Item talk:Q266197
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{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Calc-alkaline, shoshonitic, and primitive tholeiitic lavas from monogenetic volcanoes near Crater Lake, Oregon", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70200575", "url": "https://pubs.usgs.gov/publication/70200575" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70200575 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1093/petrology/31.1.135", "url": "https://doi.org/10.1093/petrology/31.1.135" } ], "journal": { "@type": "Periodical", "name": "Journal of Petrology", "volumeNumber": "31", "issueNumber": "1" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Journal of Petrology" } ], "datePublished": "1990", "dateModified": "2018-10-24", "abstract": "Quaternary monogenetic volcanism in the High Cascades of Oregon is manifested by cinder cones, lava fields, and small shields. Near Crater Lake caldera, monogenetic lava compositions include: low-K (as low as 0\u00b709% K2O) high-alumina olivine tholeiite (HAOT); medium-K. calc-alkaline basalt, basaltic andesite, and andesite; and shoshonitic basaltic andesite (2\u00b71% K2O, 1750 ppm Sr at 54% SiO2). Tholeiites have MORB-like trace element abundances except for elevated Sr, Ba, and Th and low high field strength elements (HFSE), and they represent near-primary liquids. They are similar to HAOTs from the Cascades and adjacent Basin and Range, and to many primitive basalts from intraoceanic arcs. Calc-alkaline lavas show a well-developed arc signature of high large-ion lithophile elements (LILE) and low HFSE. Their Zr and Hf concentrations are at least partly decoupled from those of Nb and Ta; HREE are low relative to HAOT. Incompatible element abundances and ratios vary widely among basaltic andesites. Some calc-alkaline lavas vented near Mount Mazama contain abundant gabbroic microxcnoliths, and are basaltic andesitic magmas contaminated with olivine gabbro.A calc-alkaline basalt and a few basaltic andesites have MgO and compatible trace element contents that suggest only minor fractionation. There appears to be a compositional continuum between primitive tholeiitic and calc-alkaline lavas. Compositional variation within suites of comagmatic primitive lavas, both tholeiitic and calc-alkaline, mainly results from different degrees of partial melting. Sources of calc-alkaline primary magmas were enriched in LILE and LREE by a subduction component and contained residual garnet, whereas sources of HAOTs had lower LILE and LREE concentrations and contained residual clinopyroxene. High and variable LILE and LREE contents of calc-alkaline lavas reflect variations in fluid-transported subduction component added to the mantle wedge, degree of partial melting, and possibly also interaction with rocks or partial melts in the lower crust.Andesites were derived from calc-alkaline basaltic andesites by fractionation of plagioclase+augite+magnetite+apatite \u00b1 orthopyroxene or olivine, commonly accompanied by assimilation. Many andesites are mixtures of andesitic or dacitic magma and a basaltic or basaltic andesitic component, or are contaminated with gabbroic material. Mingled basalt, andesite, and dacite of Williams Crater formed by multi-component, multi-stage mixing of basaltic andesitic magma, gabbro, and dacitic magma. The wide range of compositions vented from monogenetic volcanoes near Crater Lake is a result of the thick crust coupled with mild tectonic extension superimposed on a subduction-related magmatic arc.", "description": "32 p.", "publisher": { "@type": "Organization", "name": "Oxford Academic" }, "author": [ { "@type": "Person", "name": "Bacon, Charles R. cbacon@usgs.gov", "givenName": "Charles R.", "familyName": "Bacon", "email": "cbacon@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-2165-5618", "url": "https://orcid.org/0000-0002-2165-5618" }, "affiliation": [ { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ] } ], "funder": [ { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ], "spatialCoverage": [ { "@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/4074035" }, { "@type": "Place", "additionalType": "state", "name": "Oregon" } ] }, "OpenAlex": { "_id": "https://openalex.org/w2327734254", "abstract_inverted_index": { "Quaternary": [ 0 ], "monogenetic": [ 1, 23, 363 ], "volcanism": [ 2 ], "in": [ 3, 230, 268, 290 ], "the": [ 4, 87, 274, 291, 372 ], "High": [ 5, 256 ], "Cascades": [ 6, 88 ], "of": [ 7, 109, 130, 207, 220, 224, 244, 263, 278, 303, 317, 340, 348, 359, 371 ], "Oregon": [ 8 ], "is": [ 9, 368 ], "manifested": [ 10 ], "by": [ 11, 234, 301, 311, 344 ], "cinder": [ 12 ], "cones,": [ 13 ], "lava": [ 14, 24 ], "fields,": [ 15 ], "and": [ 16, 42, 44, 67, 69, 76, 89, 92, 94, 115, 120, 132, 143, 161, 173, 180, 200, 213, 232, 238, 249, 252, 257, 260, 281, 322, 338, 353 ], "small": [ 17 ], "shields.": [ 18 ], "Near": [ 19 ], "Crater": [ 20, 342, 366 ], "Lake": [ 21, 367 ], "caldera,": [ 22 ], "compositions": [ 25, 360 ], "include:": [ 26 ], "low-K": [ 27 ], "(as": [ 28 ], "low": [ 29, 70, 116, 136 ], "as": [ 30 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