Sm-Nd and REE characteristics of tourmaline and scheelite from the Bjorkdal gold deposit, northern Sweden: evidence of an intrusion-related gold deposit?
Sm-Nd and REE characteristics of tourmaline and scheelite from the Bjorkdal gold deposit, northern Sweden: evidence of an intrusion-related gold deposit?
The Björkdal quartz vein-hosted gold deposit is located ~25 km northwest of Skellefte in northern Sweden, within a Paleoproterozoic volcanosedimentary sequence at the margin of a quartz-monzodiorite granitoid. Northeast-trending (030°– 050°) quartz veins from the eastern open pit within the Björkdal deposit contain quartz, scheelite, tourmaline, calcite, and sulfides, with visible gold. Vein quartz shows undulatory extinction and sutured margins or is polycrystalline in form, features which suggest postcrystallization deformation. Coarse scheelite crystals (>5 mm) within the quartz veins are crosscut by thin veins of quartz, calcite, sulfides, and gold. The calcite in these crosscutting fractures is variably replaced by biotite or actinolite. Tourmaline from the quartz veins has low total REE contents (<1 × chondrite) and LREE-enriched patterns [(La/Sm) N = 2.8–4.5, (La/Yb)N = 1.8–5.1] with strong positive Eu anomalies (Eu/Eu* = 3.9–17.4). In contrast, the scheelite has a bell-shaped REE pattern, enriched in MREE, but also with positive Eu anomalies (Eu/Eu* = 1.4–2.4). The REE pattern of scheelite results from a strong crystallographic effect, largely due to the size of the Ca site and charge balance. Sm-Nd dating of scheelite from the Björkdal ore yields an age of 1893 ± 34 Ma, which coincides with a previously suggested age of the host intrusion. The ?Nd values of the scheelite (+1.8) and 87Sr/86Sr
initial ratios of the tourmaline (0.7013–0.7014) are also consistent with derivation of REE and Sr in these minerals from the Jörn granitoids. Overall, the petrographic, geochemical, and isotopic data strongly suggest that Björkdal is an intrusion-related gold deposit, and that there is no requirement for involvement of external postmagmatic hydrothermal fluids.
1415-1425
Roberts, S.
f095c7ab-a37b-4064-8a41-ae4820832856
Palmer, M.R.
d2e60e81-5d6e-4ddb-a243-602537286080
Waller, L.
1b66030e-2844-45a5-b7a0-bcaf6d4e6ca9
2006
Roberts, S.
f095c7ab-a37b-4064-8a41-ae4820832856
Palmer, M.R.
d2e60e81-5d6e-4ddb-a243-602537286080
Waller, L.
1b66030e-2844-45a5-b7a0-bcaf6d4e6ca9
Roberts, S., Palmer, M.R. and Waller, L.
(2006)
Sm-Nd and REE characteristics of tourmaline and scheelite from the Bjorkdal gold deposit, northern Sweden: evidence of an intrusion-related gold deposit?
Economic Geology, 101 (7), .
Abstract
The Björkdal quartz vein-hosted gold deposit is located ~25 km northwest of Skellefte in northern Sweden, within a Paleoproterozoic volcanosedimentary sequence at the margin of a quartz-monzodiorite granitoid. Northeast-trending (030°– 050°) quartz veins from the eastern open pit within the Björkdal deposit contain quartz, scheelite, tourmaline, calcite, and sulfides, with visible gold. Vein quartz shows undulatory extinction and sutured margins or is polycrystalline in form, features which suggest postcrystallization deformation. Coarse scheelite crystals (>5 mm) within the quartz veins are crosscut by thin veins of quartz, calcite, sulfides, and gold. The calcite in these crosscutting fractures is variably replaced by biotite or actinolite. Tourmaline from the quartz veins has low total REE contents (<1 × chondrite) and LREE-enriched patterns [(La/Sm) N = 2.8–4.5, (La/Yb)N = 1.8–5.1] with strong positive Eu anomalies (Eu/Eu* = 3.9–17.4). In contrast, the scheelite has a bell-shaped REE pattern, enriched in MREE, but also with positive Eu anomalies (Eu/Eu* = 1.4–2.4). The REE pattern of scheelite results from a strong crystallographic effect, largely due to the size of the Ca site and charge balance. Sm-Nd dating of scheelite from the Björkdal ore yields an age of 1893 ± 34 Ma, which coincides with a previously suggested age of the host intrusion. The ?Nd values of the scheelite (+1.8) and 87Sr/86Sr
initial ratios of the tourmaline (0.7013–0.7014) are also consistent with derivation of REE and Sr in these minerals from the Jörn granitoids. Overall, the petrographic, geochemical, and isotopic data strongly suggest that Björkdal is an intrusion-related gold deposit, and that there is no requirement for involvement of external postmagmatic hydrothermal fluids.
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Published date: 2006
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Local EPrints ID: 46095
URI: http://eprints.soton.ac.uk/id/eprint/46095
ISSN: 0361-0128
PURE UUID: dc92c411-afbe-451b-9869-b0390b3eb649
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Date deposited: 22 May 2007
Last modified: 19 Mar 2022 02:33
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L. Waller
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