FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2132397310> ?p ?o ?g. }

• W2132397310 endingPage "1472" @default.
• W2132397310 startingPage "1455" @default.
• W2132397310 abstract "Marble occurs abundantly in a portion of the Grenville Province of the Canadian Shield extending from the Adirondack Mountains, through Ontario, and into the Laurentian Highlands of Quebec, a distance of 300 km. In the Otter Lake area of western Quebec, major marble units, which are obviously metamorphosed limestone, consist of combinations of calcite, dolomite, olivine, humite-group minerals, Ca pyroxene, Ca amphibole, biotite, graphite, and retrograde serpentine and brucite, whereas minor marble units, which are evidently metasomatic rocks, consist of combinations of (pink) calcite, Ca pyroxene, Ca amphibole, biotite, garnet, K-feldspar, scapolite, and titanite. The oxygen and carbon isotopic composition of calcite in the major marble units (δ18OVSMOW in the range 28 to 17‰; δ13CPDB–1 in the range +6 to −2‰) is the same as in the Adirondacks and in unmetamorphosed Proterozoic limestone; only slight shifts (~1‰) can be attributed directly to metamorphic reactions. In bodies of minor marble, mean concentrations of 18O and 13C are slightly lower (+14.5 and +0.23‰, respectively). Mean fractionation-factors (α, expressed as 1000 ln α, are as follows: 18O, calcite/dolomite, +0.295 ( n = 11); 13C, calcite/dolomite, −0.346 ( n = 12); 18O, calcite/biotite, +3.49 ( n = 5); 13C, calcite/graphite, +3.74 ( n = 5). Additional (exploratory) results ( n = 1) on the distribution of 18O are as follows: calcite/olivine, +3.5; calcite/clinohumite, +5.1; calcite/garnet, +2.4; calcite/titanite, +3.1; calcite/Ca pyroxene, +2.0; calcite/Ca amphibole, +2.4, calcite/K-feldspar +1.8; calcite/scapolite, +2.0; calcite/serpentine, +13.9; calcite/brucite, +19.7; a trend of increasing α is related to increasing OH/(O + OH) in the non-carbonates and the preference of OH for 16O. For the first group of mineral pairs ( n ≥ a small variation in α across the study area (relative standard deviation ~0.05%) is viewed as an expression of a close approach to isotopic exchange equilibrium, and for certain pairs from the second group ( n = 1), a temperature estimate close to 700° (the biotite–garnet temperature of associated gneisses) is also viewed as evidence for equilibrium. Attainment of isotopic exchange equilibrium was facilitated by dynamic recrystallization, which occurred during the peak of metamorphism." @default.
• W2132397310 created "2016-06-24" @default.
• W2132397310 creator A5088600853 @default.
• W2132397310 date "2001-10-01" @default.
• W2132397310 modified "2023-09-26" @default.
• W2132397310 title "OXYGEN AND CARBON ISOTOPIC COMPOSITION OF GRENVILLE MARBLE, AND AN APPRAISAL OF EQUILIBRIUM IN THE DISTRIBUTION OF ISOTOPES BETWEEN CALCITE AND ASSOCIATED MINERALS, OTTER LAKE AREA, QUEBEC, CANADA" @default.
• W2132397310 cites W1521233584 @default.
• W2132397310 cites W1547907389 @default.
• W2132397310 cites W1897984470 @default.
• W2132397310 cites W1922245190 @default.
• W2132397310 cites W1965396523 @default.
• W2132397310 cites W1973432121 @default.
• W2132397310 cites W1974258155 @default.
• W2132397310 cites W1974513838 @default.
• W2132397310 cites W1977617426 @default.
• W2132397310 cites W1981792144 @default.
• W2132397310 cites W1987445809 @default.
• W2132397310 cites W1989039485 @default.
• W2132397310 cites W1989149873 @default.
• W2132397310 cites W1990581568 @default.
• W2132397310 cites W1997533928 @default.
• W2132397310 cites W2004679561 @default.
• W2132397310 cites W2008281306 @default.
• W2132397310 cites W2008286663 @default.
• W2132397310 cites W2008938437 @default.
• W2132397310 cites W2019795776 @default.
• W2132397310 cites W2026387367 @default.
• W2132397310 cites W2027419584 @default.
• W2132397310 cites W2032695617 @default.
• W2132397310 cites W2035742871 @default.
• W2132397310 cites W2035921610 @default.
• W2132397310 cites W2038149087 @default.
• W2132397310 cites W2041007525 @default.
• W2132397310 cites W2049200271 @default.
• W2132397310 cites W2052848232 @default.
• W2132397310 cites W2054075985 @default.
• W2132397310 cites W2059849751 @default.
• W2132397310 cites W2062471418 @default.
• W2132397310 cites W2066856460 @default.
• W2132397310 cites W2068202901 @default.
• W2132397310 cites W2072407455 @default.
• W2132397310 cites W2073173024 @default.
• W2132397310 cites W2080523684 @default.
• W2132397310 cites W2085786036 @default.
• W2132397310 cites W2088040215 @default.
• W2132397310 cites W2106537927 @default.
• W2132397310 cites W2120177969 @default.
• W2132397310 cites W2125273916 @default.
• W2132397310 cites W2150862234 @default.
• W2132397310 cites W2162378760 @default.
• W2132397310 cites W2164646646 @default.
• W2132397310 cites W2225568362 @default.
• W2132397310 cites W2255127968 @default.
• W2132397310 cites W2319271273 @default.
• W2132397310 cites W2327647032 @default.
• W2132397310 cites W2328438193 @default.
• W2132397310 cites W2345090980 @default.
• W2132397310 cites W243144100 @default.
• W2132397310 cites W2522811608 @default.
• W2132397310 cites W2601853714 @default.
• W2132397310 cites W2885166818 @default.
• W2132397310 doi "https://doi.org/10.2113/gscanmin.39.5.1455" @default.
• W2132397310 hasPublicationYear "2001" @default.
• W2132397310 type Work @default.
• W2132397310 sameAs 2132397310 @default.
• W2132397310 citedByCount "15" @default.
• W2132397310 countsByYear W21323973102012 @default.
• W2132397310 countsByYear W21323973102013 @default.
• W2132397310 countsByYear W21323973102014 @default.
• W2132397310 countsByYear W21323973102015 @default.
• W2132397310 countsByYear W21323973102019 @default.
• W2132397310 countsByYear W21323973102022 @default.
• W2132397310 crossrefType "journal-article" @default.
• W2132397310 hasAuthorship W2132397310A5088600853 @default.
• W2132397310 hasConcept C104779481 @default.
• W2132397310 hasConcept C121332964 @default.
• W2132397310 hasConcept C127313418 @default.
• W2132397310 hasConcept C140205800 @default.
• W2132397310 hasConcept C159985019 @default.
• W2132397310 hasConcept C17409809 @default.
• W2132397310 hasConcept C192562407 @default.
• W2132397310 hasConcept C199289684 @default.
• W2132397310 hasConcept C22117777 @default.
• W2132397310 hasConcept C2780191791 @default.
• W2132397310 hasConcept C62520636 @default.
• W2132397310 hasConcept C71468253 @default.
• W2132397310 hasConceptScore W2132397310C104779481 @default.
• W2132397310 hasConceptScore W2132397310C121332964 @default.
• W2132397310 hasConceptScore W2132397310C127313418 @default.
• W2132397310 hasConceptScore W2132397310C140205800 @default.
• W2132397310 hasConceptScore W2132397310C159985019 @default.
• W2132397310 hasConceptScore W2132397310C17409809 @default.
• W2132397310 hasConceptScore W2132397310C192562407 @default.
• W2132397310 hasConceptScore W2132397310C199289684 @default.
• W2132397310 hasConceptScore W2132397310C22117777 @default.
• W2132397310 hasConceptScore W2132397310C2780191791 @default.
• W2132397310 hasConceptScore W2132397310C62520636 @default.
• W2132397310 hasConceptScore W2132397310C71468253 @default.

• next