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SPAGGIARI, C, PIDGEON, R, WILDE, S (2007) The Jack Hills greenstone belt, Western Australia. Part 2: Lithological relationships and implications for the deposition of ≥4.0 Ga detrital zircons. Precambrian Research, 155 (3-4). 261-286 doi:10.1016/j.precamres.2007.02.004

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Reference TypeJournal (article/letter/editorial)
TitleThe Jack Hills greenstone belt, Western Australia. Part 2: Lithological relationships and implications for the deposition of ≥4.0 Ga detrital zircons
JournalPrecambrian Research
AuthorsSPAGGIARI, CAuthor
PIDGEON, RAuthor
WILDE, SAuthor
Year2007 (June 1)Volume155
Page(s)261-286Issue3-4
PublisherElsevier BV
URL
DOIdoi:10.1016/j.precamres.2007.02.004Search in ResearchGate
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Mindat Ref. ID705296Long-form Identifiermindat:1:5:705296:9
GUID0
Full ReferenceSPAGGIARI, C, PIDGEON, R, WILDE, S (2007) The Jack Hills greenstone belt, Western Australia. Part 2: Lithological relationships and implications for the deposition of ≥4.0 Ga detrital zircons. Precambrian Research, 155 (3-4). 261-286 doi:10.1016/j.precamres.2007.02.004
Plain TextSPAGGIARI, C, PIDGEON, R, WILDE, S (2007) The Jack Hills greenstone belt, Western Australia. Part 2: Lithological relationships and implications for the deposition of ≥4.0 Ga detrital zircons. Precambrian Research, 155 (3-4). 261-286 doi:10.1016/j.precamres.2007.02.004
In(2007, June) Precambrian Research Vol. 155 (3) Elsevier BV

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Jack Hills, Nookawarra Station, Murchison Shire, Western Australia, Australia

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SPAGGIARI, C (2007) The Jack Hills greenstone belt, Western AustraliaPart 1: Structural and tectonic evolution over >1.5Ga. Precambrian Research, 155 (3) 204-228 doi:10.1016/j.precamres.2007.02.007
Spaggiari, C. V. (2007) Structural and lithological evolution of the Jack Hills greenstone belt, Narryer Terrane, Yilgarn Craton, Western Australia. Record 2007/3. Geological Survey of Western Australia
Wilde, Simon A. (2010) Proterozoic volcanism in the Jack Hills Belt, Western Australia: Some implications and consequences for the World's oldest zircon population. Precambrian Research, 183 (1) 9-24 doi:10.1016/j.precamres.2010.05.007
DUNN, S, NEMCHIN, A, CAWOOD, P, PIDGEON, R (2005) Provenance record of the Jack Hills metasedimentary belt: Source of the Earth's oldest zircons. Precambrian Research, 138 (3) 235-254 doi:10.1016/j.precamres.2005.05.001
Rasmussen, Birger, Fletcher, Ian R., Muhling, Janet R., Wilde, Simon A. (2010) In situ U–Th–Pb geochronology of monazite and xenotime from the Jack Hills belt: Implications for the age of deposition and metamorphism of Hadean zircons. Precambrian Research, 180 (1) 26-46 doi:10.1016/j.precamres.2010.03.004
Compston, W., Pidgeon, R. T. (1986) Jack Hills, evidence of more very old detrital zircons in Western Australia. Nature, 321 (6072). 766-769 doi:10.1038/321766a0
Hayman, Patrick C., Fullard, Rhiannon, Cas, Ray A.F., Squire, Richard J. (2020) Clasts in Archean conglomerates and implications for uplift: Evidence from the 2.7 Ga Agnew Greenstone Belt (Western Australia) Precambrian Research, 344. 105758pp. doi:10.1016/j.precamres.2020.105758
Pidgeon, R. T., Wilde, S. A., Compston, W., Shield, M. W. (1990) Archaean evolution of the Wongan Hills Greenstone Belt, Yilgarn Craton, Western Australia. Australian Journal of Earth Sciences, 37 (3) 279-292 doi:10.1080/08120099008727927
Kober, B., Pidgeon, R.T., Lippolt, H.J. (1989) Single-zircon dating by stepwise Pb-evaporation constrains the Archean history of detrital zircons from the Jack Hills, Western Australia. Earth and Planetary Science Letters, 91 (3) 286-296 doi:10.1016/0012-821x(89)90004-6
Pidgeon, R.T., Nemchin, A.A. (2006) High abundance of early Archaean grains and the age distribution of detrital zircons in a sillimanite-bearing quartzite from Mt Narryer, Western Australia. Precambrian Research, 150 (3) 201-220 doi:10.1016/j.precamres.2006.07.008
Pidgeon, R.T, Wilde, S.A (1998) The interpretation of complex zircon U–Pb systems in Archaean granitoids and gneisses from the Jack Hills, Narryer Gneiss Terrane, Western Australia. Precambrian Research, 91 (3) 309-332 doi:10.1016/s0301-9268(98)00056-4
 
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