{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1363670320117799040.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.277.5332.1639"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.277.5332.1639"}}],"dc:title":[{"@value":"Explosive Basaltic Volcanism from Cerro Negro Volcano: Influence of Volatiles on Eruptive Style"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The 1992 and 1995 basaltic eruptions of Cerro Negro volcano, Nicaragua, had contrasting eruptive styles. Although they were nearly identical in composition, the 1992 eruption was explosive, producing a 7-kilometer-high sustained ash column, whereas the 1995 eruption was essentially effusive. The differences in water and carbon dioxide contents of melt inclusions from the two eruptions define minimum saturation pressures and show how decompression of initially similar magmas influences eruptive style. Before eruption, the explosive 1992 magma retained water and carbon dioxide while ascending to a moderate crustal level (about 6 kilometers), whereas the nonexplosive 1995 magma lost all carbon dioxide by degassing during ascent to shallow crustal levels (about 1 to 2 kilometers).</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320117799040","@type":"Researcher","foaf:name":[{"@value":"Kurt Roggensack"}],"jpcoar:affiliationName":[{"@value":"Department of Geology, Box 871404, Arizona State University, Tempe, AZ 85287–1404, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320117799041","@type":"Researcher","foaf:name":[{"@value":"Richard L. Hervig"}],"jpcoar:affiliationName":[{"@value":"Department of Geology, Box 871404, Arizona State University, Tempe, AZ 85287–1404, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320117799042","@type":"Researcher","foaf:name":[{"@value":"Steven B. McKnight"}],"jpcoar:affiliationName":[{"@value":"Department of Geology, Box 871404, Arizona State University, Tempe, AZ 85287–1404, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320117799043","@type":"Researcher","foaf:name":[{"@value":"Stanley N. Williams"}],"jpcoar:affiliationName":[{"@value":"Department of Geology, Box 871404, Arizona State University, Tempe, AZ 85287–1404, USA."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"1997-09-12","prism:volume":"277","prism:number":"5332","prism:startingPage":"1639","prism:endingPage":"1642"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.277.5332.1639"}],"createdAt":"2002-07-27","modifiedAt":"2024-01-13","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004231230385792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A petrological and geochemical study on time-series samples from Klyuchevskoy volcano, Kamchatka arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707326396544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fluid-fluxed melting of mantle versus decompression melting of hydrous mantle plume as the cause of intraplate magmatism over a stagnant slab: Implications from Fukue Volcano Group, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165287872640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Water content of primitive low-K tholeiitic basalt magma from Iwate Volcano, NE Japan arc: implications for differentiation mechanism of frontal-arc basalt magmas"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567180128612352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Switching between seismic and seismo‐acoustic harmonic tremor simulated in the laboratory: Insights into the role of open degassing channels and magma viscosity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181183669760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Primary melt from Sannome-gata volcano, NE Japan arc: constraints on generation conditions of rear-arc magmas"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182004466560","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Bromine speciation in hydrous silicate melts at high pressure"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232392375936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magmatic evolution and metal systematics of back-arc volcanic rocks of north–east Japan and implications for deposition of massive sulphide Kuroko ores"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657272722176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Volatile flux from subduction zone volcanoes: Insights from a detailed evaluation of the fluxes from volcanoes in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567481481728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Persistent gas emission originating from a deep basaltic magma reservoir of an active volcano: the case of Aso volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204228572288","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Physical and Chemical Diversity of Seafloor Hydrothermal Systems and Presentation of Associated Chemolithoautotrophic Ecosystem"},{"@language":"ja","@value":"海底熱水系の物理・化学的多様性と化学合成微生物生態系の存在様式"},{"@language":"ja-Kana","@value":"カイテイ ネッスイケイ ノ ブツリ カガクテキ タヨウセイ ト カガク ゴウセイ ビセイブツ セイタイケイ ノ ソンザイ ヨウシキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204551620352","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fluxes of volatiles (H2O, CO2, N2, Cl, F) from arc volcanoes"},{"@value":"Volatile fluxes (H2O, CO2, N2, HCl, HF) from arc volcanoes"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681502126336","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of H2O concentration in primary arc magmas: constraints from melting experiments and analyses of melt inclusions"},{"@language":"ja","@value":"島弧における初生マグマの含水量の推定：実験岩石学とメルト包有物分析からの制約"},{"@language":"ja-Kana","@value":"トウコ ニ オケル ショセイ マグマ ノ ガン スイリョウ ノ スイテイ ジッケン ガンセキガク ト メルト ホウユウブツ ブンセキ カラ ノ セイヤク"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046927360","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Large-ion lithophile elements delivered by saline fluids to the sub-arc mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996267023632256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A new technique using FT-IR micro-reflectance spectroscopy for measurement of water concentrations in melt inclusions"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.277.5332.1639"},{"@type":"CROSSREF","@value":"10.1007/s00410-017-1347-z_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-61_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2017.02.011_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.2465/gkk.110131a_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1007/s00710-013-0278-2_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-34_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1002/jgrb.50067_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1007/s00410-014-0969-7_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1016/j.jvolgeores.2013.10.007_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1007/s00410-022-01980-z_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.5026/jgeography.118.1083_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1007/s00410-020-01761-6_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2015.03.015_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"},{"@type":"CROSSREF","@value":"10.2343/geochemj.42.21_references_DOI_MvSBIhosKC4HcA6q02saRmPs9e7"}]}