Lithospheric structure of the Pilbara Craton, Capricorn Orogen and northern Yilgarn Craton, Western Australia, from teleseismic receiver functions

2003 ◽  
Vol 50 (3) ◽  
pp. 439-445 ◽  
Author(s):  
A. M. Reading ◽  
B. L. N. Kennett
Geology ◽  
2019 ◽  
Vol 47 (11) ◽  
pp. 1098-1102 ◽  
Author(s):  
Andreas Petersson ◽  
Anthony I.S. Kemp ◽  
Martin J. Whitehouse

Abstract Knowledge of the age and compositional architecture of Archean cratonic lithosphere is critical for models of geodynamics and continental growth on early Earth, but can be difficult to unravel from the exposed geology. We report the occurrence of numerous >3.7 Ga zircon crystals in 3.45 Ga rhyolites of the eastern Pilbara Craton (Western Australia), which preserve evidence for an Eoarchean meta-igneous component in the deep Pilbara crust. This inherited zircon population shares similar and distinctive age and Hf-O isotope characteristics with the oldest gneissic components of the Yilgarn Craton ∼500 km farther south, suggesting a common ca. 3.75 Ga felsic crustal nucleus to these two Archean granite-greenstone terranes. We infer a pivotal role for such ‘seeds’ in facilitating the growth and persistence of Archean continental lithosphere.


2007 ◽  
Vol 158 (3-4) ◽  
pp. 198-227 ◽  
Author(s):  
Abigail C. Allwood ◽  
Malcolm R. Walter ◽  
Ian W. Burch ◽  
Balz S. Kamber

1992 ◽  
Vol 56 (3-4) ◽  
pp. 169-189 ◽  
Author(s):  
R.I. Thorpe ◽  
A.H. Hickman ◽  
D.W. Davis ◽  
J.K. Mortensen ◽  
A.F. Trendall

2008 ◽  
Vol 162 (3-4) ◽  
pp. 354-384 ◽  
Author(s):  
Catherine V. Spaggiari ◽  
Jo-Anne Wartho ◽  
Simon A. Wilde

1992 ◽  
Vol 54 (2-4) ◽  
pp. 211-229 ◽  
Author(s):  
I.M. Tyler ◽  
I.R. Fletcher ◽  
J.R. de Laeter ◽  
I.R. Williams ◽  
W.G. Libby

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