IX. Paleozoic World
A. Cratonic sequences - large scale lithostratigraphic unit representing a major
transgressive-regressive sequence bounded by cratonwide unconformities (fig. 21.5)
- basics
- transgression
- regression
- unconformity
- Sauk sequence (latest pC - early Ordovician)
- overlies "Great Nonconformity"
- Transcontinental Arch (fig. 21.6)
- Tippecanoe sequence (mid-Ordovician - early Dev)
- very high sea level
- first well developed reefs
- Michigan Basin
(fig. 21.9 & 21.10 & 21.11)
- barrier reefs
- evaporite minerals
- Kaskaskia sequence (late Dev. - early Miss.)
- black shale
(fig. 21.15)
- carbonates
- Absaroka (late Miss - early Jurassic?)
- cyclothems
- coal
(fig. 21.19)
- reefs and evaporites
B. Tectonics - mobile belts and orogenies
- Amalgamation of Pangaea - closing of Iapetus Ocean
- Taconic - (fig. 21.26) - not a real collision event
- sudbduction zone
- mid-Ord
- Taconic highlands/Queenston Delta
- Caledonian (European name)
- Baltica and Laurentia collide to form Laurasia
- Ordovician -early Dev
(fig. 21.25)
- Old Red Sandstone
- Acadian orogeny (fig. 21.27) (American name)
- Baltica and Laurentia collide
- Devonian
- collision - Laurasia
- Hercynian-Alleghenian
- collision of Gondwana to eastern Laurasia
- Miss-Perm
- southern Appalachians (ancestral Alps)
- Ouachita-Marathon (fig. 21.29) - rotation of Gondwana
- Uralian
- collision of Siberia and Kazakhstania
- Permian
- final step in amalgamation of Pangaea
- Pangaea - Panthalassa
- Cordillera - western N. America
- Antler orogeny (fig. 21.28)
- Devonian
- accrete Klamath island arc
- ancestral Rockies
- Pennsylvanian
- high angle faults
- Sonoma orogeny
- Permian-Triassic
- another island arc
Go back to Geology page