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

Author:

Reading A. M.,Kennett B. L. N.

Publisher

Informa UK Limited

Subject

General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)

Reference36 articles.

1. AmmonC. J., RandallG. E. & ZandtG.1991. The isolation of receiver effects from teleseismic P waveforms . Bulletin of the Seismological Society of America81, 2504–2510.

2. Barley, M. E. (1998) The tectonic and metallogenic evolution of the Pilbara Craton: preface Precambrian Research, 88, pp. 1 - 2.

3. Blewett, R. S. (2002) Archaean tectonic processes: a case for horizontal shortening in the Northern Pilbara Granite‐Greenstone Terrane, Western Australia Precambrian Research, 113, pp. 87 - 120.

4. Buick, R. and Thornett, J. R. and McNaughton, N. J. and Smith, J. B. and Barley, M. E. and Savage, M. (1995) Record of emergent continental crust ∼3.5 billion years ago in the Pilbara Craton of Australia Nature, 375, pp. 574 - 577.

5. Clitheroe, G. and Gudmundsson, O. and Kennett, B. L. N. (2000) The crustal thickness of Australia Journal of Geophysical Research, 105, pp. 13697 - 13713.

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