Early archaean zircon ages from orthogneisses and anorthosites at Mount Narryer, Western Australia

[1]  K. Rosman,et al.  Sm-Nd, Pb-Pb and Rb-Sr geochronology of the manfred complex, Mount Narryer, Western Australia , 1988 .

[2]  J. Myers Oldest known terrestrial anorthosite at Mount Narryer, Western Australia , 1988 .

[3]  W. Compston,et al.  Four zircon ages from one rock: the history of a 3930 Ma-old granulite from Mount Sones, Enderby Land, Antarctica , 1986 .

[4]  W. Compston,et al.  The age and Pb loss behaviour of zircons from the Isua supracrustal belt as determined by ion microprobe , 1986 .

[5]  P. Kinny 3820 Ma zircons from a tonalitic Armîsoq gneiss in the Godthåb district of Southern West Greenland , 1986 .

[6]  W. Compston,et al.  Jack Hills, evidence of more very old detrital zircons in Western Australia , 1986, Nature.

[7]  M. McCulloch,et al.  Contrasting zircon U‐Pb and model Sm‐Nd ages for the Archaean Logue Brook Granite , 1986 .

[8]  M. Bickle,et al.  Rb‐Sr, Sm‐Nd and Pb‐Pb geochronology of ancient gneisses from Mt Narryer, Western Australia , 1985 .

[9]  T. Ireland,et al.  The age of (a tiny part of) the Australian continent , 1985, Nature.

[10]  U. Schärer,et al.  Determination of the age of the Australian continent by single-grain zircon analysis of Mt Narryer metaquartzite , 1985, Nature.

[11]  J. Myers,et al.  Early Precambrian crustal evolution at Mount Narryer, Western Australia , 1985 .

[12]  J. Wijbrans Geochronology of metamorphic terrains by the ⁴⁰Ar/³⁹Ar age spectrum method , 1985 .

[13]  W. Compston,et al.  Dating Archean zircon by ion microprobe: New light on an old problem , 1985 .

[14]  W. Compston,et al.  Unsupported radiogenic Pb in zircon: a cause of anomalously high Pb-Pb, U-Pb and Th-Pb ages , 1984 .

[15]  W. Compston,et al.  U‐Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass‐resolution ion microprobe , 1984 .

[16]  W. Compston,et al.  Ion microprobe identification of 4,100–4,200 Myr-old terrestrial zircons , 1983, Nature.

[17]  U. Schärer,et al.  Uranium–lead system in fragments of a single zircon grain , 1982, Nature.

[18]  R. D. Gee,et al.  Early Archaean gneisses from the Yilgarn Block, Western Australia , 1981 .

[19]  K. Ludwig,et al.  Uranium-lead isotope systematics and apparent ages of zircons and other minerals in precambrian granitic rocks, Granite Mountains, Wyoming , 1978 .

[20]  R. Steiger,et al.  Subcommission on geochronology: Convention on the use of decay constants in geo- and cosmochronology , 1977 .

[21]  G. L. Cumming,et al.  Ore lead isotope ratios in a continuously changing earth , 1975 .

[22]  R. Pidgeon,et al.  Examples of twinning and parallel growth in zircons from some Precambrian granites and gneisses , 1974, Mineralogical Magazine.

[23]  D.,et al.  U-Pb Systematics of Detrital Zircons from Some Unmetamorphosed to Slightly Metamorphosed Sediments of Central Europe , 2022 .