Louise Schoneveld , Walid Salama , Stephen Barnes , Catherine Spaggiari , Margaux Le Vaillant
{"title":"西澳大利亚卡尔皮尼Emu湖科马铁矿岩浆型硫化镍远景区新靶区圈定","authors":"Louise Schoneveld , Walid Salama , Stephen Barnes , Catherine Spaggiari , Margaux Le Vaillant","doi":"10.1016/j.gexplo.2025.107863","DOIUrl":null,"url":null,"abstract":"<div><div>This study tests the use of litho-geochemistry and indicator mineral analysis to delineate new exploration targets within the Emu Lake komatiite-hosted magmatic sulfide prospect within the Archean Eastern Goldfields Superterrane of Western Australia.</div><div>Massive sulfide was recently intercepted at the basal contact of a komatiite unit informally known as the Western ultramafic. The extent of this mineralisation is difficult to track along the ~15 km strike length of the ultramafic sequence due to multiple overlying and underlying barren komatiite flows and significant fault offsets. Whole-rock geochemistry shows that the Western ultramafic unit has distinctly lower Ni/Cr ratios than other ultramafic rocks in the sequence and sits firmly within the 50th percentile of channelised sheet flow komatiitic facies. This Ni/Cr ratio helps distinguish the nickel sulfide-bearing unit from the other komatiitic flows and was used to outline a new target where further drilling was successful in finding sulfide.</div><div>Indicator minerals within the Emu Lake prospect consist of arsenides and chromite. Chromites within the Western ultramafic have lower Ru contents than those within the other ultramafic units, marking interaction between silicate and sulfide melts. Arsenides are also present at Emu Lake and their Pd/Pt values signify arsenic-rich fluids interacted with magmatic sulfide accumulation along shear or fault zones. Surface samples collected above the mineralised area at the Emu Lake prospect contained sulfides (pentlandite and chalcopyrite). Primary sulfides sampled at the surface have the potential to be a powerful ex-situ indicator mineral and could be applied to magmatic sulfide exploration in greenfield terranes.</div></div>","PeriodicalId":16336,"journal":{"name":"Journal of Geochemical Exploration","volume":"278 ","pages":"Article 107863"},"PeriodicalIF":3.3000,"publicationDate":"2025-07-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Delineating new targets in a komatiite-hosted magmatic nickel sulfide prospect - Emu Lake, Kalpini, Western Australia\",\"authors\":\"Louise Schoneveld , Walid Salama , Stephen Barnes , Catherine Spaggiari , Margaux Le Vaillant\",\"doi\":\"10.1016/j.gexplo.2025.107863\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>This study tests the use of litho-geochemistry and indicator mineral analysis to delineate new exploration targets within the Emu Lake komatiite-hosted magmatic sulfide prospect within the Archean Eastern Goldfields Superterrane of Western Australia.</div><div>Massive sulfide was recently intercepted at the basal contact of a komatiite unit informally known as the Western ultramafic. The extent of this mineralisation is difficult to track along the ~15 km strike length of the ultramafic sequence due to multiple overlying and underlying barren komatiite flows and significant fault offsets. Whole-rock geochemistry shows that the Western ultramafic unit has distinctly lower Ni/Cr ratios than other ultramafic rocks in the sequence and sits firmly within the 50th percentile of channelised sheet flow komatiitic facies. This Ni/Cr ratio helps distinguish the nickel sulfide-bearing unit from the other komatiitic flows and was used to outline a new target where further drilling was successful in finding sulfide.</div><div>Indicator minerals within the Emu Lake prospect consist of arsenides and chromite. Chromites within the Western ultramafic have lower Ru contents than those within the other ultramafic units, marking interaction between silicate and sulfide melts. Arsenides are also present at Emu Lake and their Pd/Pt values signify arsenic-rich fluids interacted with magmatic sulfide accumulation along shear or fault zones. Surface samples collected above the mineralised area at the Emu Lake prospect contained sulfides (pentlandite and chalcopyrite). Primary sulfides sampled at the surface have the potential to be a powerful ex-situ indicator mineral and could be applied to magmatic sulfide exploration in greenfield terranes.</div></div>\",\"PeriodicalId\":16336,\"journal\":{\"name\":\"Journal of Geochemical Exploration\",\"volume\":\"278 \",\"pages\":\"Article 107863\"},\"PeriodicalIF\":3.3000,\"publicationDate\":\"2025-07-07\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Geochemical Exploration\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0375674225001955\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geochemical Exploration","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0375674225001955","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Delineating new targets in a komatiite-hosted magmatic nickel sulfide prospect - Emu Lake, Kalpini, Western Australia
This study tests the use of litho-geochemistry and indicator mineral analysis to delineate new exploration targets within the Emu Lake komatiite-hosted magmatic sulfide prospect within the Archean Eastern Goldfields Superterrane of Western Australia.
Massive sulfide was recently intercepted at the basal contact of a komatiite unit informally known as the Western ultramafic. The extent of this mineralisation is difficult to track along the ~15 km strike length of the ultramafic sequence due to multiple overlying and underlying barren komatiite flows and significant fault offsets. Whole-rock geochemistry shows that the Western ultramafic unit has distinctly lower Ni/Cr ratios than other ultramafic rocks in the sequence and sits firmly within the 50th percentile of channelised sheet flow komatiitic facies. This Ni/Cr ratio helps distinguish the nickel sulfide-bearing unit from the other komatiitic flows and was used to outline a new target where further drilling was successful in finding sulfide.
Indicator minerals within the Emu Lake prospect consist of arsenides and chromite. Chromites within the Western ultramafic have lower Ru contents than those within the other ultramafic units, marking interaction between silicate and sulfide melts. Arsenides are also present at Emu Lake and their Pd/Pt values signify arsenic-rich fluids interacted with magmatic sulfide accumulation along shear or fault zones. Surface samples collected above the mineralised area at the Emu Lake prospect contained sulfides (pentlandite and chalcopyrite). Primary sulfides sampled at the surface have the potential to be a powerful ex-situ indicator mineral and could be applied to magmatic sulfide exploration in greenfield terranes.
期刊介绍:
Journal of Geochemical Exploration is mostly dedicated to publication of original studies in exploration and environmental geochemistry and related topics.
Contributions considered of prevalent interest for the journal include researches based on the application of innovative methods to:
define the genesis and the evolution of mineral deposits including transfer of elements in large-scale mineralized areas.
analyze complex systems at the boundaries between bio-geochemistry, metal transport and mineral accumulation.
evaluate effects of historical mining activities on the surface environment.
trace pollutant sources and define their fate and transport models in the near-surface and surface environments involving solid, fluid and aerial matrices.
assess and quantify natural and technogenic radioactivity in the environment.
determine geochemical anomalies and set baseline reference values using compositional data analysis, multivariate statistics and geo-spatial analysis.
assess the impacts of anthropogenic contamination on ecosystems and human health at local and regional scale to prioritize and classify risks through deterministic and stochastic approaches.
Papers dedicated to the presentation of newly developed methods in analytical geochemistry to be applied in the field or in laboratory are also within the topics of interest for the journal.