An extensive, crustally-derived, 3325 to 3310 Ma silicic volcanoplutonic suite in the eastern Pilbara Craton: evidence from the Kelly Belt, McPhee Dome and Corunna Downs Batholith
- 28 May 1999
- journal article
- Published by Elsevier
- Vol. 96 (1-2) , 41-62
- https://doi.org/10.1016/s0301-9268(99)00003-0
Abstract
No abstract availableKeywords
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