The six crystal systems | Optical Mineralogy Lesson 2 | Crystallography
GEO -VENTURES
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The six crystal systems | Optical Mineralogy Lesson 2 | Crystallography
10 просмотров · 9 дн. назад
GEO -VENTURES
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10 просмотров · 9 дн. назад
📐 OPTICAL MINERALOGY LESSON 2: Basic Crystallography & External Symmetry
Prescribed Reference: Klein & Dutrow (2007) Manual of Mineral Science (23rd ed., Chapter 6)
Welcome to Lesson 2 of our Geology & Optical Mineralogy series! In this tutorial, we explore the geometric fundamentals of crystallography. Learn how internal unit cell translation dictates external crystal symmetry, master the 4 primary symmetry elements (Rotation axes, Mirror planes m, Center of Inversion i, and Rotoinversion axes), orient 3D crystallographic reference axes (a, b, c and a1, a2, a3, c), prove why 5-fold rotation axes are forbidden in 3D lattices, and explore the diagnostic rules, unit cell constraints, and mineral examples for all 6 Crystal Systems (Isometric, Tetragonal, Orthorhombic, Hexagonal, Monoclinic, Triclinic).
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⏱️ TIMESTAMPS:
00:00 - Introduction & Learning Outcomes
00:48 - What is Basic Crystallography? (External Morphology vs. Internal Unit Cells)
01:40 - Defining Symmetry in Crystalline Solids (Invariance & Point Symmetry)
02:30 - Proper Rotation Axes (1, 2, 3, 4, 6-Fold) & The 5-Fold Axis Prohibition
03:55 - Mirror Planes (m) & Center of Inversion (i) Mechanics
05:26 - Rotoinversion Axes (1-bar, 2-bar, 3-bar, 4-bar, 6-bar Equivalences)
07:24 - Crystallographic Reference Axes (a, b, c & Hexagonal 4-Axis Convention)
08:35 - Overview of the 6 Crystal Systems (Classification Criteria)
09:08 - 1. Triclinic & 2. Monoclinic Crystal Systems
11:01 - 3. Orthorhombic & 4. Tetragonal Crystal Systems
12:38 - 5. Hexagonal (incl. Trigonal Division) & 6. Isometric (Cubic) Systems
17:48 - Analytical Challenge Questions (Self-Assessment)
17:59 - Detailed Step-by-Step Answer Keys
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🔑 KEY TERMS & CONCEPTS:
Crystallography: Scientific study of crystal form, external symmetry, and 3D internal atomic arrangements.
Symmetry: Pattern uniformity where an object is brought into self-coincidence via rotation, reflection, or inversion.
Rotation Axes (n-fold): Axis about which a crystal rotates by 360°/n to repeat (1, 2, 3, 4, 6-fold permitted).
5-Fold Axis Prohibition: Regular pentagons cannot tile 3D space periodically without leaving empty voids.
Mirror Plane (m): Imaginary plane dividing a crystal into exact reflection halves across a boundary.
Center of Inversion (i): Internal central point in centrosymmetric crystals where (x,y,z) is related to (-x,-y,-z).
Rotoinversion Axes (n-bar): Compound operation combining rotation (360°/n) followed by point inversion.
Isometric (Cubic) System: a1 = a2 = a3, α = β = γ = 90°; diagnostic symmetry = 4 three-fold triad axes.
Tetragonal System: a = b ≠ c, α = β = γ = 90°; diagnostic symmetry = 1 four-fold tetrad axis parallel to c.
Orthorhombic System: a ≠ b ≠ c, α = β = γ = 90°; diagnostic symmetry = 3 perpendicular two-fold axes or 3 m.
Hexagonal System: a1 = a2 = a3 ≠ c, α = β = 90°, γ = 120°; 4-axis convention; 1 six-fold or 3-fold axis.
Monoclinic System: a ≠ b ≠ c, α = γ = 90°, β greater than 90°; diagnostic symmetry = 1 two-fold axis or 1 mirror plane.
Triclinic System: a ≠ b ≠ c, α ≠ β ≠ γ ≠ 90°; lowest symmetry system (possesses only 1-fold or 1-bar center).
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📖 ACADEMIC REFERENCES & SOURCES:
1. Klein, C., & Dutrow, B. (2007). The 23rd Edition of the Manual of Mineral Science (after James D. Dana). John Wiley & Sons, Inc. [Chapter 6: Crystallography, pp. 136-168].
2. Nesse, W. D. (2011). Introduction to Mineralogy (2nd ed.). Oxford University Press. [Chapter 6: Crystallography].
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🌐 RECOMMENDED DIGITAL STUDY RESOURCES:
Mindat.org Open Data Portal: https://www.mindat.org (Global database featuring 6,000+ mineral species, point groups & photos)
Webmineral Database: http://www.webmineral.com (Crystallography 3D Java/HTML5 applets & Dana taxonomy)
Crystallography Open Database (COD): http://www.crystallography.net (Open-access database of downloadable 3D CIF files)
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