Evidence from U–Pb zircon and 40 Ar/ 39 Ar muscovite detrital mineral ages in metasandstones for movement of the Torlesse suspect terrane around the eastern margin of Gondwanaland

Author:

Adams C.J.1,Barley M.E.2,Fletcher I.R.2,Pickard A.L.3

Affiliation:

1. Institute of Geological and Nuclear Sciences, PO Box 31312, Lower Hutt, New Zealand,

2. Centre for Strategic Mineral Deposits, Department of Geology and Geophysics, University of Western Australia, Nedlands, Western Australia 6907, Australia,

3. Centre for Strategic Mineral Deposits, Department of Geology and Geophysics, University of Western Australia, Nedlands, Western Australia 6907, Australia

Publisher

Wiley

Subject

Geology

Reference59 articles.

1. Geochronological studies of the Swanson Formation of Marie Byrd Land, West Antarctica, and correlation with northern Victoria Land, East Antarctica, and South Island, New Zealand

2. Geochronology of granite terranes in the Ford Ranges, Marie Byrd Land, West Antarctica

3. 3C.J. Adams, 1996 . A Queensland provenance for New Zealand Permo-Triassic Torlesse metagreywacke terranes: a review of the age and isotopic evidence. In:Mesozoic Geology of the Eastern Australia Plate Conference, Brisbane, Australia.Geological Society of Australia Inc., Extended Abstracts no. 43, pp. 1 -6.

4. 4C.J. Adams, 1997 . Tracing the continuity and ancestry of Paleozoic and Mesozoic metasedimentary terranes at the southwest pacific margin of Gondwana by their age and strontium isotopic characteristics. In: Terrane Dynamics-97 (J.D. Bradshaw and S.W. Weaver, eds), 10-14 February 1997, International Conference on Terrane Geology, University of Canterbury, Christchurch, New Zealand, p. 1.

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