Rapport fra prospekteringsarbeider i Bidjovagge - 1996, HMC - 1996 Report - Bidjovagge Prosjekt, Part I - 1996 Exploration Summary
Bedrift BCLX Consulting Ltd, Norway Gold Exploration, Geologiske Tjenester
- Geografi
- Kautokeino
- Geometri
- Punktgeometri
- Publisert
- Kildestatus
- Publisert
Registrert posisjon
Interaktiv kartflate · Punktgeometri
Punktsymbol, ikke område. Markøren gjør kildepunktet mulig å finne og fokusere; den representerer ingen utstrekning.
Geometri: © DMF. Bakgrunnskart: © OpenStreetMap-bidragsytere. NGU-forekomster kan vises som kontekst og dokumenterer ikke reserve, kvalitet eller drivverdighet. Kartet viser et regulatorisk/geografisk kildeobjekt, ikke underjordisk utstrekning.
Eksakte kildefelt
Fraværende valgfrie felt blir ikke erstattet med dekorasjon eller antakelser.
- Rapportnummer
- BV4565
- Register
- Undersøkelsesrapporter
- Status hos DMF
- Publisert
- Mottatt
- Forfatter
- Pierce, Garth
- Bedrift
- BCLX Consulting Ltd, Norway Gold Exploration, Geologiske Tjenester
- Kommune
- Kautokeino
- Fylke
- Finnmark
- Sammendrag
- Table # 3 gives a list of drill results as reported by HMC in it's public releases . Detailed drill data including summary drill logs, assays, sections and field logs are included as Appendixes # 2 a,b,c and d. The 1996 drill program failed to delineate any significant new zones of near surface mineralization. Copper and gold values were however widespread and the alteration system is extensive. Drill holes such as 96-13 show the tenor of the mineralization that still remains to be tested near surface. Deeper intercepts such as those in 96-1, 96-5 and 96-11 indicate the potential for deeper zones of mineralization at Bidjovagge. For the most part the Bidjovagge ore zones are poorly tested below 150 meters. The style of mineralization at Bidjovagge is fairly unique and can best be described as fracture controlled sulfide ores which most commonly take on a stockwork appearance. The mineralization is best developed as replacement zones superimposed on a highly altered calcareous sedimentary succession.Within this stratigraphy copper -gold ores are spatially related to graphitic horizons and in some instances the best ores appear to be zones of intense alteration where these graphite beds have been completely replaced to sodium rich felsites . The mineralizing processes may in part be related to the mafic dike suite, principally alkaline gabbro and diabase sills, which intude the host rocks. The ores do however show some features which are more characteristic of skarn or contact replacement copper - gold mineralization related to diorite or syenodiorite intrusions . At Bidjovagge such intrusives would have to be at depth and future exploration should at least consider this potential. The ores exposed at surface,could simply cap a more extensive hydrothermal cell at depth . The ore forming processes at Bidjovagge are extensive and appear to go to depth; further drilling is therefore strongly recommended. Se også BV 4566, BV 4567 og BV 4568
- Rapport hos DMF
- Åpne rapport
Direktoratet for mineralforvaltning
Objektet kommer fra datasettet «Undersøkelsesrapporter» og vises med kildegeometrien uendret i betydning.
Hva objektet ikke dokumenterer
Oppføringen dokumenterer at DMF har publisert rapportmetadata. Kartet viser DMFs egne rapportpunkter, ikke rapportens fulle undersøkelsesområde. Mineralradar tolker ikke PDF-innholdet og utleder ikke ny aktivitet, funn, reserve, kvalitet eller økonomisk potensial fra rapporten.
Regulatorisk kronologi
Kildedato og Radar-observasjon beholdes som ulike tidssemantikker.
Ingen senere endringer observert
Objektets nåtilstand er tilgjengelig, men historikken inneholder ingen hendelser etter baseline.