To determine which portion of the spherical projection is used in crystallographic analysis, we examine standard mineralogical practice.
1. Understanding Spherical Projections in Crystallography:
Stereographic projections are fundamental tools for representing 3D crystallographic orientations on a 2D plane.
2. Standard Practice:
Mineralogists typically use the top half (upper hemisphere) of the spherical projection for routine crystallographic analysis because:
3. Key Reasons:
- The upper hemisphere projection is sufficient for most symmetry operations
- Crystal faces in the lower hemisphere can be represented as equivalent upper hemisphere positions
- Simplifies interpretation while maintaining all essential crystallographic information
- Follows the conventional Wulff net projection method used in most crystallographic studies
4. Projection Methodology:
- Upper hemisphere (top half) plotted as solid circles
- Lower hemisphere points are projected through the sphere's center to appear in the upper hemisphere
- Standard stereographic projections in mineralogy textbooks primarily show upper hemisphere
5. When Full Sphere is Used:
The complete spherical projection is only needed for:
- Specialized studies of antisymmetry
- Certain twinning relationships
- Complete Laue symmetry analysis
6. Practical Applications:
- Determining crystal symmetry classes
- Analyzing face orientations
- Studying zone axis relationships
- Routine interfacial angle measurements
Conclusion:
For standard crystallographic analysis, mineralogists primarily use the top half of the spherical projection.
Final Answer:
The correct option is: top half.