Matches in SemOpenAlex for { <https://semopenalex.org/work/W2353554859> ?p ?o ?g. }
- W2353554859 endingPage "214" @default.
- W2353554859 startingPage "205" @default.
- W2353554859 abstract "Coexisting minerals of the hollandite-cryptomelane series, piemontite-group, and abswurmbachite-braunite series occur as a small nodule in a quartzose schist (metachert) from the epidote-amphibolite facies area of the Sanbagawa metamorphic belt, central Shikoku, Japan. Strontium, Ba. K. and Pb contents of the hollandite-cryptomelane minerals are 0.00-0.42, 0.07-0.99, 0.00-0.75 and 0.00-0.05 apfu (atoms per formula unit: O = 16), respectively. The piemontite-group minerals can be divided into common piemontite (Ca > Sr in the ten-coordinated A2-site) and strontiopiemontite (Sr > Ca). Strontium. Ba and Pb contents of the strontiopiemontite reach 0.71, 0.26 and 0.20 apfu (O = 12.5), respectively, suggesting the existence of two possible new end- members for epidote-group minerals: “Ba-piemontite [BaCa(Mn3+, Fe3+, Al)3Si3O12(OH)]” and Pb- piemontite [PbCa(Mn3+, Fe3+, Al)3Si3O12(OH)]”. The abswunnbachite-braunite series minerals (Cu = 0.30-0.53 apfu: O = 12) contain up to 0.34 apfu Mg, indicating the exchange Mg(Mn2+, Cu)-1. Distribution coefficients for Sr between the hollandite-cryptomelane series and the piemontite-group minerals are up to 20. implying that the hollandite-type structure with its large open tunnel is more suitable for incorporation of Sr than the A2-site of the piemontite-group minerals. A synthetic aluminosilicate analogue of the hollandite-cryptomelane compound is stable under P > 8-10 GPa. and suggests the hollandite-type aluminosilicate may be a reservoir of Sr and other large-ion-lithophile elements in the upper mantle." @default.
- W2353554859 created "2016-06-24" @default.
- W2353554859 creator A5001200304 @default.
- W2353554859 creator A5075675321 @default.
- W2353554859 date "2001-03-01" @default.
- W2353554859 modified "2023-10-18" @default.
- W2353554859 title "Partitioning of Sr between coexisting minerals of the hollandite- and piemontite-groups in a quartz-rich schist from the Sanbagawa metamorphic belt, Japan" @default.
- W2353554859 cites W1599002981 @default.
- W2353554859 cites W1928320224 @default.
- W2353554859 cites W1990412025 @default.
- W2353554859 cites W1996729893 @default.
- W2353554859 cites W1997731948 @default.
- W2353554859 cites W1998639266 @default.
- W2353554859 cites W2000684013 @default.
- W2353554859 cites W2001874262 @default.
- W2353554859 cites W2015602078 @default.
- W2353554859 cites W2017649324 @default.
- W2353554859 cites W2020915460 @default.
- W2353554859 cites W2027751460 @default.
- W2353554859 cites W2027789099 @default.
- W2353554859 cites W2030114314 @default.
- W2353554859 cites W2036086801 @default.
- W2353554859 cites W2046025164 @default.
- W2353554859 cites W2046697179 @default.
- W2353554859 cites W2057026910 @default.
- W2353554859 cites W2059551652 @default.
- W2353554859 cites W2060179714 @default.
- W2353554859 cites W2064437445 @default.
- W2353554859 cites W2075157849 @default.
- W2353554859 cites W2081859428 @default.
- W2353554859 cites W2082601356 @default.
- W2353554859 cites W2082832579 @default.
- W2353554859 cites W2098617829 @default.
- W2353554859 cites W2120360513 @default.
- W2353554859 cites W2141784230 @default.
- W2353554859 cites W2146396587 @default.
- W2353554859 cites W2162094172 @default.
- W2353554859 cites W2165275251 @default.
- W2353554859 cites W2167590372 @default.
- W2353554859 cites W2184011537 @default.
- W2353554859 cites W2317268950 @default.
- W2353554859 cites W2321749361 @default.
- W2353554859 cites W2327694683 @default.
- W2353554859 cites W2331013610 @default.
- W2353554859 cites W2335219246 @default.
- W2353554859 cites W2466901080 @default.
- W2353554859 cites W2482188364 @default.
- W2353554859 cites W2487312215 @default.
- W2353554859 cites W2500159714 @default.
- W2353554859 cites W2528618266 @default.
- W2353554859 cites W2587998086 @default.
- W2353554859 cites W2598570935 @default.
- W2353554859 cites W2752336021 @default.
- W2353554859 cites W2994538385 @default.
- W2353554859 cites W578639431 @default.
- W2353554859 cites W2504964583 @default.
- W2353554859 cites W2520973154 @default.
- W2353554859 doi "https://doi.org/10.2138/am-2001-2-301" @default.
- W2353554859 hasPublicationYear "2001" @default.
- W2353554859 type Work @default.
- W2353554859 sameAs 2353554859 @default.
- W2353554859 citedByCount "14" @default.
- W2353554859 countsByYear W23535548592013 @default.
- W2353554859 countsByYear W23535548592014 @default.
- W2353554859 countsByYear W23535548592020 @default.
- W2353554859 countsByYear W23535548592023 @default.
- W2353554859 crossrefType "journal-article" @default.
- W2353554859 hasAuthorship W2353554859A5001200304 @default.
- W2353554859 hasAuthorship W2353554859A5075675321 @default.
- W2353554859 hasConcept C101139013 @default.
- W2353554859 hasConcept C127313418 @default.
- W2353554859 hasConcept C151730666 @default.
- W2353554859 hasConcept C17409809 @default.
- W2353554859 hasConcept C178790620 @default.
- W2353554859 hasConcept C185592680 @default.
- W2353554859 hasConcept C199289684 @default.
- W2353554859 hasConcept C26687426 @default.
- W2353554859 hasConcept C2776432453 @default.
- W2353554859 hasConcept C2777844515 @default.
- W2353554859 hasConcept C2778357522 @default.
- W2353554859 hasConcept C2778410265 @default.
- W2353554859 hasConcept C2779851234 @default.
- W2353554859 hasConcept C2779870107 @default.
- W2353554859 hasConcept C2781084986 @default.
- W2353554859 hasConcept C2993225395 @default.
- W2353554859 hasConcept C518915863 @default.
- W2353554859 hasConceptScore W2353554859C101139013 @default.
- W2353554859 hasConceptScore W2353554859C127313418 @default.
- W2353554859 hasConceptScore W2353554859C151730666 @default.
- W2353554859 hasConceptScore W2353554859C17409809 @default.
- W2353554859 hasConceptScore W2353554859C178790620 @default.
- W2353554859 hasConceptScore W2353554859C185592680 @default.
- W2353554859 hasConceptScore W2353554859C199289684 @default.
- W2353554859 hasConceptScore W2353554859C26687426 @default.
- W2353554859 hasConceptScore W2353554859C2776432453 @default.
- W2353554859 hasConceptScore W2353554859C2777844515 @default.
- W2353554859 hasConceptScore W2353554859C2778357522 @default.
- W2353554859 hasConceptScore W2353554859C2778410265 @default.