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Please use this identifier to cite or link to this item: https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/59809
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dc.contributor.authorHolden, DJen_US
dc.date.accessioned2013-10-23T03:50:07Z-
dc.date.issued1990en_US
dc.identifier.govdocCR1990-0142en_US
dc.identifier.urihttps://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/59809en_US
dc.description.abstractIt appears that the tin-tantalum mineralisation is carried in pegmatite veins which are located inside or adjacent to the contact metamorphic andalusite isograd and around the upper greenschist-biotite regional metamorphic isograd. The veins are generally concordant with the major structural features. The overall trend for veining is that it is parallel to the S(1) cleavage.en_US
dc.subject.classificationPegmatiteen_US
dc.subject.classificationTin depositsen_US
dc.subject.classificationTantalumen_US
dc.subject.classificationLiterature reviewsen_US
dc.subject.classificationReinterpretationen_US
dc.subject.classificationGeophysical surveysen_US
dc.subject.classificationStructural geologyen_US
dc.titleAnnual report EL 5687 Bynoe areaen_US
dc.relation.isatmap100Bynoe 5072en_US
dc.relation.isatmap250Darwin SD5204en_US
dc.relation.isatgeolprovincePine Creek Orogenen_US
dc.description.stratnameBurrell Creek Formationen_US
dc.identifier.tenureEL5687en_US
dc.description.modifyhistory02/10/2003en_US
dc.description.modifyhistory26/02/2004en_US
dc.description.modifyhistory21/04/2005en_US
dc.description.modifyhistory24/10/2006en_US
dc.description.modifyhistory09/02/2015en_US
dc.contributor.holderKakadu Resourcesen_US
dc.contributor.holderSirocco Resourcesen_US
dc.identifier.collectionnameMinerals Exploration Reports (MEX)en_US
dc.identifier.govdocprefixCR1990en_US
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Appears in Collections:Minerals Exploration Reports (MEX)

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