Genetic types of tantalum ore deposits and their economic importance |
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| Abstract: | Metasediments and meta-igneous rocks of the Willyama Supergroup in the Paleoproterozoic Olary Block of South Australia were deposited at ～1700 Ma. Intrusion by I-type granitoids at 1630 Ma was followed by the Olarian Orogeny, comprising two events of deformation and high-grade metamorphism at 1590 ± 20 Ma. Regional S-type granites and rare-metal pegmatites also formed during the Olarian Orogeny. The K-Ar isotopic system in primary pegmatitic muscovite closed at ～1505 ± 7 Ma, and the third event (regressive) of deformation and metamorphism together with minor granite emplacement, associated with the Olarian Orogeny, occurred at 1500 ± 20 Ma. A widespread thermal event occurred at 1100 to 1200 Ma and resulted from the Musgravian Orogeny. This was followed by crustal extension, tholeiitic dolerite dike intrusion, and rifting at 700 to 800 Ma. Cooling after the Delamerian Orogeny is recorded at ～466 to 475 Ma in the muscovite data. The 40Ar/39Ar data from many mica samples are complex because of multiple phases of thermal resetting and regression. This partial resetting of the K-Ar system is characterized by multiple age components and mixtures between them. |
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