Flat vein formation in a transitional crustal setting by self-induced fluid pressure equilibrium — an example from the Géant Dormant gold mine, Canada
- DOI
- 10.1016/s0169-1368(00)00012-3
- Published
- 2000-12
- Container
- Ore Geology Reviews
- Publisher
- Elsevier BV
- Open access
- unknown
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Cite this work
BibTeX
@article{allodium:10.1016/s0169-1368-00-00012-3,
title = {Flat vein formation in a transitional crustal setting by self-induced fluid pressure equilibrium — an example from the Géant Dormant gold mine, Canada},
author = {Damien Gaboury and Réal Daigneault},
year = {2000},
journal = {Ore Geology Reviews},
doi = {10.1016/s0169-1368(00)00012-3},
url = {https://doi.org/10.1016/s0169-1368(00)00012-3}
}RIS
TY - JOUR TI - Flat vein formation in a transitional crustal setting by self-induced fluid pressure equilibrium — an example from the Géant Dormant gold mine, Canada AU - Damien Gaboury AU - Réal Daigneault PY - 2000 JO - Ore Geology Reviews DO - 10.1016/s0169-1368(00)00012-3 UR - https://doi.org/10.1016/s0169-1368(00)00012-3 ER -
APA
Gaboury, D., & Daigneault, R. (2000). Flat vein formation in a transitional crustal setting by self-induced fluid pressure equilibrium — an example from the Géant Dormant gold mine, Canada. Ore Geology Reviews. https://doi.org/10.1016/s0169-1368(00)00012-3
Source records
- crossref · retrieved 2026-09-26T15:00:06.856Z