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Mesozoic EraMesozoic Era
GeologyGeology
Phanerozoic EonPhanerozoic EonMesozoic EraMesozoic Era
• 3 periods3 periods• Age of ReptilesAge of Reptiles
– TriassicTriassic– JurassicJurassic– CretaceousCretaceous
MesozoicMesozoicOverviewOverview
• GlobalGlobal– Breakup of PangaeaBreakup of Pangaea
• North AmericaNorth America– CordilleranCordilleran
– Eastern Coastal RegionEastern Coastal Region
Subduction zone after N.A. Subduction zone after N.A. moves westmoves west
Cordilleran OrogenyCordilleran Orogeny
Fault block mountainsFault block mountains
MesozoicMesozoicPangaea BreakupPangaea Breakup
• Greatly influenced geology/biology/climateGreatly influenced geology/biology/climate
• Fracturing of continentsFracturing of continents
i.e. S. Africa Rifti.e. S. Africa Rift
– Associated with extensionAssociated with extension
– Triple junctionTriple junction
Mantle plume = bulgeMantle plume = bulge
2 arms join in fracturing2 arms join in fracturing
33rdrd failed arm = aulacogen failed arm = aulacogen
(Niger, Miss, Amazon)(Niger, Miss, Amazon)
Continental Drift Continental Drift Geographic FitGeographic Fit
• Continents seem to fit together like pieces of a puzzleContinents seem to fit together like pieces of a puzzle
Mesozoic PaleogeographyMesozoic PaleogeographyTriassicTriassic
• Laurasia and Gondwana Laurasia and Gondwana (L. Tr)(L. Tr)– N. America from S. America and Africa (L. Tr-E. Jr)N. America from S. America and Africa (L. Tr-E. Jr)– Tethys to AtlanticTethys to Atlantic
– Note location along equatorNote location along equator
Mesozoic PaleogeographyMesozoic PaleogeographyJurassicJurassic
• Fragmentation of Gondwana Fragmentation of Gondwana (L. Tr & Jr)(L. Tr & Jr)
– Antarctica and Australia break off (L. Tr)Antarctica and Australia break off (L. Tr)
– India splits and moves northIndia splits and moves north
Pangaea RiftingPangaea RiftingJurassicJurassic
• Thick evaporitesThick evaporites
Mesozoic PaleogeographyMesozoic PaleogeographyCretaceousCretaceous
• S. America from Africa S. America from Africa (begin L. Jr)(begin L. Jr)– E. Tethys closes; Mediterranean prototype formsE. Tethys closes; Mediterranean prototype forms
– Australia and Antarctica separate (end of K)Australia and Antarctica separate (end of K)
– India moves northwardIndia moves northward
– K transgressionK transgression
Mesozoic Ocean CirculationMesozoic Ocean CirculationTriassic to CretaceousTriassic to Cretaceous
• Evolution of oceanic circulationEvolution of oceanic circulation– Simple pattern in a single oceanSimple pattern in a single ocean– Complex in newly formed oceansComplex in newly formed oceans
N.A. PaleogeographyN.A. PaleogeographyContinental InteriorContinental Interior
• Mostly above water; no epeiric seasMostly above water; no epeiric seas• See only Zuni (E. Jr-Paleo) & Absaroka See only Zuni (E. Jr-Paleo) & Absaroka
sequencessequences
N.A. PaleogeographyN.A. PaleogeographyEastern Coastal RegionEastern Coastal Region
• Alleghenian orogeny uplifted Alleghenian orogeny uplifted AppalachiansAppalachians
• Erosion = coarse sedimentsErosion = coarse sediments
• Pangaea rifting = fault block Pangaea rifting = fault block basinsbasins
– Newark group (6000m), poorly Newark group (6000m), poorly sorted, non-marine (L. Tr-E. Jr)sorted, non-marine (L. Tr-E. Jr)
– Reptilian footprints Reptilian footprints no dinos no dinos
– Dikes & sills (Palisades)Dikes & sills (Palisades)– After rifting = passive marginAfter rifting = passive margin
Uplifted mtns. planed offUplifted mtns. planed off
– K = Appalachians upliftedK = Appalachians uplifted
N.AN.A. . PaleogeographyPaleogeographyGulf CoastGulf Coast
• N. America and S. America N. America and S. America get evaporites (L. Tr)get evaporites (L. Tr)
• Form salt domes; no Form salt domes; no evaporites (L. Jr)evaporites (L. Jr)
• Transgressive/regressive Transgressive/regressive sea, i.e. shale, LS, sea, i.e. shale, LS, sandstonesandstone
• End of K transgressionsEnd of K transgressions
• K reefs commonK reefs common
Western N.A. PaleographyWestern N.A. Paleography• Permian arc like Japanese arcPermian arc like Japanese arc
– Subduction, get arc and oceanic arc plastered to continentSubduction, get arc and oceanic arc plastered to continent
– Produce Sonoma OrogenyProduce Sonoma Orogeny
– Steep subduction (L. Tr)Steep subduction (L. Tr)
• Oc-Cont convergence, i.e. S. America after orogenyOc-Cont convergence, i.e. S. America after orogeny
– Oc-Cont convergence control Meso and Ceno tectonicsOc-Cont convergence control Meso and Ceno tectonics– Modern Circum-Pacific orogenic system bornModern Circum-Pacific orogenic system born
Western N.A. PaleographyWestern N.A. PaleographyTriassicTriassic
• Shallow – ss-sh-lsShallow – ss-sh-ls• Regression followedRegression followed
– Marginal marine & non-marineMarginal marine & non-marine Red beds (L. Tr)Red beds (L. Tr)
• Moenkopi Moenkopi (L. Tr)(L. Tr)
• ShinarumpShinarump
• Chinle Chinle (U. Tr)(U. Tr)
– MS, tracks-streams, flood plainsMS, tracks-streams, flood plains– Local marine = lsLocal marine = ls
– Unconformably overlies MoenkopiUnconformably overlies Moenkopi– Erosion of exposed AZ, CO, IDErosion of exposed AZ, CO, ID
– Sh, siltst, - petrified forestSh, siltst, - petrified forest– Ash provides silicaAsh provides silica– Amphibians, small dinosAmphibians, small dinos
Western North AmericaWestern North AmericaTectonic EvolutionTectonic Evolution
• 2 opposite-dipping SZ2 opposite-dipping SZ– Franciscan deposition – trench (M.–L. Jr)Franciscan deposition – trench (M.–L. Jr)
– Up to 7000 mUp to 7000 m
– Greywacke, chert, sh, brecciaGreywacke, chert, sh, breccia
– BlueschistBlueschist
Western North AmericaWestern North AmericaFranciscanFranciscan
• Reconstruction of the depositional environment of the Reconstruction of the depositional environment of the Franciscan GroupFranciscan Group
Western North AmericaWestern North AmericaTectonic EvolutionTectonic Evolution
• Great Valley GroupGreat Valley Group
– Shelf and slope depositionShelf and slope deposition
– Forearc basinForearc basin
Western North AmericaWestern North AmericaTectonic EvolutionTectonic Evolution
• Cordilleran OrogenyCordilleran Orogeny– Several phasesSeveral phases Nevada Orogeny – huge batholiths (L. Jr-K)Nevada Orogeny – huge batholiths (L. Jr-K) Sevier Orogeny – Pacific Plate subducted (K)Sevier Orogeny – Pacific Plate subducted (K) Laramid Orogeny – anticlines & dunes (L. K)Laramid Orogeny – anticlines & dunes (L. K)
Western N.AmericaWestern N.AmericaCause of MigrationCause of Migration
• As subducting plate moved at a lower angle, the As subducting plate moved at a lower angle, the depth of melting moved to eastdepth of melting moved to east
Western N.A. PaleogeographyWestern N.A. PaleogeographyJurassic &Jurassic & CretaceousCretaceous
Jurassic Navajo SS, ZionJurassic Navajo SS, Zion
• Clean, x-bedded SS Clean, x-bedded SS (M. Jr)(M. Jr)
• Nevadan orogenyNevadan orogeny
• Cretaceous interior Cretaceous interior seawayseaway
– Marine, Sundance Sea Marine, Sundance Sea
– Stream, lake depositsStream, lake deposits
– Ms, sh = MorrisonMs, sh = Morrison
– Dinos (Jr)Dinos (Jr)
– Big inland sea – Gulf to Arctic Big inland sea – Gulf to Arctic
– Accelerated spreading Accelerated spreading
Western North AmericaWestern North AmericaMicroplatesMicroplates
• >25% from accretion of microplates>25% from accretion of microplates
– Material added to continentsMaterial added to continents
– Different in fossils, stratigraphy, structure, Different in fossils, stratigraphy, structure, paleomagnetismpaleomagnetism
– Formed elsewhere, transported along faultsFormed elsewhere, transported along faults