Assessing volcanic origins within detrital zircon populations——A case study from the Mesozoic non-volcanic margin of southern Australia
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摘要
Detrital zircon U/Pb geochronology is a common tool used to resolve stratigraphic questions,inform basin evolution and constrain regional geological histories.In favourable circumstances,detrital zircon populations can contain a concomitant volcanic contribution that provides constraints on the age of deposition.However,for non-volcanic settings,proving isolated detrital zircon grains are from contemporaneous and potentially remote volcanism is challenging.Here we use same grain(U-Th)/He thermochronology coupled with U/Pb geochronology to identify detrital zircon grains of contemporary volcanic origin.(U-Th)/He ages from Cretaceous zircon grains in southern Australia define a single population with a weighted mean age of 104±6.1 Ma.indistinguishable from zircon U/Pb geochronology and palynology(～104.0-107.5 Ma).Detrital zircon trace-element geochemistry is consistent with a continental signature for parent rocks and coupled with detrital grain ages,supports derivation from a>2000 km distant early-to mid-Cretaceous Whitsunday Volcanic Province in eastern Australia.Thus,integration of biostratigraphy,single-grain zircon double-dating(geochronology and thermochronology)and grain geochemistry enhances fingerprinting of zircon source region and transport history.A distal volcanic source and rapid continental-scale transport to southern Australia is supported here.
Detrital zircon U/Pb geochronology is a common tool used to resolve stratigraphic questions,inform basin evolution and constrain regional geological histories.In favourable circumstances,detrital zircon populations can contain a concomitant volcanic contribution that provides constraints on the age of deposition.However,for non-volcanic settings,proving isolated detrital zircon grains are from contemporaneous and potentially remote volcanism is challenging.Here we use same grain(U-Th)/He thermochronology coupled with U/Pb geochronology to identify detrital zircon grains of contemporary volcanic origin.(U-Th)/He ages from Cretaceous zircon grains in southern Australia define a single population with a weighted mean age of 104±6.1 Ma.indistinguishable from zircon U/Pb geochronology and palynology(～104.0-107.5 Ma).Detrital zircon trace-element geochemistry is consistent with a continental signature for parent rocks and coupled with detrital grain ages,supports derivation from a>2000 km distant early-to mid-Cretaceous Whitsunday Volcanic Province in eastern Australia.Thus,integration of biostratigraphy,single-grain zircon double-dating(geochronology and thermochronology)and grain geochemistry enhances fingerprinting of zircon source region and transport history.A distal volcanic source and rapid continental-scale transport to southern Australia is supported here.
Detrital zircon U/Pb geochronology is a common tool used to resolve stratigraphic questions,inform basin evolution and constrain regional geological histories.In favourable circumstances,detrital zircon populations can contain a concomitant volcanic contribution that provides constraints on the age of deposition.However,for non-volcanic settings,proving isolated detrital zircon grains are from contemporaneous and potentially remote volcanism is challenging.Here we use same grain(U-Th)/He thermochronology coupled with U/Pb geochronology to identify detrital zircon grains of contemporary volcanic origin.(U-Th)/He ages from Cretaceous zircon grains in southern Australia define a single population with a weighted mean age of 104±6.1 Ma.indistinguishable from zircon U/Pb geochronology and palynology(～104.0-107.5 Ma).Detrital zircon trace-element geochemistry is consistent with a continental signature for parent rocks and coupled with detrital grain ages,supports derivation from a>2000 km distant early-to mid-Cretaceous Whitsunday Volcanic Province in eastern Australia.Thus,integration of biostratigraphy,single-grain zircon double-dating(geochronology and thermochronology)and grain geochemistry enhances fingerprinting of zircon source region and transport history.A distal volcanic source and rapid continental-scale transport to southern Australia is supported here.
引文
Barham,M.,Kirkland,C.L,Reynolds,S.,O'Leary,M.J.,Evans,N.J.,Allen,H.,Haines.P.W.,Hocking,R.M.,McDonald,B.J.,Belousova,E.,Goodall,J.,2016.The answers are blowin'in the wind:ultra-distal ashfall zircons,indicators of Cretaceous super-eruptions in eastern Gondwana.Geology 44,643-646.
Barham,M.,Reynolds,S.,Kirkland,C.I.,O'Leary,M.J.,Evans,N.J.,Allen,H.J.,Haines,P.W.,Hocking,R.M.,McDonald,B.J.,2018.Sediment routing and basin evolution in Proterozoic to Mesozoic east Gondwana:a case study from southern Australia.Gondwana Research 58,122-140.
Belousova,E.,Griffin,W.,O'Reilly.S.Y.,Fisher,N.,2002.Igneous zircon:trace element composition as an indicator of source rock type.Contributions to Mineralogy and Petrology 143,602-622.
Blakey,R.C.,2008.Gondwana palcogcography from assembly to breakup—A 500m.y.odyssey.In:Fielding,C.R.,Frank.T.D.,Isbell,J.L.(Eds.),Resolving the Late Paleozoic Ice Age in Time and Space.The Geological Society of America,Special Paper 441,Boulder,Colorado,pp.1-28.
Blevin,J.E.,Cathro,D.L,2008.Australian Southern Margin Synthesis,Project GA707,pp.1-104.
Blundy,J.,Wood.B.,1994.Prediction of crystal-melt partition coefficients from elastic moduli.Nature 372,452.
Boynton,W.V.,1984.Chapter 3-cosmochemistry of the rare Earth elements:meteorite studies.In:Henderson,P.(Ed.),Developments in Geochemistry.Elsevier,pp.63-1 14.
Bryan,S.E.,Constantine.A.E.,Stephens,C.J.,Ewart,A.,Schon.R.W.,Parianos,J.,1997.Early Cre taceous volcano-sedimentary successions along the eastern Australian continental margin:implications for the break-up of eastern Gondwana.Earth and Planetary Science Letters 153,85-102.
Bryan,S.E.,Cook,A.G.,Allen,C.M.,Siegel,C.,Purdy,D.J.,Greentree,J.S.,Uysal,I.T.,2012.Early-mid cretaceous tectonic evolution of eastern Gondwana:from silicic LIP magmatism to continental rupture.Episodes 35,142-152.
Bryan,S.E.,Ewart,A.,Stephens,C.J.,Parianos,J.,Downes,P.J.,2000.The Whitsunday Volcanic Province,Central Queensland,Australia:lithological and stratigraphic investigations of a silicic-dominated large igneous province.Journal of Volcanology and Geothermal Research 99,55-78.
Bryan,S.E.,Peate,I.U.,Peate,D.W.,Self,S.,Jerram,D.A.,Mawby,M.R.,Marsh,J.S.,Miller,J.A.,2010.The largest volcanic eruptions on Earth.Earth Science Reviews102.207-229.
Buret,Y.,von Quadt,A.,Heinrich,C.,Selby,D.,Walle,M.,Peytcheva,I.,2016.From a long-lived upper-crustal magma chamber to rapid porphyry copper emplacement:reading the geochemistry of zircon crystals at Bajo de la Alumbrera(NW Argentina).Earth and Planetary Science Letters 450,120-131.
Burgess,S.D.,Bowring,S.A,Fleming,T.H.,Elliot,D.H.,2015.High-precision geochronology links the Ferrar large igneous province with early-Jurassic ocean anoxia and biotic crisis.Earth and Planetary Science Letters 415.90-99.
Campbell,I.H.,Reiners,P.W.,Allen,C.M.,Nicolescu,S.,Upadhyay,R.,2005.He-Pb double dating of detrital zircons from the Ganges and Indus Rivers:implication for quantifying sediment recycling and provenance studies.Earth and Planetary Science Letters 237,402-432.
Cawood,P.A.,Hawkesworth,C.J.,Dhuime,B.,2012.Detrital zircon record and tectonic setting.Geology 40,875-878.
Cawood,P.A.Nemchin.A.A.,Freeman,M.,Sircombe,K.,2003.Linking source and sedimentary basin:detrital zircon record of sediment flux along a modern river system and implications for provenance studies.Earth and Planetary Science Letters 210,259-268.
Cecil,M.R.,Ducea,M.N.,Reiners,P.,Gehrels,G.,Mulch,A.,Allen,C.,Campbell,1.,2010.Provenance of Eocene river sediments from the central northern Sierra Nevada and implications for paleotopography.Tectonics 29,TC6010.https://doi.org/10.1029/2010TC002717.
Chapman,J.B.,Gehrels,G.E.,Ducea,M.N.,Giesler,N.,Pullen.A.,2016.A new method for estimating parent rock trace element concentrations from zircon.Chemical Geology 439,59-70.
Constantine,A.E.,2001.Sedimentology,Stratigraphy and Palacoenvironment of the Upper Jurassic-Lower Cretaceous Non-marine Strzelecki Group,Gippsland Basin,Southeastern Australia.Department of Earth Sciences.Monash University,Melbourne,Australia.
Corfu,F.,Hanchar,J.M.,Hoskin,P.W.O.,Kinny,P.,2003.Atlas of zircon textures.Reviews in Mineralogy and Geochemistry 53,469.
Danisik,M.,Stepancíkova,P.,Evans,N.J.,2012.Constraining long-term denudation and faulting history in intraplate regions by multisystem thcrmochronology:an example of the Sudetic Marginal Fault(Bohemian Massif,central Europe).Tectonics 31.
Dickinson,W.R.,Gehrels,G.E.,2009.Use of U-Pb ages of detrital zircons to infer maximum depositional ages of strata:a test against a Colorado Plateau Mesozoic database.Earth and Planetary Science Letters 288,115-125.
Dickinson,W.R.,Gehrels,G.E.,2010.Insights into north American paleogeography and paleotectonics from U-Pb ages of detrital zircons in Mesozoic strata of the Colorado plateau,USA.International Journal of Earth Sciences 99,1247-1265.
Direen,N.G.,Borissova,I.,Stagg,H.MJ.,Colwell,J.B.,Symonds,P.A.,2007.Nature of the continent-ocean transition zone along the southern Australian continental margin:a comparison of the Naturaliste Plateau,SW Australia,and the central Great Australian Bight sectors.Geological Society London Special Publications282,239-263.
Direen,N.G.,Stagg.H.MJ.,Symonds,P.A.,Colwell,J.B.,2008.Architecture of volcanic rifted margins:new insights from the Exmouth-gascoyne margin,Western Australia.Australian Journal of Earth Sciences 55,341-363.
Direen,N.G.,Stagg.H.M.J.,Symonds,P.A.,Colwell,J.B.,2011.Dominant symmetry of a conjugate southern Australian and East Antarctic magma-poor rifted margin segment.Geochemistry,Geophysics,Geosystems 12,Q02006.https://doi.org/10.1029/2010GC003306.
Duddy,I.R.,2003.Mesozoic.In:Birch,W.D.(Ed.),Geology of Victoria.Geological Society of Australia Special Publication,vol.23,pp.239-289.
Duddy,I.R.,2016.Gondwana-wide thermotectonic events and their expression in southern and south-eastern Australia before and after break-up:denudation,volcanism,sedimentation and provenance.In:Gross er,M.(Ed.), 2016 Selwyn Symposium.Supercontinents Assembly through Break-Up:An eastern Gondwana Perspective.The Geological Society of Australia-Victoria Division.The University of Melbourne,pp.39-41.
Ewart,A.,Schon,R.W.,Chappell,B.W.,1992.The Cretaceous volcanic-plutonic province of the central Queensland(Australia)coast—a rift related'calc-alkaline'province.Earth and Environmental Science Transactions of the Royal Society of Edinburgh 83,327-345.
Farley,KA,Wolf,R.A.,Silver,L.T.,1996.The effects of long alpha-stopping distances on(U-Th)/He ages.Geochimica et Cosmochimica Acta 60,4223-4229.
Fedo,C.M.,Sircombe,K.N.,Rainbird,R.H.,2003.Detrital zircon analysis of the sedimentary record.Reviews in Mineralogy and Geodiemistry 53,277-303.
Felton,E.A.,1992.Sedimentary History of the Early Cretaceous Otway Group,Otway Basin.Department of Geology.The University of Wollongong.Australia.
Fielding,L,Najman,Y.,Millar,I.,Butterworth,P.,Ando,S.,Padoan,M.,Barfod,D.,Kneller.,B.,201 7.A detrital record of the Nile River and its catchment Journal of the Geological Society 174,301-317.
Fisher,R.V.,1961.Proposed classification of volcaniclastic sediments and rocks.GSA Bulletin 72,1409-1414.
Fisher,R.V.,Schmincke,H.-U.,1984.Pyroclastic Rocks.Spinger-Verlag,Berlin.
Gagnevin,D.,Daly,J.S.,Kronz,A.,2010.Zircon texture and chemical composition as a guide to magmatic processes and mixing in a granitic environment and coeval volcanic system.Contributions to Mineralogy and Petrology 159,579-596.
Galbraith,RF.,1988.Graphical display of estimates having differing standard errors.Technometrics 30,271-281.
Galbraith,R.F.,1990.The radial plot:graphical assessment of spread in ages.International Journal of Radiation Applications and Instrumentation Part D Nuclear Tracks and Radiation Measurements 17,207-214.
Gallagher,K.,Dumitru,TA.,Gleadow,A.J.W.,1994.Constraints on the vertical motion of eastern Australia during the Mesozoic Basin Research 6,77-94.
Gallagher,K.,Lambeck,K.,1989.Subsidence,sedimentation and sea-level changes in the Eromanga Basin,Australia.Basin Research 2,115-131.
Gehrels,G.,2014.Detrital zircon U-Pb geochronology applied to tectonics.Annual Review of Earth and Planetary Sciences 42,127-149.
Geoscience Australia,2018.Otway Basin.Geoscience Australia.
Geoscience Australia and the Australian Stratigraphy Commission,2018.Australian Stratigraphic Units Database.Geoscience Australia and Australian Stratigraphy Commission.
Gibbons,A.D.,Whittaker,J.M.,M(u|¨)ller,R.D.,2013.The breakup of East Gondwana:assimilating constraints from Cre taceous ocean basins around India into a bestfit tectonic model.Journal of Geophysical Research Solid Earth 118,808-822.
Gleadow,A.J.W.,Duddy,I.R.,1981.Early Cretaceous volcanism and the early breakup history of southeastern Australia:evidence from fission track dating of volcaniclastic sediments.In:Gondwana Five:Selected Papers and Abstracts,fifth Gondwana symposium,pp.295-300.
Gradstein,F.M.,Ogg,J.G.,Schmitz,M.,Ogg,G.,2012.The Geologic Time Scale 2012.Elsevier,Amsterdam,the Netherlands.
Greentree,J.,2011.Palaeoenvironmental Setting of Dinosaur Trackways in the Context of the Closing Stages of Eromanga Basin Evolution.Queensland University of Technology,Brisbane,Australia,p.107.
Grey,K.,Hocking,R.H.,Stevens,M.K.,Bagas,L.,Carlsen,G.M.,Irimies,F.,Pirajno,F.,Haines,P.W.,Apak,S.N.,200.5.Lithostratigraphic Nomenclature of the Officer Basin and Correlative Parts of the Paterson Orogen,Western Australia.
Grimes,C.B.,John.B.E.,Kelemen,P.B.,Mazdab,F.K.,Wooden,J.L.,Cheadle,M.J.,Hangh(?)j,K.,Schwartz,J.J.,2007.Trace element chemistry of zircons from oceanic crust:a method for distinguishing detrital zircon provenance.Geology35,643-646.
Grimes,C.B.,Wooden,J.L,Cheadle,M.J.,John,B.E.,2015."Fingerprinting"tectonomagmatic provenance using trace elements in igneous zircon.Contributions to Mineralogy and Petrology 170,1-26.
Guenthner,W.R.,Reiners,P.W.,Ketcham,R.A.,Nasdala,L.,Giester,G.,2013.Helium diffu sion in natural zircon:radiation damage,anisotropy,and the interpretation of zircon(U-Th)/He thermochronology.American Journal of Science 313,145-198.
Haq,B.U.,2014.Cretaceous eustasy revisited.Global and Planetary Change 113,44-58.
Heiken.,G.,1985.Volcanic Ash.University of California Press,Los Alamos,USA.
Helby,R.,Morgan,R.,Partridge,A.D.,1987.A palynological zonation of the Australian Mesozoic.In:Jell,P.A.(Ed.),Studies in Australian Mesozoic Palynology.Memoir Association Australasian Palaeontologists,pp.1-94.
Hopkinson,T.N.,Harris,N.B.W.,Warren,C.J.,Spencer,C.J.,Roberts,N.M.W.,Horstwood,M.S.A.,Parrish,R.R.,Eimf,2017.The identification and significance of pure sediment-derived granites.Earth and Planetary Science Letters 467,57-63.
Hou,B.,Keeling.J.,Reid,A.,Fairclough,M.,Wairland,I.,Belousova,E.,Frakes,L.,Hocking,R.,2011.Heavy mineral sands in the Eucla Basin,Southern Australia:depositional and province-scale prospectivity.Economic Geology 106,687-712.
Ito,H.,Spencer,C.J.,Danisik,M.,Hoiland,C.W.,2017.Magmatic tempo of Earth's youngest exposed plutons as revealed by detrital zircon U-Pb geochronology.Scientific Reports 7.12457.
Kaczmarek,M.-A.,Miintener,O.,Rubatto,D.,2008.Trace element chemistry and U-Pb dating of zircons from oceanic gabbros and their relationship with whole rock composition(Lanzo,Italian Alps).Contributions to Mineralogy and Petrology 155,295-312.
Kirkland,C.I.,Daly,J.S.,Whitehouse,M.J.,2007.Provenance and terrane evolution of the kalak nappe complex,Norwegian caledonides:implications for neoproterozoic paleogeography and tectonics.The Journal of Geology 115,21-41.
Kirkland,C.L,Smithies,R.H.,Spaggiari,C.V.,Wingate,M.T.D.,Quentin de Gromard,R.,Clark,C.,Gardiner.N.J.,Belousova,E.A.,2017.Proterozoic crustal evolution of the Eucla basement,Australia:implications for destruction of oceanic crust during emergence of Nuna.Lithos 278-281,427-444.
Laurie,J.R.,Bodorkos,S., Nicoll,R.S.,Crowley,J.L.,Mantle,D.J.,Mory,A.J.,Wood,G.R.,Backhouse,J.,Holmes,E.K.,Smith,T.E.,Champion,D.C.,2016.Calibrating themiddle and late Permian palynostratigraphy of Australia to the geologic timescale via U-Pb zircon CA-IDTIMS dating.Australian Journal of Earth Sciences63,701-730.
Lissenberg,C.J.,Rioux,M.,Shimizu,N.,Bowring,SA.,Mevel,C.,2009.Zircon dating of oceanic crustal accretion.Science 323,1048-1050.
Lloyd,J.,Collins,A.S.,Payne,J.L.,Glorie,S.,Holford,S.,Reid,A.J.,2016.Tracking the Cretaceous transcontinental Ceduna River through Australia:the hafnium isotope record of detrital zircons from offshore southern Australia.Geoscience Frontiers 7,237-244.
Lowry,D.C.,1970.In:Australia,G.S.o.W.(Ed.),Geology of the Western Australian Part of the Eucla Basin.Geological Survey of Western Australia,Perth,p.207.
Ludwig,K.R.,2012.User's manual for isoplot/Ex,v.3.75,A Geochronological Toolkit for Microsoft Excel,vol.5.Berkeley Geochronological Center Special Publications.
MacDonald,J.D.,Holford,S.P.,Green,P.F.,Duddy,I.R.,King.R.C.,Backe,G.,2013.Detrital zircon data reveal the origin of Australia's largest delta system.Journal of the Geological Society 170,3-6.
Makulini,P.,Kirkland,C.L.,Barham,M.,2018.Zircon grain shape holds provenance information;a case study from southwestern Australia.Geological Journal 1-15.
Mami,T.,Kenji,H.,Kenichiro,T.,Takeyoshi,Y.,Tomokazu,H.,Shoichi,K.,2017.Timescale of magma chamber processes revealed by U-Pb ages,trace element contentis and morphology of zircons from the Ishizuchi caldera,Southwest Japan Arc Island Arc 26,e 12182.
Markwitz,V.,Kirkland,C.L.,2018.Source to sink zircon grain shape:constraints on selective preservation and significance for Western Australian Proterozoic basin provenance.Geoscience Frontiers 9,415-430.
Markwitz,V.,Kirkland,C.L,Mehnert,A.,Gessner,K.,Shaw,J.,2017.3-D characterization of detrital zircon grains and its implications for fluvial transport,mixing.and preservation bias.Geochemistry,Geophysics,Geosystems 18,4655-4673.
Matthews,K.J.,Hale,A.J.,Gurnis,M.,Miiller,R.D.,DiCaprio,L,2011.Dynamic subsidence of eastern Australia during the cretaceous.Gondwana Res earch 19,372-383.
McKenzie.N.R.,Smye,A.J.,Hegde,V.S.,Stockli,D.F.,2018.Continental growth histories revealed by detrital zircon trace elements:a case study from India.Geology 46,275-278.
Meeuws,F.J.E.,Holford,S.P.,Foden,J.D.,Schofield,N.,2016.Distribution,chronology and causes of Cretaceous-Cenozoic magmatism along the magma-poor rifted southern Australian margin:Links between mantle melting and basin formation.Marine and Petroleum Geology 73,271-298.
Menzies,M.A., Klemperer,S.L,Ebinger,C.J.,Baker,J.,2002.Characteristics of volcanic rifted margins.In:Menzies,MA.,Klemperer.S.L.,Ebinger,C.J.,Baker,J.(Eds.),Volcanic Rifted Margins.Geological Society of America.
Metcalfe,I.,Crowley,J.L.,Nicoll,R.S.,Schmitz,M.,2015.High-precision U-Pb CATIMS calibration of Middle Permian to Lower Triassic sequences,mass extinction and extreme climate-change in eastern Australian Gondwana.Gondwana Research 28.61-81.
Mihut,D.,Muller,R.D.,1998.Volcanic margin formation and mesozoic rift propagators in the cuvier abyssal plain off western Australia.Journal of Geophysical Research Solid Earth 103,27135-27149.
Mory,A.J.,Crowley,J.L.,Backhouse,J.,Nicoll,RS.,Bryan. S.E.,López Martinez,M.,Mantle,D.J.,2017.Apparent conflicting Roadian-Wordian(middle permian)CA-IDTIMS and palynology ages from the canning basin,western Australia.Australian Journal of Earth Sciences 64,889-901.
M(u|¨)ller,R.D.,Flament,N..Matthews,K.J.,Williams,S.F.,Guris,M.,2016.Formation of Australian continental margin highlands driven by pla te-mantle interaction.Earth and Planetary Science Letters 441,60-70.
M(u|¨)ller,R.D.,Gaina,C.,Clark,S.,2000.Seafloor spreading around Australia.In:Veevers,J.(Ed.),Billion-year Earth History of Australia and Neighbours in Gondwanaland.Gemoc Press.Sydney,Australia,pp.18-28.
Norvick,M.S.,Smith,M.A.,Power,M.R.,2001.The plate tectonic evolution of eastern australasia guided by the stratigraphy of the Gippsland basin.In:Hill,K.C.,Bernecker,T.(Eds.),Eastern Australasian Basins Symposium:A Refocused Energy Perspective for the Future.Petroleum Exploration Society of Australia,Special Publications,Melbourne,pp.15-24.
Olierook,H.K.H.,Barham,M.,Fitzsimons,I.C.W.,Timms,N.E.,Jiang,Q.,Evans,N.J.,McDonald.B.J.,201 9.Tectonic controls on sediment provenance evolution in rift basins:detrital zircon U-Pb and Hf isotope analysis from the Perth Basin.Western Australia.Gondwana Research 66,126-142.
Olierook,H.K.H.,Jourdan,F.,Merle,R.E.,Timms,N.E.,Kusznir,N.,Muhling,J.R.,2016.Bunbury Basalt:Gondwana breakup products or earliest vestiges of the Kerguelen mantle plume?Earth and Planetary Science Letters 440,20-32.
Olierook,H.K.H.,Timms,N.E.,Wellmann,J.F.,Corbel,S.,Wilkes,P.G.,2015.3D structural and stratigraphic model of the Perth Basin,Western Australia:implications for sub-basin evolution.Australian Journal of Earth Sciences 62.447-467.
Partridge,A.D.,2006.Late Cretaceous palynology zonations for Australia.In:Monteil,E.(Ed.),Australian Mesozoic and Cenozoic Palynology ZonationsUpdated to the 2004 Geologic Timescale.Geoscience Australia,p.8.
Pirajno,F.,Hoatson,D.M.,2012.A review of Australia's Large Igneous Provinces and associated mineral systems:implications for mantle dynamics through geological time.Ore Geology Reviews 48,2-54.
Playford,P.E.,Cockbain,A.E.,Low.G.H.,1976.Geology of the Perth Basin,western Australia,vol.124.Geological Survey of Western Australia Bulletin,Perth,Australia.
Pointon,M A.,Chew,D.M.,Ovtcharova,M.,Sevastopulo,G.D.,Crowley,Q.G.,2012.New high-precision U-Pb dates from western European Carboniferous tuffs;implications for time scale calibration,the periodicity of late Carboniferous cycles and stratigraphical correlation.Journal of the Geological Society 169,713-721.
Pointon,M.A.,Chew,D.M.,Ovtcharova.M.,Sevastopulo.,G.D.,Delcambre,B.,2014.High-precision U-Pb zircon CA-ID-TIMS dates from western European late Visean bentonites.Journal of the Geological Society 171,649-658.
Rahl,J.M.,Reiners,P.W.,Campbell,I.H.,Nicolescu,S.,Allen,C.M.,2003.Combined single-grain(U-Th)/He and U/Pb dating of detrital zircons from the Navajo Sandstone,Utah.Geology 3 1,761-764.
Rasmussen,B.,Fletcher,I.R.,2010.Dating sedimentary rocks using in situ U-Pb geochronology of syneruptive zircon in ash-fall tuffs<1 mm thick.Geology 38,299-302.
Reid.A.,Keeling,J.,Boyd,D.,Belousova,E.,Hou,B.,2013.Source of zircon in worldclass heavy mineral placer deposits of the Cenozoic Eucla Basin,southern Australia from LA-ICPMS U-Pb geochronology.Sedimentary Geology 286-287,1-19.
Reiners.,P.W.,Campbell,I.H.,Nicolescu,S.,Allen,C.M.,Hourigan,J.K.,Garver,J.I.,Mattinson,J.M.,Cowan,D.S.,2005.(U-Th)/(He-Pb)double dating of detrital zircons.American Journal of Science 305,259-311.
Reiners,P.W.,Spell,T.L.,Nicolescu,S.,Zanetti,KA.2004.Zircon(U-Th)/He thermochronometry:He diffusion and comparisons with~(40)Ar/~(39)Ar dating.Geochimica et Cosmochimica Acta 68,1857-1887.
Salles,T.,Flament,N.,M(u|¨)ller,D.,2017.Influence of mantle flow on the drainage of eastern Australia since the Jurassic Period.Geochemistry,Geophysics,Geosystems 18,280-305.
Sano,Y.,Tsutsumi,Y.,Terada,K.,Kaneoka,I.,2002.Ion microprobe U-Pb dating of Quaternary zircon:implication for magma cooling and residence time.Journal of Volcanology and Geothermal Research 117,285-296.
Saylor,J.E.,Stockli,D.F.,Horton.B.K.,Nic,J.,Mora,A.,2012.Dis criminating rapid exhumation from syndepositional volcanism using detrital zircon double dating:implications for the tectonic history of the Eastern Cordillera,Colombia.GSA Bulletin 124,762-779.
Schmitz,M.D.,2012.Radiogenic isotope geochronology.In:Gradstein,F.,Ogg,J.G.,Schmitz,M.,Ogg,G.(Eds.),The Geological Timescale.Elsevier,Amsterdam,pp.115-12 7.
Schoene,B.,Condon,D.J.,Morgan,L.,Mclean,N.,2013.Precision and accuracy in geochronology.Elements 9,19-24.
Schofield,A.,Totterdell,J.,2008.Distribution,Timing and Origin of Magmatism in the Bight and Eucla Basins,p.19.
Seton,M.M(u|¨)lle r,R.D.,Zahirovic,S.,Gaina,C.,Torsvik,T.,Shephard,G.,Talsma,A.,Gurnis,M.,Turner,M.,Maus,S.,Chandler,M.,2012.Global continental and ocean basin reconstructions since 200Ma.Earth-Science Reviews 113,212-270.
Sircombe.K.N.,Freeman,M.J.,1999.Provenance of detrital zircons on the Western Australia coastline—implications for the geologic history of the Perth basin and denudation of the Yilgam craton.Geology 27,879-882.
Spencer,CJ.,Cavosie,A.J.,Raub,T.D.,Rollinson,H.,Jeon,H..Searle,M.P.,Miller,J.A.,McDonald,B.J.,Evans,N.J.,The Edinburgh Ion Microprobe Facility,2017.Evidence for melting mud in Earth's mantle from extreme oxygen isotope signatures in zircon.Geology 45,975-978.
Spencer,C.J.,Danisik,M.,Ito,H.,Hoiland,C.,Tapster.S.,Jeon,H.,McDonald,B.,Evans,N.J.,2019.Rapid exhumation of Earth's youngest exposed granites driven by subduction of an oceanic arc Geophysical Research Letters 46.https://doi.org/10.1029/2018GL080579.
Spencer,C.J.,Kirkland,C.L.,Roberts,N.M.W.,2018.Implications of erosion and bedrock composition on zircon fertility:examples from South America and Western Australia.Terra Nova 30,289-295.
Spencer,CJ.,Kirkland,C.L,Taylor,RJ.M.,2016.Strategies towards statistically robust interpretations of in situ U-Pb zircon geochronology.Geoscience Frontiers 7,58 1-589.
Stagg,H.MJ.,Cockshell,C.D.,Willcox,J.B.,Hill,A.J.,Needham,D.J.L.,Thomas,B.,O'Brien,G.W.,Hough,L.P.,1990.Basins of the Great Australian Bight Region:Geology and Petroleum Potential.Bureau of Mineral Resources.Continental Margins Program Folio 5.
Suthren.R.J.,1985.Facies analysis of volcaniclastic sediments:a review.Geological Society,London,Special Publications 18,123-146.
Tosolini,A.-M.P.,Korasidis,V.A.,Wagstaff,B.E.,Cantrill,D.J.,Gallagher,S.J.,Norvick,M.S.,2018.Palaeoenvironments and palaeocommunities from lower cretaceous high-latitude sites,Otway Basin,southeastern Australia.Palaeogeography,Palaeoclimatology,Palaeoecology 496,62-84.
Totterdell,J.M.,Bradshaw,B.E.,2004.The structural framework and tectonic evolution of the Bight Basin.In:Boult,P.J.,Johns,D.R.,Lang,S.C.(Eds.),Eastern Australasian Basins Symposium II.Petroleum Exploration Society of Australia,Special Publication,pp.41-61.
Totterdell.J.M.,Krassay,A.A.,2003.Sequence stratigraphic correlation of onshore and offshore Bight Basin successions.Geoscience Australia Record 2003/02,50 pp.
Trail,D.,Bruce Watson,E.,Tailby,N.D.,2012.Ce and Eu anomalies in zircon as proxies for the oxidation state of magmas.Geochimica et Cosmochimica Acta97,70-87.
Tucker.R.T.,Roberts,E.M.,Henderson,R.A.,Kemp,A.I.S.,2016.Large igneous province or long-lived magmatic arc along the eastern margin of Australia during the Cretaceous? Insights from the sedimentary record.The Geological Society of America Bulletin 128,1461-1480.
Tucker,R.T.,Roberts,F.M.,Hu,Y.,Kemp,A.I.S.,Salisbury,S.W.,2013.Detrital zircon age constraints for the Winton formation,Queensland:contextualizing Australia's late cretaceous dinosaur faunas.Gondwana Research 24.767-779.
Veevers,J.J.,2000.Change of tectono-stratigraphic regime in the Australian plate during the 99 Ma(mid-Cretaceous)and 43 Ma(mid-Eocene)swerves of the Pacific.Geology 28,47-50.
Veevers.J.J.,Belousova,E.A.,Saeed,A.,2016.Zircons traced from the 700-500 Ma transgondwanan supermountains and the gamburtsev subglacial mountains to the ordovician lachlan orogen,cretaceous Ceduna delta,and modem channel country,central-southern Australia.Sedimentary Geology 334,1 1 5-141.
Veevers,J.J.,Saeed,A.,Belousova,E.A.,Griffin,W.L,2005.U-Pb ages and source composition by Hf-is otope and trace-element analysis of detrital zircons in Permian sandstone and modern sand from southwestern Australia and a review of the paleogeographical and denudational history of the Yilgarn Craton.Earth Science Reviews 68,245-279.
Vermeesch,P.,2009.RadialPlotter:aJava application for fission track,luminescence and other radial plots.Radiation Measurements 44,409-410.
Vermeesch,P.,2012.On the visualisation of detrital age distributions.Chemical Geology 312-313,190-194.
Ware,B.,2018.Large Igneous Provinces of the Southern Hemisphere:Isotopic Geochemistry and Flagioclas e and Pyroxene~(40)Ar/~(39)Ar Geochronology of the Kalkarindji,Karoo and Ferrar Province s.Department of Applied Geology.Curtin University,Perth,Western Australia,p.419.
Wendt,I.,Carl,C.,1991.The statistical distribution of the mean squared weighted deviation.Chemical Geology Isotope Geoscience Section 86,275-285.
Xu,J., Stockli,D.F.,Snedden,J.W.,2017.Enhanced provenance interpretation using combined U-Pb and(U-Th)/He double dating of detrital zircon grains from lower Miocene strata,proximal Gulf of Mexico Basin,North America.Earth and Planetary Science Letters 475,44-57.
Barham,M.,Reynolds,S.,Kirkland,C.I.,O'Leary,M.J.,Evans,N.J.,Allen,H.J.,Haines,P.W.,Hocking,R.M.,McDonald,B.J.,2018.Sediment routing and basin evolution in Proterozoic to Mesozoic east Gondwana:a case study from southern Australia.Gondwana Research 58,122-140.
Belousova,E.,Griffin,W.,O'Reilly.S.Y.,Fisher,N.,2002.Igneous zircon:trace element composition as an indicator of source rock type.Contributions to Mineralogy and Petrology 143,602-622.
Blakey,R.C.,2008.Gondwana palcogcography from assembly to breakup—A 500m.y.odyssey.In:Fielding,C.R.,Frank.T.D.,Isbell,J.L.(Eds.),Resolving the Late Paleozoic Ice Age in Time and Space.The Geological Society of America,Special Paper 441,Boulder,Colorado,pp.1-28.
Blevin,J.E.,Cathro,D.L,2008.Australian Southern Margin Synthesis,Project GA707,pp.1-104.
Blundy,J.,Wood.B.,1994.Prediction of crystal-melt partition coefficients from elastic moduli.Nature 372,452.
Boynton,W.V.,1984.Chapter 3-cosmochemistry of the rare Earth elements:meteorite studies.In:Henderson,P.(Ed.),Developments in Geochemistry.Elsevier,pp.63-1 14.
Bryan,S.E.,Constantine.A.E.,Stephens,C.J.,Ewart,A.,Schon.R.W.,Parianos,J.,1997.Early Cre taceous volcano-sedimentary successions along the eastern Australian continental margin:implications for the break-up of eastern Gondwana.Earth and Planetary Science Letters 153,85-102.
Bryan,S.E.,Cook,A.G.,Allen,C.M.,Siegel,C.,Purdy,D.J.,Greentree,J.S.,Uysal,I.T.,2012.Early-mid cretaceous tectonic evolution of eastern Gondwana:from silicic LIP magmatism to continental rupture.Episodes 35,142-152.
Bryan,S.E.,Ewart,A.,Stephens,C.J.,Parianos,J.,Downes,P.J.,2000.The Whitsunday Volcanic Province,Central Queensland,Australia:lithological and stratigraphic investigations of a silicic-dominated large igneous province.Journal of Volcanology and Geothermal Research 99,55-78.
Bryan,S.E.,Peate,I.U.,Peate,D.W.,Self,S.,Jerram,D.A.,Mawby,M.R.,Marsh,J.S.,Miller,J.A.,2010.The largest volcanic eruptions on Earth.Earth Science Reviews102.207-229.
Buret,Y.,von Quadt,A.,Heinrich,C.,Selby,D.,Walle,M.,Peytcheva,I.,2016.From a long-lived upper-crustal magma chamber to rapid porphyry copper emplacement:reading the geochemistry of zircon crystals at Bajo de la Alumbrera(NW Argentina).Earth and Planetary Science Letters 450,120-131.
Burgess,S.D.,Bowring,S.A,Fleming,T.H.,Elliot,D.H.,2015.High-precision geochronology links the Ferrar large igneous province with early-Jurassic ocean anoxia and biotic crisis.Earth and Planetary Science Letters 415.90-99.
Campbell,I.H.,Reiners,P.W.,Allen,C.M.,Nicolescu,S.,Upadhyay,R.,2005.He-Pb double dating of detrital zircons from the Ganges and Indus Rivers:implication for quantifying sediment recycling and provenance studies.Earth and Planetary Science Letters 237,402-432.
Cawood,P.A.,Hawkesworth,C.J.,Dhuime,B.,2012.Detrital zircon record and tectonic setting.Geology 40,875-878.
Cawood,P.A.Nemchin.A.A.,Freeman,M.,Sircombe,K.,2003.Linking source and sedimentary basin:detrital zircon record of sediment flux along a modern river system and implications for provenance studies.Earth and Planetary Science Letters 210,259-268.
Cecil,M.R.,Ducea,M.N.,Reiners,P.,Gehrels,G.,Mulch,A.,Allen,C.,Campbell,1.,2010.Provenance of Eocene river sediments from the central northern Sierra Nevada and implications for paleotopography.Tectonics 29,TC6010.https://doi.org/10.1029/2010TC002717.
Chapman,J.B.,Gehrels,G.E.,Ducea,M.N.,Giesler,N.,Pullen.A.,2016.A new method for estimating parent rock trace element concentrations from zircon.Chemical Geology 439,59-70.
Constantine,A.E.,2001.Sedimentology,Stratigraphy and Palacoenvironment of the Upper Jurassic-Lower Cretaceous Non-marine Strzelecki Group,Gippsland Basin,Southeastern Australia.Department of Earth Sciences.Monash University,Melbourne,Australia.
Corfu,F.,Hanchar,J.M.,Hoskin,P.W.O.,Kinny,P.,2003.Atlas of zircon textures.Reviews in Mineralogy and Geochemistry 53,469.
Danisik,M.,Stepancíkova,P.,Evans,N.J.,2012.Constraining long-term denudation and faulting history in intraplate regions by multisystem thcrmochronology:an example of the Sudetic Marginal Fault(Bohemian Massif,central Europe).Tectonics 31.
Dickinson,W.R.,Gehrels,G.E.,2009.Use of U-Pb ages of detrital zircons to infer maximum depositional ages of strata:a test against a Colorado Plateau Mesozoic database.Earth and Planetary Science Letters 288,115-125.
Dickinson,W.R.,Gehrels,G.E.,2010.Insights into north American paleogeography and paleotectonics from U-Pb ages of detrital zircons in Mesozoic strata of the Colorado plateau,USA.International Journal of Earth Sciences 99,1247-1265.
Direen,N.G.,Borissova,I.,Stagg,H.MJ.,Colwell,J.B.,Symonds,P.A.,2007.Nature of the continent-ocean transition zone along the southern Australian continental margin:a comparison of the Naturaliste Plateau,SW Australia,and the central Great Australian Bight sectors.Geological Society London Special Publications282,239-263.
Direen,N.G.,Stagg.H.MJ.,Symonds,P.A.,Colwell,J.B.,2008.Architecture of volcanic rifted margins:new insights from the Exmouth-gascoyne margin,Western Australia.Australian Journal of Earth Sciences 55,341-363.
Direen,N.G.,Stagg.H.M.J.,Symonds,P.A.,Colwell,J.B.,2011.Dominant symmetry of a conjugate southern Australian and East Antarctic magma-poor rifted margin segment.Geochemistry,Geophysics,Geosystems 12,Q02006.https://doi.org/10.1029/2010GC003306.
Duddy,I.R.,2003.Mesozoic.In:Birch,W.D.(Ed.),Geology of Victoria.Geological Society of Australia Special Publication,vol.23,pp.239-289.
Duddy,I.R.,2016.Gondwana-wide thermotectonic events and their expression in southern and south-eastern Australia before and after break-up:denudation,volcanism,sedimentation and provenance.In:Gross er,M.(Ed.), 2016 Selwyn Symposium.Supercontinents Assembly through Break-Up:An eastern Gondwana Perspective.The Geological Society of Australia-Victoria Division.The University of Melbourne,pp.39-41.
Ewart,A.,Schon,R.W.,Chappell,B.W.,1992.The Cretaceous volcanic-plutonic province of the central Queensland(Australia)coast—a rift related'calc-alkaline'province.Earth and Environmental Science Transactions of the Royal Society of Edinburgh 83,327-345.
Farley,KA,Wolf,R.A.,Silver,L.T.,1996.The effects of long alpha-stopping distances on(U-Th)/He ages.Geochimica et Cosmochimica Acta 60,4223-4229.
Fedo,C.M.,Sircombe,K.N.,Rainbird,R.H.,2003.Detrital zircon analysis of the sedimentary record.Reviews in Mineralogy and Geodiemistry 53,277-303.
Felton,E.A.,1992.Sedimentary History of the Early Cretaceous Otway Group,Otway Basin.Department of Geology.The University of Wollongong.Australia.
Fielding,L,Najman,Y.,Millar,I.,Butterworth,P.,Ando,S.,Padoan,M.,Barfod,D.,Kneller.,B.,201 7.A detrital record of the Nile River and its catchment Journal of the Geological Society 174,301-317.
Fisher,R.V.,1961.Proposed classification of volcaniclastic sediments and rocks.GSA Bulletin 72,1409-1414.
Fisher,R.V.,Schmincke,H.-U.,1984.Pyroclastic Rocks.Spinger-Verlag,Berlin.
Gagnevin,D.,Daly,J.S.,Kronz,A.,2010.Zircon texture and chemical composition as a guide to magmatic processes and mixing in a granitic environment and coeval volcanic system.Contributions to Mineralogy and Petrology 159,579-596.
Galbraith,RF.,1988.Graphical display of estimates having differing standard errors.Technometrics 30,271-281.
Galbraith,R.F.,1990.The radial plot:graphical assessment of spread in ages.International Journal of Radiation Applications and Instrumentation Part D Nuclear Tracks and Radiation Measurements 17,207-214.
Gallagher,K.,Dumitru,TA.,Gleadow,A.J.W.,1994.Constraints on the vertical motion of eastern Australia during the Mesozoic Basin Research 6,77-94.
Gallagher,K.,Lambeck,K.,1989.Subsidence,sedimentation and sea-level changes in the Eromanga Basin,Australia.Basin Research 2,115-131.
Gehrels,G.,2014.Detrital zircon U-Pb geochronology applied to tectonics.Annual Review of Earth and Planetary Sciences 42,127-149.
Geoscience Australia,2018.Otway Basin.Geoscience Australia.
Geoscience Australia and the Australian Stratigraphy Commission,2018.Australian Stratigraphic Units Database.Geoscience Australia and Australian Stratigraphy Commission.
Gibbons,A.D.,Whittaker,J.M.,M(u|¨)ller,R.D.,2013.The breakup of East Gondwana:assimilating constraints from Cre taceous ocean basins around India into a bestfit tectonic model.Journal of Geophysical Research Solid Earth 118,808-822.
Gleadow,A.J.W.,Duddy,I.R.,1981.Early Cretaceous volcanism and the early breakup history of southeastern Australia:evidence from fission track dating of volcaniclastic sediments.In:Gondwana Five:Selected Papers and Abstracts,fifth Gondwana symposium,pp.295-300.
Gradstein,F.M.,Ogg,J.G.,Schmitz,M.,Ogg,G.,2012.The Geologic Time Scale 2012.Elsevier,Amsterdam,the Netherlands.
Greentree,J.,2011.Palaeoenvironmental Setting of Dinosaur Trackways in the Context of the Closing Stages of Eromanga Basin Evolution.Queensland University of Technology,Brisbane,Australia,p.107.
Grey,K.,Hocking,R.H.,Stevens,M.K.,Bagas,L.,Carlsen,G.M.,Irimies,F.,Pirajno,F.,Haines,P.W.,Apak,S.N.,200.5.Lithostratigraphic Nomenclature of the Officer Basin and Correlative Parts of the Paterson Orogen,Western Australia.
Grimes,C.B.,John.B.E.,Kelemen,P.B.,Mazdab,F.K.,Wooden,J.L.,Cheadle,M.J.,Hangh(?)j,K.,Schwartz,J.J.,2007.Trace element chemistry of zircons from oceanic crust:a method for distinguishing detrital zircon provenance.Geology35,643-646.
Grimes,C.B.,Wooden,J.L,Cheadle,M.J.,John,B.E.,2015."Fingerprinting"tectonomagmatic provenance using trace elements in igneous zircon.Contributions to Mineralogy and Petrology 170,1-26.
Guenthner,W.R.,Reiners,P.W.,Ketcham,R.A.,Nasdala,L.,Giester,G.,2013.Helium diffu sion in natural zircon:radiation damage,anisotropy,and the interpretation of zircon(U-Th)/He thermochronology.American Journal of Science 313,145-198.
Haq,B.U.,2014.Cretaceous eustasy revisited.Global and Planetary Change 113,44-58.
Heiken.,G.,1985.Volcanic Ash.University of California Press,Los Alamos,USA.
Helby,R.,Morgan,R.,Partridge,A.D.,1987.A palynological zonation of the Australian Mesozoic.In:Jell,P.A.(Ed.),Studies in Australian Mesozoic Palynology.Memoir Association Australasian Palaeontologists,pp.1-94.
Hopkinson,T.N.,Harris,N.B.W.,Warren,C.J.,Spencer,C.J.,Roberts,N.M.W.,Horstwood,M.S.A.,Parrish,R.R.,Eimf,2017.The identification and significance of pure sediment-derived granites.Earth and Planetary Science Letters 467,57-63.
Hou,B.,Keeling.J.,Reid,A.,Fairclough,M.,Wairland,I.,Belousova,E.,Frakes,L.,Hocking,R.,2011.Heavy mineral sands in the Eucla Basin,Southern Australia:depositional and province-scale prospectivity.Economic Geology 106,687-712.
Ito,H.,Spencer,C.J.,Danisik,M.,Hoiland,C.W.,2017.Magmatic tempo of Earth's youngest exposed plutons as revealed by detrital zircon U-Pb geochronology.Scientific Reports 7.12457.
Kaczmarek,M.-A.,Miintener,O.,Rubatto,D.,2008.Trace element chemistry and U-Pb dating of zircons from oceanic gabbros and their relationship with whole rock composition(Lanzo,Italian Alps).Contributions to Mineralogy and Petrology 155,295-312.
Kirkland,C.I.,Daly,J.S.,Whitehouse,M.J.,2007.Provenance and terrane evolution of the kalak nappe complex,Norwegian caledonides:implications for neoproterozoic paleogeography and tectonics.The Journal of Geology 115,21-41.
Kirkland,C.L,Smithies,R.H.,Spaggiari,C.V.,Wingate,M.T.D.,Quentin de Gromard,R.,Clark,C.,Gardiner.N.J.,Belousova,E.A.,2017.Proterozoic crustal evolution of the Eucla basement,Australia:implications for destruction of oceanic crust during emergence of Nuna.Lithos 278-281,427-444.
Laurie,J.R.,Bodorkos,S., Nicoll,R.S.,Crowley,J.L.,Mantle,D.J.,Mory,A.J.,Wood,G.R.,Backhouse,J.,Holmes,E.K.,Smith,T.E.,Champion,D.C.,2016.Calibrating themiddle and late Permian palynostratigraphy of Australia to the geologic timescale via U-Pb zircon CA-IDTIMS dating.Australian Journal of Earth Sciences63,701-730.
Lissenberg,C.J.,Rioux,M.,Shimizu,N.,Bowring,SA.,Mevel,C.,2009.Zircon dating of oceanic crustal accretion.Science 323,1048-1050.
Lloyd,J.,Collins,A.S.,Payne,J.L.,Glorie,S.,Holford,S.,Reid,A.J.,2016.Tracking the Cretaceous transcontinental Ceduna River through Australia:the hafnium isotope record of detrital zircons from offshore southern Australia.Geoscience Frontiers 7,237-244.
Lowry,D.C.,1970.In:Australia,G.S.o.W.(Ed.),Geology of the Western Australian Part of the Eucla Basin.Geological Survey of Western Australia,Perth,p.207.
Ludwig,K.R.,2012.User's manual for isoplot/Ex,v.3.75,A Geochronological Toolkit for Microsoft Excel,vol.5.Berkeley Geochronological Center Special Publications.
MacDonald,J.D.,Holford,S.P.,Green,P.F.,Duddy,I.R.,King.R.C.,Backe,G.,2013.Detrital zircon data reveal the origin of Australia's largest delta system.Journal of the Geological Society 170,3-6.
Makulini,P.,Kirkland,C.L.,Barham,M.,2018.Zircon grain shape holds provenance information;a case study from southwestern Australia.Geological Journal 1-15.
Mami,T.,Kenji,H.,Kenichiro,T.,Takeyoshi,Y.,Tomokazu,H.,Shoichi,K.,2017.Timescale of magma chamber processes revealed by U-Pb ages,trace element contentis and morphology of zircons from the Ishizuchi caldera,Southwest Japan Arc Island Arc 26,e 12182.
Markwitz,V.,Kirkland,C.L.,2018.Source to sink zircon grain shape:constraints on selective preservation and significance for Western Australian Proterozoic basin provenance.Geoscience Frontiers 9,415-430.
Markwitz,V.,Kirkland,C.L,Mehnert,A.,Gessner,K.,Shaw,J.,2017.3-D characterization of detrital zircon grains and its implications for fluvial transport,mixing.and preservation bias.Geochemistry,Geophysics,Geosystems 18,4655-4673.
Matthews,K.J.,Hale,A.J.,Gurnis,M.,Miiller,R.D.,DiCaprio,L,2011.Dynamic subsidence of eastern Australia during the cretaceous.Gondwana Res earch 19,372-383.
McKenzie.N.R.,Smye,A.J.,Hegde,V.S.,Stockli,D.F.,2018.Continental growth histories revealed by detrital zircon trace elements:a case study from India.Geology 46,275-278.
Meeuws,F.J.E.,Holford,S.P.,Foden,J.D.,Schofield,N.,2016.Distribution,chronology and causes of Cretaceous-Cenozoic magmatism along the magma-poor rifted southern Australian margin:Links between mantle melting and basin formation.Marine and Petroleum Geology 73,271-298.
Menzies,M.A., Klemperer,S.L,Ebinger,C.J.,Baker,J.,2002.Characteristics of volcanic rifted margins.In:Menzies,MA.,Klemperer.S.L.,Ebinger,C.J.,Baker,J.(Eds.),Volcanic Rifted Margins.Geological Society of America.
Metcalfe,I.,Crowley,J.L.,Nicoll,R.S.,Schmitz,M.,2015.High-precision U-Pb CATIMS calibration of Middle Permian to Lower Triassic sequences,mass extinction and extreme climate-change in eastern Australian Gondwana.Gondwana Research 28.61-81.
Mihut,D.,Muller,R.D.,1998.Volcanic margin formation and mesozoic rift propagators in the cuvier abyssal plain off western Australia.Journal of Geophysical Research Solid Earth 103,27135-27149.
Mory,A.J.,Crowley,J.L.,Backhouse,J.,Nicoll,RS.,Bryan. S.E.,López Martinez,M.,Mantle,D.J.,2017.Apparent conflicting Roadian-Wordian(middle permian)CA-IDTIMS and palynology ages from the canning basin,western Australia.Australian Journal of Earth Sciences 64,889-901.
M(u|¨)ller,R.D.,Flament,N..Matthews,K.J.,Williams,S.F.,Guris,M.,2016.Formation of Australian continental margin highlands driven by pla te-mantle interaction.Earth and Planetary Science Letters 441,60-70.
M(u|¨)ller,R.D.,Gaina,C.,Clark,S.,2000.Seafloor spreading around Australia.In:Veevers,J.(Ed.),Billion-year Earth History of Australia and Neighbours in Gondwanaland.Gemoc Press.Sydney,Australia,pp.18-28.
Norvick,M.S.,Smith,M.A.,Power,M.R.,2001.The plate tectonic evolution of eastern australasia guided by the stratigraphy of the Gippsland basin.In:Hill,K.C.,Bernecker,T.(Eds.),Eastern Australasian Basins Symposium:A Refocused Energy Perspective for the Future.Petroleum Exploration Society of Australia,Special Publications,Melbourne,pp.15-24.
Olierook,H.K.H.,Barham,M.,Fitzsimons,I.C.W.,Timms,N.E.,Jiang,Q.,Evans,N.J.,McDonald.B.J.,201 9.Tectonic controls on sediment provenance evolution in rift basins:detrital zircon U-Pb and Hf isotope analysis from the Perth Basin.Western Australia.Gondwana Research 66,126-142.
Olierook,H.K.H.,Jourdan,F.,Merle,R.E.,Timms,N.E.,Kusznir,N.,Muhling,J.R.,2016.Bunbury Basalt:Gondwana breakup products or earliest vestiges of the Kerguelen mantle plume?Earth and Planetary Science Letters 440,20-32.
Olierook,H.K.H.,Timms,N.E.,Wellmann,J.F.,Corbel,S.,Wilkes,P.G.,2015.3D structural and stratigraphic model of the Perth Basin,Western Australia:implications for sub-basin evolution.Australian Journal of Earth Sciences 62.447-467.
Partridge,A.D.,2006.Late Cretaceous palynology zonations for Australia.In:Monteil,E.(Ed.),Australian Mesozoic and Cenozoic Palynology ZonationsUpdated to the 2004 Geologic Timescale.Geoscience Australia,p.8.
Pirajno,F.,Hoatson,D.M.,2012.A review of Australia's Large Igneous Provinces and associated mineral systems:implications for mantle dynamics through geological time.Ore Geology Reviews 48,2-54.
Playford,P.E.,Cockbain,A.E.,Low.G.H.,1976.Geology of the Perth Basin,western Australia,vol.124.Geological Survey of Western Australia Bulletin,Perth,Australia.
Pointon,M A.,Chew,D.M.,Ovtcharova,M.,Sevastopulo,G.D.,Crowley,Q.G.,2012.New high-precision U-Pb dates from western European Carboniferous tuffs;implications for time scale calibration,the periodicity of late Carboniferous cycles and stratigraphical correlation.Journal of the Geological Society 169,713-721.
Pointon,M.A.,Chew,D.M.,Ovtcharova.M.,Sevastopulo.,G.D.,Delcambre,B.,2014.High-precision U-Pb zircon CA-ID-TIMS dates from western European late Visean bentonites.Journal of the Geological Society 171,649-658.
Rahl,J.M.,Reiners,P.W.,Campbell,I.H.,Nicolescu,S.,Allen,C.M.,2003.Combined single-grain(U-Th)/He and U/Pb dating of detrital zircons from the Navajo Sandstone,Utah.Geology 3 1,761-764.
Rasmussen,B.,Fletcher,I.R.,2010.Dating sedimentary rocks using in situ U-Pb geochronology of syneruptive zircon in ash-fall tuffs<1 mm thick.Geology 38,299-302.
Reid.A.,Keeling,J.,Boyd,D.,Belousova,E.,Hou,B.,2013.Source of zircon in worldclass heavy mineral placer deposits of the Cenozoic Eucla Basin,southern Australia from LA-ICPMS U-Pb geochronology.Sedimentary Geology 286-287,1-19.
Reiners.,P.W.,Campbell,I.H.,Nicolescu,S.,Allen,C.M.,Hourigan,J.K.,Garver,J.I.,Mattinson,J.M.,Cowan,D.S.,2005.(U-Th)/(He-Pb)double dating of detrital zircons.American Journal of Science 305,259-311.
Reiners,P.W.,Spell,T.L.,Nicolescu,S.,Zanetti,KA.2004.Zircon(U-Th)/He thermochronometry:He diffusion and comparisons with~(40)Ar/~(39)Ar dating.Geochimica et Cosmochimica Acta 68,1857-1887.
Salles,T.,Flament,N.,M(u|¨)ller,D.,2017.Influence of mantle flow on the drainage of eastern Australia since the Jurassic Period.Geochemistry,Geophysics,Geosystems 18,280-305.
Sano,Y.,Tsutsumi,Y.,Terada,K.,Kaneoka,I.,2002.Ion microprobe U-Pb dating of Quaternary zircon:implication for magma cooling and residence time.Journal of Volcanology and Geothermal Research 117,285-296.
Saylor,J.E.,Stockli,D.F.,Horton.B.K.,Nic,J.,Mora,A.,2012.Dis criminating rapid exhumation from syndepositional volcanism using detrital zircon double dating:implications for the tectonic history of the Eastern Cordillera,Colombia.GSA Bulletin 124,762-779.
Schmitz,M.D.,2012.Radiogenic isotope geochronology.In:Gradstein,F.,Ogg,J.G.,Schmitz,M.,Ogg,G.(Eds.),The Geological Timescale.Elsevier,Amsterdam,pp.115-12 7.
Schoene,B.,Condon,D.J.,Morgan,L.,Mclean,N.,2013.Precision and accuracy in geochronology.Elements 9,19-24.
Schofield,A.,Totterdell,J.,2008.Distribution,Timing and Origin of Magmatism in the Bight and Eucla Basins,p.19.
Seton,M.M(u|¨)lle r,R.D.,Zahirovic,S.,Gaina,C.,Torsvik,T.,Shephard,G.,Talsma,A.,Gurnis,M.,Turner,M.,Maus,S.,Chandler,M.,2012.Global continental and ocean basin reconstructions since 200Ma.Earth-Science Reviews 113,212-270.
Sircombe.K.N.,Freeman,M.J.,1999.Provenance of detrital zircons on the Western Australia coastline—implications for the geologic history of the Perth basin and denudation of the Yilgam craton.Geology 27,879-882.
Spencer,CJ.,Cavosie,A.J.,Raub,T.D.,Rollinson,H.,Jeon,H..Searle,M.P.,Miller,J.A.,McDonald,B.J.,Evans,N.J.,The Edinburgh Ion Microprobe Facility,2017.Evidence for melting mud in Earth's mantle from extreme oxygen isotope signatures in zircon.Geology 45,975-978.
Spencer,C.J.,Danisik,M.,Ito,H.,Hoiland,C.,Tapster.S.,Jeon,H.,McDonald,B.,Evans,N.J.,2019.Rapid exhumation of Earth's youngest exposed granites driven by subduction of an oceanic arc Geophysical Research Letters 46.https://doi.org/10.1029/2018GL080579.
Spencer,C.J.,Kirkland,C.L.,Roberts,N.M.W.,2018.Implications of erosion and bedrock composition on zircon fertility:examples from South America and Western Australia.Terra Nova 30,289-295.
Spencer,CJ.,Kirkland,C.L,Taylor,RJ.M.,2016.Strategies towards statistically robust interpretations of in situ U-Pb zircon geochronology.Geoscience Frontiers 7,58 1-589.
Stagg,H.MJ.,Cockshell,C.D.,Willcox,J.B.,Hill,A.J.,Needham,D.J.L.,Thomas,B.,O'Brien,G.W.,Hough,L.P.,1990.Basins of the Great Australian Bight Region:Geology and Petroleum Potential.Bureau of Mineral Resources.Continental Margins Program Folio 5.
Suthren.R.J.,1985.Facies analysis of volcaniclastic sediments:a review.Geological Society,London,Special Publications 18,123-146.
Tosolini,A.-M.P.,Korasidis,V.A.,Wagstaff,B.E.,Cantrill,D.J.,Gallagher,S.J.,Norvick,M.S.,2018.Palaeoenvironments and palaeocommunities from lower cretaceous high-latitude sites,Otway Basin,southeastern Australia.Palaeogeography,Palaeoclimatology,Palaeoecology 496,62-84.
Totterdell,J.M.,Bradshaw,B.E.,2004.The structural framework and tectonic evolution of the Bight Basin.In:Boult,P.J.,Johns,D.R.,Lang,S.C.(Eds.),Eastern Australasian Basins Symposium II.Petroleum Exploration Society of Australia,Special Publication,pp.41-61.
Totterdell.J.M.,Krassay,A.A.,2003.Sequence stratigraphic correlation of onshore and offshore Bight Basin successions.Geoscience Australia Record 2003/02,50 pp.
Trail,D.,Bruce Watson,E.,Tailby,N.D.,2012.Ce and Eu anomalies in zircon as proxies for the oxidation state of magmas.Geochimica et Cosmochimica Acta97,70-87.
Tucker.R.T.,Roberts,E.M.,Henderson,R.A.,Kemp,A.I.S.,2016.Large igneous province or long-lived magmatic arc along the eastern margin of Australia during the Cretaceous? Insights from the sedimentary record.The Geological Society of America Bulletin 128,1461-1480.
Tucker,R.T.,Roberts,F.M.,Hu,Y.,Kemp,A.I.S.,Salisbury,S.W.,2013.Detrital zircon age constraints for the Winton formation,Queensland:contextualizing Australia's late cretaceous dinosaur faunas.Gondwana Research 24.767-779.
Veevers,J.J.,2000.Change of tectono-stratigraphic regime in the Australian plate during the 99 Ma(mid-Cretaceous)and 43 Ma(mid-Eocene)swerves of the Pacific.Geology 28,47-50.
Veevers.J.J.,Belousova,E.A.,Saeed,A.,2016.Zircons traced from the 700-500 Ma transgondwanan supermountains and the gamburtsev subglacial mountains to the ordovician lachlan orogen,cretaceous Ceduna delta,and modem channel country,central-southern Australia.Sedimentary Geology 334,1 1 5-141.
Veevers,J.J.,Saeed,A.,Belousova,E.A.,Griffin,W.L,2005.U-Pb ages and source composition by Hf-is otope and trace-element analysis of detrital zircons in Permian sandstone and modern sand from southwestern Australia and a review of the paleogeographical and denudational history of the Yilgarn Craton.Earth Science Reviews 68,245-279.
Vermeesch,P.,2009.RadialPlotter:aJava application for fission track,luminescence and other radial plots.Radiation Measurements 44,409-410.
Vermeesch,P.,2012.On the visualisation of detrital age distributions.Chemical Geology 312-313,190-194.
Ware,B.,2018.Large Igneous Provinces of the Southern Hemisphere:Isotopic Geochemistry and Flagioclas e and Pyroxene~(40)Ar/~(39)Ar Geochronology of the Kalkarindji,Karoo and Ferrar Province s.Department of Applied Geology.Curtin University,Perth,Western Australia,p.419.
Wendt,I.,Carl,C.,1991.The statistical distribution of the mean squared weighted deviation.Chemical Geology Isotope Geoscience Section 86,275-285.
Xu,J., Stockli,D.F.,Snedden,J.W.,2017.Enhanced provenance interpretation using combined U-Pb and(U-Th)/He double dating of detrital zircon grains from lower Miocene strata,proximal Gulf of Mexico Basin,North America.Earth and Planetary Science Letters 475,44-57.