Item talk:Q273322
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Scientific communications: Re-Os sulfide (bornite, chalcopyrite, and pyrite) systematics of the carbonate-hosted copper deposits at ruby creek, southern brooks range, Alaska", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70034769", "url": "https://pubs.usgs.gov/publication/70034769" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70034769 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.2113/gsecongeo.104.3.437", "url": "https://doi.org/10.2113/gsecongeo.104.3.437" }, { "@type": "PropertyValue", "propertyID": "ISSN", "value": "03610128" } ], "journal": { "@type": "Periodical", "name": "Economic Geology", "volumeNumber": "104", "issueNumber": "3" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Economic Geology" } ], "datePublished": "2009", "dateModified": "2012-03-12", "abstract": "New Re-Os data for chalcopyrite, bornite, and pyrite from the carbonate-hosted Cu deposit at Ruby Creek (Bornite), Alaska, show extremely high Re abundances (hundreds of ppb, low ppm) and contain essentially no common Os. The Re-Os data provide the first absolute ages of ore formation for the carbonate-hosted Ruby Creek Cu-(Co) deposit and demonstrate that the Re-Os systematics of pyrite, chalcopyrite, and bornite are unaffected by greenschist metamorphism. The Re-Os data show that the main phase of Cu mineralization pre dominantly occurred at 384 ?? 4.2 Ma, with an earlier phase possibly at ???400 Ma. The Re-Os data are consistent with the observed paragenetic sequence and coincide with zircon U-Pb ages from igneous rocks within the Ambler metallogenic belt, some of which are spatially and genetically associated with regional volcanogenic massive sulfide deposits. The latter may suggest a temporal link between regional magmatism and hydrothermal mineralization in the Ambler district. The utility of bornite and chalcopyrite, in addition to pyrite, contributes to a new understanding of Re-Os geochronology and permits a refinement of the genetic model for the Ruby Creek deposit. ?? 2009 Society of Economices Geologists, Inc.", "publisher": { "@type": "Organization", "name": "U.S. Geological Survey" }, "author": [ { "@type": "Person", "name": "Selby, D.", "givenName": "D.", "familyName": "Selby" }, { "@type": "Person", "name": "Kelley, K. D.", "givenName": "K. D.", "familyName": "Kelley", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-3232-5809", "url": "https://orcid.org/0000-0002-3232-5809" } }, { "@type": "Person", "name": "Zieg, J.", "givenName": "J.", "familyName": "Zieg" }, { "@type": "Person", "name": "Hitzman, M.W.", "givenName": "M.W.", "familyName": "Hitzman" } ] }, "OpenAlex": { "_id": "https://openalex.org/W2068493056", "abstract_inverted_index": { "New": [ 0 ], "Re-Os": [ 1, 35, 56, 69, 95, 165 ], "data": [ 2, 36, 70, 96 ], "for": [ 3, 45, 175 ], "chalcopyrite,": [ 4, 60, 154 ], "bornite,": [ 5 ], "and": [ 6, 28, 52, 61, 104, 123, 142, 153, 167 ], "pyrite": [ 7 ], "from": [ 8, 110 ], "the": [ 9, 38, 46, 55, 73, 100, 114, 146, 172, 176 ], "carbonate-hosted": [ 10, 47 ], "Cu": [ 11, 77 ], "deposit": [ 12, 51 ], "at": [ 13, 81, 91 ], "Ruby": [ 14, 48, 177 ], "Creek": [ 15, 49, 178 ], "(Bornite),": [ 16 ], "Alaska,": [ 17 ], "show": [ 18, 71 ], "extremely": [ 19 ], "high": [ 20 ], "Re": [ 21 ], "abundances": [ 22 ], "(hundreds": [ 23 ], "of": [ 24, 42, 58, 76, 119, 151, 164, 171 ], "ppb,": [ 25 ], "low": [ 26 ], "ppm)": [ 27 ], "contain": [ 29 ], "essentially": [ 30 ], "no": [ 31 ], "common": [ 32 ], "Os.": [ 33 ], "The": [ 34, 68, 94, 132, 149 ], "provide": [ 37 ], "first": [ 39 ], "absolute": [ 40 ], "ages": [ 41, 109 ], "ore": [ 43 ], "formation": [ 44 ], "Cu-(Co)": [ 50 ], "demonstrate": [ 53 ], "that": [ 54, 72 ], "systematics": [ 57 ], "pyrite,": [ 59, 158 ], "bornite": [ 62, 152 ], "are": [ 63, 97, 121 ], "unaffected": [ 64 ], "by": [ 65 ], "greenschist": [ 66 ], "metamorphism.": [ 67 ], "main": [ 74 ], "phase": [ 75, 89 ], "mineralization": [ 78, 144 ], "predominantly": [ 79 ], "occurred": [ 80 ], "384": [ 82 ], "\u00b1": [ 83 ], "4.2": [ 84 ], "Ma,": [ 85 ], "with": [ 86, 99, 106, 126 ], "an": [ 87 ], "earlier": [ 88 ], "possibly": [ 90 ], "~400": [ 92 ], "Ma.": [ 93 ], "consistent": [ 98 ], "observed": [ 101 ], "paragenetic": [ 102 ], "sequence": [ 103 ], "coincide": [ 105 ], "zircon": [ 107 ], "U-Pb": [ 108 ], "igneous": [ 111 ], "rocks": [ 112 ], "within": [ 113 ], "Ambler": [ 115, 147 ], "metallogenic": [ 116 ], "belt,": [ 117 ], "some": [ 118 ], "which": [ 120 ], "spatially": [ 122 ], "genetically": [ 124 ], "associated": [ 125 ], "regional": [ 127, 140 ], "volcanogenic": [ 128 ], "massive": [ 129 ], "sulfide": [ 130 ], "deposits.": [ 131 ], "latter": [ 133 ], "may": [ 134 ], "suggest": [ 135 ], "a": [ 136, 161, 169 ], "temporal": [ 137 ], "link": [ 138 ], "between": [ 139 ], "magmatism": [ 141 ], "hydrothermal": [ 143 ], "in": [ 145, 155 ], "district.": [ 148 ], "utility": [ 150 ], "addition": [ 156 ], "to": [ 157, 160 ], "contributes": [ 159 ], "new": [ 162 ], "understanding": [ 163 ], "geochronology": [ 166 ], "permits": [ 168 ], "refinement": [ 170 ], "genetic": [ 173 ], "model": [ 174 ], "deposit.": [ 179 ] }, "apc_list": null, "apc_paid": null, "authorships": [ { "author_position": "first", "author": { "id": "https://openalex.org/A5081959981", "display_name": "David Selby", "orcid": "https://orcid.org/0000-0001-9798-2351" }, "institutions": [ { "id": "https://openalex.org/I190082696", "display_name": "Durham University", "ror": "https://ror.org/01v29qb04", "country_code": "GB", "type": "education", "lineage": [ "https://openalex.org/I190082696" ] } ], "countries": [ "GB" ], "is_corresponding": false, "raw_author_name": "D. 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