Fossils are generally preserved in sedimentary rocks because deposition and low-temperature burial allow fossilization, whereas igneous rocks destroy remains through high-temperature magma and metamorphic rocks alter or obliterate fossils due to heat and pressure.
Related Articles
THE REPETITION THEORY
Crystallography is fundamentally based on periodic atomic repetition governed by symmetry elements—translation, rotation, reflection, inversion, and their combinations—which determine crystal structures and their 1D, 2D, and 3D patterns.
Read More
CRYSTALLOGRAPHIC SYMMETRY ELEMENTS
Crystallographic symmetry elements—zones and zone axes, center of symmetry (i), mirror planes (m), and rotation axes (n)—describe the geometric regularity of crystals and are fundamental for classifying crystal systems.
Read More
CRYSTALLOGRAPHIC PROJECTION
Crystallographic projection converts a crystal’s 3D form into 2D representations—through spherical, gnomonic, orthographic, and especially stereographic projections—to analyze crystal face orientation and symmetry.
Read More