FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1877444998> ?p ?o ?g. }

• W1877444998 endingPage "1209" @default.
• W1877444998 startingPage "1198" @default.
• W1877444998 abstract "Other| December 01, 1997 Experimental study of the system phlogopite-diopside from 3.5 to 17 GPa Robert W. Luth Robert W. Luth University of Alberta, Department of Earth and Atmospheric Sciences, Edmonton, AB, Canada Search for other works by this author on: GSW Google Scholar American Mineralogist (1997) 82 (11-12): 1198–1209. https://doi.org/10.2138/am-1997-11-1216 Article history first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Robert W. Luth; Experimental study of the system phlogopite-diopside from 3.5 to 17 GPa. American Mineralogist 1997;; 82 (11-12): 1198–1209. doi: https://doi.org/10.2138/am-1997-11-1216 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search nav search search input Search input auto suggest search filter All ContentBy SocietyAmerican Mineralogist Search Advanced Search Abstract On the basis of both natural samples and experimental studies, clinopyroxene is a potential reservoir for potassium in the Earth’s mantle. The amount of K partitioning into clinopyroxene depends on the phase assemblage present, the bulk composition, pressure, and temperature. To investigate some of these dependencies, subsolidus and melting phase relations in the system phlogopite-diopside have been studied to 17 GPa. In this system, phlogopite becomes unstable with increasing pressure, breaking down to potassium richterite, which in turn breaks down to another K-bearing hydrous phase (phase X), such that a K-rich phase coexists with clinopyroxene to 17 GPa. Clinopyroxenes contain ≤1.3 wt% K2O in assemblages of phlogopite + clinopyroxene ± olivine ± liquid at 3–5 GPa, phlogopite + clinopyroxene + garnet ± olivine ± liquid at 7–9 GPa, clinopyroxene + garnet + olivine ± potassium richterite ± liquid at 11 GPa, and clinopyroxene + olivine + garnet + phase X at 14 and 17 GPa.In these assemblages, K is partitioned into hydrous phases or liquid, rather than into the clinopyroxene. By inference, phlogopite (or its higher-pressure breakdown products) is the primary host for K in the mantle (if H2O is present), and any coexisting clinopyroxene has very low concentrations of K. Conversely, the natural occurrence of clinopyroxene with >> 1 wt% K2O requires that phlogopite, potassium richterite, or phase X is not stable in the local source environment of such samples. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article." @default.
• W1877444998 created "2016-06-24" @default.
• W1877444998 creator A5072706704 @default.
• W1877444998 date "1997-12-01" @default.
• W1877444998 modified "2023-10-16" @default.
• W1877444998 title "Experimental study of the system phlogopite-diopside from 3.5 to 17 GPa" @default.
• W1877444998 cites W121579099 @default.
• W1877444998 cites W1965658370 @default.
• W1877444998 cites W1969859799 @default.
• W1877444998 cites W1970767963 @default.
• W1877444998 cites W1975757281 @default.
• W1877444998 cites W1978393671 @default.
• W1877444998 cites W1981344517 @default.
• W1877444998 cites W1989092054 @default.
• W1877444998 cites W1990722868 @default.
• W1877444998 cites W1990740187 @default.
• W1877444998 cites W1996951608 @default.
• W1877444998 cites W1998937825 @default.
• W1877444998 cites W2004307298 @default.
• W1877444998 cites W2012367671 @default.
• W1877444998 cites W2015357291 @default.
• W1877444998 cites W2016056728 @default.
• W1877444998 cites W2022390096 @default.
• W1877444998 cites W2029411395 @default.
• W1877444998 cites W2030114314 @default.
• W1877444998 cites W2030800261 @default.
• W1877444998 cites W2036689902 @default.
• W1877444998 cites W2041584645 @default.
• W1877444998 cites W2047963618 @default.
• W1877444998 cites W2048506031 @default.
• W1877444998 cites W2056122128 @default.
• W1877444998 cites W2057834112 @default.
• W1877444998 cites W2074002285 @default.
• W1877444998 cites W2081514820 @default.
• W1877444998 cites W2096684208 @default.
• W1877444998 cites W2252547811 @default.
• W1877444998 cites W2258570876 @default.
• W1877444998 cites W2314985557 @default.
• W1877444998 cites W2469766991 @default.
• W1877444998 cites W2581664821 @default.
• W1877444998 cites W564400156 @default.
• W1877444998 cites W598528115 @default.
• W1877444998 cites W91897106 @default.
• W1877444998 doi "https://doi.org/10.2138/am-1997-11-1216" @default.
• W1877444998 hasPublicationYear "1997" @default.
• W1877444998 type Work @default.
• W1877444998 sameAs 1877444998 @default.
• W1877444998 citedByCount "123" @default.
• W1877444998 countsByYear W18774449982012 @default.
• W1877444998 countsByYear W18774449982013 @default.
• W1877444998 countsByYear W18774449982014 @default.
• W1877444998 countsByYear W18774449982015 @default.
• W1877444998 countsByYear W18774449982016 @default.
• W1877444998 countsByYear W18774449982017 @default.
• W1877444998 countsByYear W18774449982018 @default.
• W1877444998 countsByYear W18774449982019 @default.
• W1877444998 countsByYear W18774449982020 @default.
• W1877444998 countsByYear W18774449982021 @default.
• W1877444998 countsByYear W18774449982022 @default.
• W1877444998 countsByYear W18774449982023 @default.
• W1877444998 crossrefType "journal-article" @default.
• W1877444998 hasAuthorship W1877444998A5072706704 @default.
• W1877444998 hasConcept C127313418 @default.
• W1877444998 hasConcept C161191863 @default.
• W1877444998 hasConcept C17409809 @default.
• W1877444998 hasConcept C199289684 @default.
• W1877444998 hasConcept C2777018398 @default.
• W1877444998 hasConcept C2778805511 @default.
• W1877444998 hasConcept C2778882853 @default.
• W1877444998 hasConcept C41008148 @default.
• W1877444998 hasConcept C67236022 @default.
• W1877444998 hasConceptScore W1877444998C127313418 @default.
• W1877444998 hasConceptScore W1877444998C161191863 @default.
• W1877444998 hasConceptScore W1877444998C17409809 @default.
• W1877444998 hasConceptScore W1877444998C199289684 @default.
• W1877444998 hasConceptScore W1877444998C2777018398 @default.
• W1877444998 hasConceptScore W1877444998C2778805511 @default.
• W1877444998 hasConceptScore W1877444998C2778882853 @default.
• W1877444998 hasConceptScore W1877444998C41008148 @default.
• W1877444998 hasConceptScore W1877444998C67236022 @default.
• W1877444998 hasIssue "11-12" @default.
• W1877444998 hasLocation W18774449981 @default.
• W1877444998 hasOpenAccess W1877444998 @default.
• W1877444998 hasPrimaryLocation W18774449981 @default.
• W1877444998 hasRelatedWork W1963499998 @default.
• W1877444998 hasRelatedWork W2023967750 @default.
• W1877444998 hasRelatedWork W2057871327 @default.
• W1877444998 hasRelatedWork W2072250941 @default.
• W1877444998 hasRelatedWork W2101513265 @default.
• W1877444998 hasRelatedWork W2143639303 @default.
• W1877444998 hasRelatedWork W2161120573 @default.
• W1877444998 hasRelatedWork W2924778358 @default.
• W1877444998 hasRelatedWork W2966395559 @default.
• W1877444998 hasRelatedWork W3021404025 @default.
• W1877444998 hasVolume "82" @default.
• W1877444998 isParatext "false" @default.
• W1877444998 isRetracted "false" @default.
• W1877444998 magId "1877444998" @default.

• next