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Geochemistry of the Mount-Windsor Volcanics - Implications for the Tectonic Setting of Cambro-Ordovician Volcanic-Hosted Massive Sulfide Mineralization in Northeastern Australia
Citation
Stolz, AJ, Geochemistry of the Mount-Windsor Volcanics - Implications for the Tectonic Setting of Cambro-Ordovician Volcanic-Hosted Massive Sulfide Mineralization in Northeastern Australia, Economic Geology, 90, (5) pp. 1080-1097. ISSN 0361-0128 (1995) [Refereed Article]
DOI: doi:10.2113/gsecongeo.90.5.1080
Abstract
The Mount Windsor subprovince is an important relic of Upper Cambrian to Lower Ordovician sedimentation and volcanism in the northern part of the Tasman orogenic zone. Volcanic-hosted massive sulfide mineralization occurs at several stratigraphic horizons. Major and trace element data and Nd isotope ratios are presented for the least altered coherent units from the three major volcanic-bearing formations in the Mount Windsor subprovince. The data are used to discriminate four major phases of volcanism and related intrusive activity derived from three isotopically discrete sources and to assess the geodynamic setting in which the volcanism occurred. -from Author
Item Details
| Item Type: | Refereed Article |
|---|---|
| Research Division: | Earth Sciences |
| Research Group: | Geochemistry |
| Research Field: | Exploration Geochemistry |
| Objective Division: | Mineral Resources (excl. Energy Resources) |
| Objective Group: | Other Mineral Resources (excl. Energy Resources) |
| Objective Field: | Mineral Resources (excl. Energy Resources) not elsewhere classified |
| Author: | Stolz, AJ (Dr Andrew Stolz) |
| ID Code: | 6018 |
| Year Published: | 1995 |
| Web of Science® Times Cited: | 41 |
| Deposited By: | Earth Sciences |
| Deposited On: | 1995-08-01 |
| Last Modified: | 2011-08-25 |
| Downloads: | 0 |
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