FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3204328984> ?p ?o ?g. }

• W3204328984 abstract "Abstract A subvolcanic-hydrothermal system involves complex interaction between magma, magmatic fluids, and hydrothermal system at stratovolcanoes in subduction setting. These interactions are responsible for magmatic-hydrothermal eruption associated with rapid injection of magmatic gas into hydrothermal system at a certain depth of volcanic edifice. However, capturing these interactions is challenging due to inaccessibility to the crater conduit within the edifice. Therefore, we selected a method to analyze the volcanic products from several episodic phreatic and phreatomagmatic eruptions during the Holocene at Tangkuban Parahu, Indonesia. In this context, Holocene volcanic products are one of the best examples to understand an interplay between magma, magmatic fluids, and hydrothermal system in producing violent eruptions. In this study, we carried out petrological and sulfur isotope analysis only for the hydrothermally altered lithic ash particles, a part of proximal volcanic products. Mineral assemblages mostly exhibit a typical acid-sulfate and advanced argillic alteration, consisting of alunite, kaolinite, and silica minerals. Acid-sulfate and advanced argillic alteration indicates that those mineral assemblages were formed under the formation temperature ranging from ~100 to ~260 . The calculated temperature from sulfur isotopic fractionation of sulfate-sulfide shows 230-240 , which is almost identical with assigned temperature from mineral assemblages. Sulfur isotope and jarosite occurrence indicate the supergene alteration associated with oxygen entrainment to the hydrothermal system that oxidize pyrite to jarosite. Sulfur isotopic variation throughout the studied stratigraphy represents influx of magmatic gas to the hydrothermal system. Moreover, zoned P-bearing alunite represents repetitive injection of magmatic gas to the active acidic hydrothermal system, which also indicates the magmatic-hydrothermal interaction below the crater. Occurrence of enargite and chalcopyrite represents the nature of upper-level high sulfidation system at shallow volcanic edifice of the Tangkuban Parahu volcano. Furthermore, we showed that coupled petrological and sulfur isotope analysis has paramount importance to evaluate the conditions of the subvolcanic hydrothermal system, magmatic-hydrothermal interaction, and the origin of steam-blast eruptions at volcanoes that contain subvolcanic-hydrothermal systems." @default.
• W3204328984 created "2021-10-11" @default.
• W3204328984 creator A5011939127 @default.
• W3204328984 creator A5032794889 @default.
• W3204328984 creator A5036040439 @default.
• W3204328984 creator A5040036731 @default.
• W3204328984 creator A5089074672 @default.
• W3204328984 date "2021-01-12" @default.
• W3204328984 modified "2023-09-23" @default.
• W3204328984 title "Exploring magmatic gas and subvolcanic hydrothermal system interactions: Mineralogy and sulfur isotope characteristics of the Holocene volcanic products at Mt. Tangkuban Parahu, Indonesia." @default.
• W3204328984 doi "https://doi.org/10.21203/rs.3.rs-141850/v1" @default.
• W3204328984 hasPublicationYear "2021" @default.
• W3204328984 type Work @default.
• W3204328984 sameAs 3204328984 @default.
• W3204328984 citedByCount "0" @default.
• W3204328984 crossrefType "posted-content" @default.
• W3204328984 hasAuthorship W3204328984A5011939127 @default.
• W3204328984 hasAuthorship W3204328984A5032794889 @default.
• W3204328984 hasAuthorship W3204328984A5036040439 @default.
• W3204328984 hasAuthorship W3204328984A5040036731 @default.
• W3204328984 hasAuthorship W3204328984A5089074672 @default.
• W3204328984 hasBestOaLocation W32043289841 @default.
• W3204328984 hasConcept C120806208 @default.
• W3204328984 hasConcept C127313418 @default.
• W3204328984 hasConcept C151730666 @default.
• W3204328984 hasConcept C156622251 @default.
• W3204328984 hasConcept C15785431 @default.
• W3204328984 hasConcept C17409809 @default.
• W3204328984 hasConcept C192241223 @default.
• W3204328984 hasConcept C199289684 @default.
• W3204328984 hasConcept C2775929177 @default.
• W3204328984 hasConcept C2776062231 @default.
• W3204328984 hasConcept C2776222295 @default.
• W3204328984 hasConcept C2781427754 @default.
• W3204328984 hasConcept C92720285 @default.
• W3204328984 hasConceptScore W3204328984C120806208 @default.
• W3204328984 hasConceptScore W3204328984C127313418 @default.
• W3204328984 hasConceptScore W3204328984C151730666 @default.
• W3204328984 hasConceptScore W3204328984C156622251 @default.
• W3204328984 hasConceptScore W3204328984C15785431 @default.
• W3204328984 hasConceptScore W3204328984C17409809 @default.
• W3204328984 hasConceptScore W3204328984C192241223 @default.
• W3204328984 hasConceptScore W3204328984C199289684 @default.
• W3204328984 hasConceptScore W3204328984C2775929177 @default.
• W3204328984 hasConceptScore W3204328984C2776062231 @default.
• W3204328984 hasConceptScore W3204328984C2776222295 @default.
• W3204328984 hasConceptScore W3204328984C2781427754 @default.
• W3204328984 hasConceptScore W3204328984C92720285 @default.
• W3204328984 hasLocation W32043289841 @default.
• W3204328984 hasOpenAccess W3204328984 @default.
• W3204328984 hasPrimaryLocation W32043289841 @default.
• W3204328984 hasRelatedWork W1566110655 @default.
• W3204328984 hasRelatedWork W2019479767 @default.
• W3204328984 hasRelatedWork W2089784784 @default.
• W3204328984 hasRelatedWork W2606209987 @default.
• W3204328984 hasRelatedWork W2802672225 @default.
• W3204328984 hasRelatedWork W2955667102 @default.
• W3204328984 hasRelatedWork W2995785690 @default.
• W3204328984 hasRelatedWork W3158274433 @default.
• W3204328984 hasRelatedWork W3204328984 @default.
• W3204328984 hasRelatedWork W4281937037 @default.
• W3204328984 isParatext "false" @default.
• W3204328984 isRetracted "false" @default.
• W3204328984 magId "3204328984" @default.
• W3204328984 workType "article" @default.