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TitreNon-hydrothermal origin of apatite in SEDEX mineralization and host rocks of the Howard's Pass district, Yukon, Canada
AuteurGadd, M G; Layton-Matthews, D; Peter, J M
SourceAmerican Mineralogist vol. 101, 5, 2016 p. 1061-1071, https://doi.org/10.2138/am-2016-5550
Année2016
Séries alt.Ressources naturelles Canada, Contribution externe 20182477
ÉditeurWalter de Gruyter GmbH
Documentpublication en série
Lang.anglais
DOIhttps://doi.org/10.2138/am-2016-5550
Mediapapier; en ligne; numérique
ProvinceYukon
ProgrammeSystèmes volcaniques et sédimentaires, Initiative géoscientifique ciblée (IGC-5)
Diffusé2016 05 02
Résumé(disponible en anglais seulement)
The Howard's Pass district (HPD) comprises 14 Zn-Pb sedimentary exhalative (SEDEX) deposits and is located within the Selwyn basin, Yukon, Canada. Although the HPD is renowned for its large accumulation of base-metal sulfides, in places the Late Ordovician to Early Silurian host rocks also contain abundant carbonate-bearing fluorapatite (CBFA). This mineral is present stratigraphically below, within, and above the SEDEX deposits and occurs as fine-grained layers that are interbedded with cherty carbonaceous mudstone. Electron probe microanalysis and laser ablation-inductively coupled plasma-mass spectrometric analysis reveal that mineral compositions and rare earth element-yttrium (REE-Y) systematics, respectively, are remarkably similar throughout the stratigraphic succession. North American Shale Composite (NASC)-normalized La/Sm and La/Yb ratios indicate that the original REE compositions in CBFA have undergone only minor compositional modification subsequent to deposition. Uniformly negative Ce anomalies indicate that the mineral formed in analogous manner to modern and ancient sedimentary phosphorites under suboxic bottom-water conditions. Europium anomalies are mostly absent, indicating that reduced, slightly acidic high-temperature hydrothermal fluids were not a major source of REE-Y to CBFA. The chemical homogeneity of the mineral irrespective of its stratigraphic position indicates that a common process was responsible for its deposition within the sedimentary rocks of the HPD. On the basis of the similarity of the REE patterns to modern and ancient phosphorites, and the absence of positive Eu anomalies, we conclude that the CBFA is of hydrogenous origin, and not hydrothermal as suggested by previous workers. As such, phosphorite formation in the HPD is casually related to SEDEX Zn-Pb deposit formation. © 2016 by Walter de Gruyter Berlin/Boston 2016.
GEOSCAN ID311068