Chapter 3: Day 6: Rock Processing Flashcards
Lithification
Processes by which sediments are transformed into sedimentary rocks
Compaction
Increased pressure from overlying sediment
Cementation
Binding together of sediments. By Calcite, Silica, and Iron Oxide
Fossils
Traces or remains of prehistoric life. Are the most important inclusions. Help determine past environments. Used as time indicators. Used for matching rocks from different places
New Rock From Old
. Form from preexisting igneous, sedimentary, or metamorphic rocks
. Take place due to temperatures and pressures unlike those in which it formed
. Leads to changes in mineralogy, texture, and chemical composition
. Often progresses incrementally
What are 3 Degrees of Metamorphism?
. Exhibited by rock texture and mineralogy
. Low-grade, slight changes (e.g., shale becomes slate)
. High-grade, obliteration of original features (e.g., shale becomes gneiss)
What are 4 Metamorphic Agents?
. Heat
. Pressure (stress)
. Confining pressure—from burial
. Differential stress—occurs during mountain building
Chemically active fluids
. Mainly water and other volatiles
. Promote recrystallization by enhancing ion migration
Foliation Texture
. Flat arrangement of mineral grains or structures
. Minerals are perpendicular to the compressional force/force of being squeezed in together
. Is formed where metamorphic rocks has differential stress that squeezes the rock together.
What are 4 Common Solutions of Foliation
slate, phyllite, schist, gneiss
Nonfoliated texture
. Contain equidimensional crystals
. Resembles a coarse-grained igneous rock
What are 2 Common Solutions of Nonfoliated texture
quartzite, marble
Metallic Mineral Resources
Produced by Igneous and Metamorphic processes. Most important ore deposits are generated from hydrothermal (hot-water) solutions
Examples of Metallic Mineral Resources
Gold, silver, copper, mercury, lead, etc.
Pegmatites
. Form fluid-rich environment, have unusually large crystals
. Vein deposits in fractures or bedding planes
. Disseminated deposits that are distributed throughout the rock