Sedimentary Rocks and Diagenesis Flashcards
(5 cards)
Laminated siltstone vs bedded siltstone
mudstone vs shale
Laminated siltstone
laminae <10mm thick
Bedded siltstone:
beds are >10mm thick
Mudstone:
clay content is between 33-65%
Shale: Laminated and clay content is >65%
Type, composition, origin of conglomerates and diamictites
Quartzose (Oligomict) conglomerates
* Derived from rocks containing quartzite beds, or quartz veins, or chert beds
* Common
* thin layers in sandstone units
* Most fluvial in origin (braided streams)
* some littoral (beach) environment
Polymict, petromict conglomerates, and diamictites
* Various lithologies; petromict contain metastable clasts
* May reach great thicknesses (thousands of meters)
* Rapid erosion of highlands
* Sediment gravity-flow processes
* Glacial deposits
Intraformational conglomerates
* Clasts from within the depositional basin
* Deformation structures, fragments of deformed sediments (e.g. mud and lime clasts)
* Sediment rip-ups by tidal currents, storms, etc.
Siliciclastic rocks
Siliciclastic sediments are classified according to grain size and composition
- Terrigenous particles; minerals, rock fragments (may incl. minor bioclast particles)
Conglomerates and diamictites: - Epiclastic conglomerates/diamictites -> Extraformational & Intraformational
- Clast-supported -> Conglomerates, orthoconglomerates
- Matrix-supported -> paraconglomerates and diamictites
- Further subdivision: Clast stability, Clast lithology:
>90 supported clasts:
clast supported = quartzose conglomerate
matrix supported = quartzose diamictite
<90 supported clasts:
clast supported = petromict conglomerate
matrix supported = petromict diamictite
breccias - Cataclastic breccia (landslide or slump, tectonic, collapse)
- Solution breccia (remaining insoluble fragments)
, sandstones, wackes, mudrocks: laminated siltstone, bedded mudstone
*Carbonate rocks
- Limestones, dolostones, reef rocks
- Carbonate particles; framework grains, matrix
Carbonate rocks
- Limestones
Main types of sediment particles: - Gravel size
-(Large skeletal particles, Extraclasts, Intraclasts) - Sand-sized particles
-(Skeletal particles, Fragments of calcareous algae, Ooids, Pellets) - Mud-sized particles (carbonate oozes)
-Coccolithophores, Foraminifers, Other mud-sized skeletal fragments, Mud-sized “extraclasts’,Micrite - Other types (framework carbonates)
- Stromatolites, Reef rocks, Dolostones
- Form largely by replacement of limestone precursor
‘ - Dolostones
-Form largely by replacement of limestone precursor
Diagenesis
Three main stages
* Shallow, deep burial, uplift/erosion (back to surface)
* Different types of cement and textures
* May record complex diagenetic history (precipitation/dissolution and temporal changes)