Detrital Sedimentary Rocks Flashcards
what are the 4 main possible components of detrital sedimentary rocks
- mineral grains
- lithic fragments
- biogenic material
- chemical precipitates
what are the 3 primary clast sizes
- gravel
- sand
- mud
rocks with gravel-sized clasts
gravelstones/rudite
gravelstones made of rounded sediments
conglomerate
gravelstones made of angular sediments
breccia
gravelstones that eroded and lithified in place, making the clasts’ and matrices’ composition uniform
intraformational
gravelstones with clasts or matrices derived from outside the depositional area, making the clasts’ and matrices’ composition varied
extraformational
clast-supported conglomerates
orthoconglomerate
matrix-supported conglomerates
paraconglomerate
gravelstones with more than 90% of the framework clasts consisting of a single or few resistant rocks or minerals
oligomict
gravelstones with clasts of various compositions that are prone to weathering
petromict
gravelstones with clasts of a single composition
monomictic
gravelstones with clasts composed of about 2-4 different types
diamictic
gravelstones with clasts of numerous types
polymictic
gravelstone composed of lithified colluvium deposited from mass wasting
diamictite
rocks with sand sized clasts
sandstone/arenite
diagram that classifies sandstone on percentages of quartz, feldspar, and lithic fragments
Pettijohn Sandstone Classification
sandstones with significant amount of feldspar
arkose
sandstones with significant amount of mud matrix
wacke
older, general term for matrix rich sandstone
graywacke
3 sediment settings
- magmatic arc source
- recycled orogen source
- continental block source
sediments derived from volcanic-magmatic arcs formed over subduction zones along convergent plate boundaries
magmatic arc-source
contains sedimentary rocks, metamorphic rocks, and recycled volcanic-magmatic arc sediments derived from uplifted recycled accretionary complexes
subduction complexes
contains sedimentary and metamorphic rocks of both continental, and oceanic origin, uplifted during the continental collisions that close ocean basins
collision orogens