- Title
- Geochemical characteristics and structural setting of lithium–caesium–tantalum pegmatites of the Dorchap Dyke Swarm, northeast Victoria, Australia
- Creator
- Hines, Benjamin; Turnbull, D.; Ashworth, Luisa; McKnight, Stafford
- Date
- 2023
- Type
- Text; Journal article
- Identifier
- http://researchonline.federation.edu.au/vital/access/HandleResolver/1959.17/194431
- Identifier
- vital:18352
- Identifier
-
https://doi.org/10.1080/08120099.2023.2209649
- Identifier
- ISSN:0812-0099 (ISSN)
- Abstract
- The Dorchap Dyke Swarm hosts the first recorded occurrence of lithium–caesium–tantalum (LCT) pegmatites in Victoria, Australia. Syn-orogenic emplacement of pegmatite dykes occurred along a northwest-trending shear system during the Benambran Orogeny. Pegmatites are derived from fractionated melt associated with the Mount Wills Granite, which is an S-type, peraluminous granite originating from supracrustal melting of Ordovician sedimentary sequences. A distinct, eastward-oriented fractionation trend across the Dorchap Dyke Swarm has highlighted a 20 × 8 km highly fractionated zone in the northeastern Dorchap Range, which includes spodumene- and petalite-bearing pegmatites. A distinct pattern of elemental enrichment (P > Cs > Be > Nb
- Publisher
- Taylor and Francis Ltd.
- Relation
- Australian Journal of Earth Sciences Vol. 70, no. 6 (2023), p. 763-800
- Rights
- All metadata describing materials held in, or linked to, the repository is freely available under a CC0 licence
- Rights
- https://creativecommons.org/licenses/by-nc-nd/4.0/
- Rights
- Copyright © 2023 The Author(s)
- Rights
- Open Access
- Subject
- 41 Environmental Sciences; 51 Physical Sciences; Dorchap Dyke Swarm; Lachlan fold belt; Lithium–caesium–tantalum; Omeo metamorphic complex; Pegmatite
- Full Text
- Reviewed
- Hits: 626
- Visitors: 613
- Downloads: 23
Thumbnail | File | Description | Size | Format | |||
---|---|---|---|---|---|---|---|
View Details Download | SOURCE1 | Published version | 14 MB | Adobe Acrobat PDF | View Details Download |