: Ease of Weathering
- 7.02: Siliciclastic Sediments
- 7.03: Transportation Deposition and Lithification
- 7.3.01: Clastic Sedimentation
- 7.3.02: Chemical Sedimentation
- 7.04: Sedimentary Minerals
- 7.4.01: Common Minerals
- 7.4.02: Clay Minerals
- 7.4.03: Carbonate Minerals
- 7.4.04: Sulfate Minerals
- 7.4.05: Halides
- 7.4.06: Zeolites
- 7.4.07: Chert
- 7.05: Common Sedimentary Rocks
- 7.5.01: Clastic Sedimentary Rocks
- 7.5.02: Chemical Sedimentary Rocks
- 7.5.03: Organic Sedimentary Rocks
- 7.06: Sedimentary Environments and Facies
- 08: Metamorphic Minerals and Metamorphic Rocks
- 8.01: Different Kinds of Metamorphism
- 8.1.01: 8.1.1 Regional Metamorphism
- 8.1.02: Contact Metamorphism
- 8.1.03: Hydrothermal Metamorphism
- 8.1.04: Dynamic Metamorphism
- 8.1.05: Impact Metamorphism
- 8.1.06: Rocks of Different Metamorphic Grade
- 8.1.07: Prograde and Retrograde Metamorphism
- 8.02: Pressure and Temperature
- 8.2.01: 8.2.1 Heat and Temperature
- 8.2.02: Pressure and Depth
- 8.2.03: Directed Stress
- 8.2.04: Metamorphic Fluids
- 8.03: Metamorphic Textures
- 8.3.01: Grain size and Porphyroblasts
- 8.3.02: Lineations and Foliations
- 8.3.03: Slate
- 8.3.04: Phyllite
- 8.3.05: Schist
- 8.3.06: Gneiss
- 8.3.07: Nonfoliated Metamorphic Rocks
- 8.04: Metamorphic Reactions
- 8.4.01: Different Kinds of Reactions
- 8.4.02: Metamorphic Phase Diagrams
- 8.05: Metamorphic Rocks of Different Compositions
- 8.06: Metasedimentary Rocks
- 8.6.01: Metamorphosed Pelitic Rocks (Metapelites)
- 8.6.02: Metamorphosed Sandstones (Metapsammites)
- 8.6.03: Metamorphosed Limestones and Dolostones (Marbles)
- 8.6.04: Metamorphosed Iron Formations
- 8.07: Metaigneous Rocks and Minerals
- 8.7.01: Metamorphosed Granitic Rocks
- 8.7.02: Metamorphosed Mafic Rocks (Metabasites)
- 8.7.03: Metamorphosed Ultramafic Rocks
- 8.08: High-Pressure Rocks and Minerals
- 09: Ore Deposits and Economic Minerals
- 9.01: Mineral Commodities
- 9.1.01: Mineral Resources
- 9.1.02: The History of Mining
- 9.1.03: Mineral Deposits Ore Deposits and Mining
- 9.1.04: Natural Abundances of Elements
- 9.1.05: Worldwide Distribution
- 9.02: Ore Minerals
- 9.2.01: Native Elements- Metals Semimetals and Nonmetals
- 9.2.02: Sulfides and Sulfosalts
- 9.2.03: Oxides and Hydroxides
- 9.2.04: Gems and Gem Minerals
- 9.03: Types of Ore Deposits
- 9.3.01: Magmatic Ore Deposits
- 9.3.02: Hydrothermal Ore Deposits
- 9.3.03: Sedimentary Ore Deposits
- 10: Crystal Morphology and Symmetry
- 10.01: Symmetry
- 10.1.01: Introduction
- 10.1.02: Identifying Symmetry
- 10.1.03: Mirror Planes
- 10.1.04: Rotational Symmetry
- 10.1.05: Inversion Centers
- 10.1.06: Symmetry Operates on Everything
- 10.1.07: Symmetry Is a Property
- 10.02: Stereo Diagrams
- 10.2.01: Symmetry on Stereo Diagrams
- 10.03: From Points to Crystal Faces and Forms
- 10.3.01: Special Forms and General Forms
- 10.3.02: Open Forms and Closed Forms
- 10.04: Combinations of Symmetry Elements- Point Groups
- 10.4.01: Special Angles and General Angles
- 10.05: Point Groups and Crystal Systems
- 10.5.01: Forms and Point Groups
- 10.5.02: Characteristics of Crystals Belonging to the Different Crystal Systems
- 11: Crystallography
- 11.01: Observations in the Seventeenth through Nineteenth Centuries
- 11.02: Translational Symmetry
- 11.03: Unit Cells and Lattices in Two Dimension
- 11.3.01: Motifs and Unit Cells
- 11.3.02: What are the Possible Plane Lattices
- 11.3.03: How May Motifs and Lattices Combine
- 11.04: Unit Cells and Lattices in Three Dimensions
- 11.4.01: Bravais Lattices
- 11.4.02: Unit Cell Symmetry and Crystal Symmetry
- 11.05: Symmetry of Three Dimensional Atomic Arrangements
- 11.5.01: Space Group Operators
- 11.06: Space Groups
- 11.07: Crystal Habit and Crystal Faces
- 11.08: Quantitative Aspects of Unit Cells Points Lines and Planes
- 11.8.01: Unit Cell Parameters and Crystallographic Axes
- 11.8.02: Points in Unit Cells
- 11.8.03: Lines and Directions in Crystals
- 11.8.04: Planes in Crystals
- 11.09: Miller Indices
- 11.10: The Miller Indices of Planes within a Crystal Structure
- 11.11: Confusing Notations
- 11.12: Crystal Forms and the Miller Index
- 11.12.01: Zones and Zone Axes
- 11.12.02: General Forms and Special Forms
- 12: X-ray Diffraction and Mineral Analysis
- 12.01: X-ray Diffraction
- 12.1.01: Intensity of Diffraction
- 12.1.02: Intensity of Diffraction- Halite
- 12.1.03: X-ray Patterns Symmetry and Mineral Identification
- 12.1.04: Extinctions
- 12.1.05: Indexing Patterns and Determining Cell Parameters
- 12.1.06: Uncertainties
- 12.1.07: Single Crystal Diffraction
- 12.1.08: The Discovery of X-rays and Diffraction
- 12.1.09: What are X-rays
- 12.1.10: Interactions of X-Rays and Atoms
- 12.1.11: Interference of X-Ray Waves
- 12.1.12: Diffraction by a Row of Atoms
- 12.1.13: Diffraction by Planes of Atoms
- 12.1.14: Routine X-Ray Analysis- Powder Diffraction
- 12.1.15: Data and Processing
- 12.1.16: Effects of Different X-ray Wavelengths
- 12.02: Obtaining a Mineral Analysis
- 12.2.01: Electron Microscopes
- 12.2.02: 12.2.2 Electron Microprobes
- 12.2.03: Other Analytical Techniques
- 13: Crystal Structures
- 13.01: The Impact of X-ray Crystallography
- 13.02: Ionic Crystals
- 13.2.01: Ionic Radii
- 13.2.02: Coordination Number
- 13.2.03: Different Kinds of Bonding
- 13.03: Closest Packing
- 13.3.01: Closest Packing in Two Dimensions
- 13.3.02: Packing in Three Dimensions
- 13.3.03: Exceptions to Closest Packing
- 13.04: Paulings Rules
- 13.4.01: Paulings First Rule
- 13.4.02: Paulings Second Rule
- 13.4.03: Paulings Third Rule
- 13.4.04: Paulings Fourth Rule
- 13.4.05: Paulings Fifth Rule
- 13.05: Oxygen and Other Common Elements
- 13.06: Silicate Structures in General
- 13.6.01: Silicate Classification
- 13.6.02: Chemical Trends
- 13.6.03: Complex Atomic Arrangements
- 13.6.04: Elemental Substitutions in Silicates
- 13.6.05: Melting and Weathering Relationships
- 13.07: Structures of the Basic Silicate Subclasses
- 13.7.01: Framework Silicates
- 13.7.02: Sheet Silicates
- 13.7.03: Single Chain Silicates (Pyroxenes and Pyroxenoids)
- 13.7.04: Double Chain Silicates (Amphiboles)
- 13.7.05: Ring Silicates
- 13.7.06: Paired Tetrahedral Silicates
- 13.7.07: Isolated Tetrahedral Silicates
- 13.08: Structures and Chemistry of Nonsilicates
- 14: Mineral Descriptions
- 14.01: Silicate Class
- 14.1.01: Silicate Class - Framework Silicates
- 14.1.02: Silicate Class - Sheet Silicates
- 14.1.03: Silicate Class - Chain Silicates
- 14.1.04: Silicate Class - Ring Silicates
- 14.1.05: Silicate Class - Isolated Tetrahedral Silicates
- 14.1.06: Paired Tetrahedral Silicates
- 14.02: Native Elements
- 14.03: Sulfide Minerals
- 14.3.01: Tetrahedral Sulfides and Arsenides
- 14.3.02: Octahedral Sulfide Group Minerals
- 14.3.03: Other Sulfide Minerals
- 14.04: Halide Minerals
- 14.05: Oxide Minerals
- 14.5.01: Tetrahedral and Octahedral Oxides
- 14.5.02: Spinels and other Oxides with Mixed Coordination
- 14.06: Hydroxide Minerals
- 14.07: Carbonates and Nitrates
- 14.7.01: Calcite Group Minerals
- 14.7.02: Dolomite Group Minerals
- 14.7.03: Aragonite Group Minerals
- 14.7.04: Other Carbonate Minerals
- 14.7.05: Nitrate Group Minerals
- 14.08: Borate Minerals
- 14.09: Sulfate Minerals
- 14.10: Tungstates Molybdates and Chromates
- 14.11: Phosphates Arsenates and Vanadates