FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2106301591> ?p ?o ?g. }

• W2106301591 endingPage "40" @default.
• W2106301591 startingPage "3" @default.
• W2106301591 abstract "The Varberg–Torpa charnockite–granite association (Varberg, SW Sweden) consists of the magmatic Varberg charnockite (1399 ± 6 Ma) and the Torpa granite (1380 ± 12 Ma). The Torpa granite is both continuous and, based on its whole-rock geochemistry, synmagmatic with the Varberg charnockite. The granite body also contains a number of charnockite inliers. P–T estimation using garnet–clinopyroxene and orthopyroxene–clinopyroxene Fe–Mg exchange thermometry and garnet–orthopyroxene–plagioclase–quartz barometry gives temperatures and pressures (750–850°C; 800–850 MPa) that most probably approximate the P–T conditions during emplacement of the charnockite compared with a lower crystallization temperature (650–700°C) for the granite. The earliest recognized fluid inclusions in both the granite and charnockite consist of H2O–CO2 mixtures (H2O volume fraction 0·2–0·7). Fluid inclusions in the charnockite are characterized by high CO2 densities (up to 1·0 g cm−3; 40–90% bulk CO2), of probable magmatic origin, and are best preserved in garnet, plagioclase, and fluorapatite (in order of decreasing CO2 densities), and sometimes also in clinopyroxene. Fluid inclusions with the highest CO2 densities (1·08–1·10 g cm−3) are found in quartz (Th –31 to –36°C) and may have originated under high P–T conditions during emplacement and cooling of the charnockite. Magmatic fluids in the granite correspond to aqueous–carbonic inclusions with an estimated bulk composition (mol %) of H2O 73%, CO2 25%, NaCl 2%. The salinity of the solutes in the granite (typically 14–20 wt % NaCl-eq.) is generally higher than for the charnockite (0–8 wt % NaCl-eq.). Field, petrographic, mineralogical, geochemical, and fluid inclusion evidence indicates that, compared with the H2O-rich granite, the magma responsible for the charnockite had a preponderance of CO2 over H2O, which lowered the H2O activity in the melt, stabilizing ortho- and clinopyroxene. This evidence also supports the idea that the granite and charnockite were derived from a common source magma (most probably a fluid-rich basalt at the base of the crust) as a result of fractional crystallization." @default.
• W2106301591 created "2016-06-24" @default.
• W2106301591 creator A5007625041 @default.
• W2106301591 creator A5022321555 @default.
• W2106301591 creator A5078358216 @default.
• W2106301591 date "2012-10-25" @default.
• W2106301591 modified "2023-09-27" @default.
• W2106301591 title "The Varberg-Torpa Charnockite-Granite Association, SW Sweden: Mineralogy, Petrology, and Fluid Inclusion Chemistry" @default.
• W2106301591 cites W1532172917 @default.
• W2106301591 cites W1830358639 @default.
• W2106301591 cites W1972717431 @default.
• W2106301591 cites W1975436931 @default.
• W2106301591 cites W1978443253 @default.
• W2106301591 cites W1985160890 @default.
• W2106301591 cites W1987304681 @default.
• W2106301591 cites W1988953887 @default.
• W2106301591 cites W1990564225 @default.
• W2106301591 cites W2004919191 @default.
• W2106301591 cites W2006576973 @default.
• W2106301591 cites W2011488152 @default.
• W2106301591 cites W2012532958 @default.
• W2106301591 cites W2017031317 @default.
• W2106301591 cites W2018050219 @default.
• W2106301591 cites W2019204577 @default.
• W2106301591 cites W2021787304 @default.
• W2106301591 cites W2022558625 @default.
• W2106301591 cites W2023949103 @default.
• W2106301591 cites W2024921949 @default.
• W2106301591 cites W2027763109 @default.
• W2106301591 cites W2032486206 @default.
• W2106301591 cites W2034467201 @default.
• W2106301591 cites W2034671041 @default.
• W2106301591 cites W2037093925 @default.
• W2106301591 cites W2039052178 @default.
• W2106301591 cites W2039411725 @default.
• W2106301591 cites W2045341141 @default.
• W2106301591 cites W2046050954 @default.
• W2106301591 cites W2046141409 @default.
• W2106301591 cites W2047842327 @default.
• W2106301591 cites W2051469631 @default.
• W2106301591 cites W2053618571 @default.
• W2106301591 cites W2054940051 @default.
• W2106301591 cites W2057692293 @default.
• W2106301591 cites W2058841017 @default.
• W2106301591 cites W2060768492 @default.
• W2106301591 cites W2064567073 @default.
• W2106301591 cites W2074452712 @default.
• W2106301591 cites W2079772117 @default.
• W2106301591 cites W2080461060 @default.
• W2106301591 cites W2081507714 @default.
• W2106301591 cites W2082261829 @default.
• W2106301591 cites W2094017972 @default.
• W2106301591 cites W2098118945 @default.
• W2106301591 cites W2106146079 @default.
• W2106301591 cites W2112222104 @default.
• W2106301591 cites W2113127006 @default.
• W2106301591 cites W2122934607 @default.
• W2106301591 cites W2128383999 @default.
• W2106301591 cites W2131590321 @default.
• W2106301591 cites W2132514060 @default.
• W2106301591 cites W2133431446 @default.
• W2106301591 cites W2135979974 @default.
• W2106301591 cites W2143105947 @default.
• W2106301591 cites W2153586185 @default.
• W2106301591 cites W2156402670 @default.
• W2106301591 cites W2163403879 @default.
• W2106301591 cites W2164711061 @default.
• W2106301591 cites W2166125718 @default.
• W2106301591 cites W2171170313 @default.
• W2106301591 cites W2314518426 @default.
• W2106301591 cites W2318413759 @default.
• W2106301591 cites W2328081335 @default.
• W2106301591 cites W2330756480 @default.
• W2106301591 cites W2353870592 @default.
• W2106301591 cites W2467110588 @default.
• W2106301591 cites W2514193346 @default.
• W2106301591 cites W2516007964 @default.
• W2106301591 cites W4233237988 @default.
• W2106301591 cites W4248816266 @default.
• W2106301591 cites W4254941725 @default.
• W2106301591 doi "https://doi.org/10.1093/petrology/egs060" @default.
• W2106301591 hasPublicationYear "2012" @default.
• W2106301591 type Work @default.
• W2106301591 sameAs 2106301591 @default.
• W2106301591 citedByCount "32" @default.
• W2106301591 countsByYear W21063015912014 @default.
• W2106301591 countsByYear W21063015912015 @default.
• W2106301591 countsByYear W21063015912017 @default.
• W2106301591 countsByYear W21063015912018 @default.
• W2106301591 countsByYear W21063015912019 @default.
• W2106301591 countsByYear W21063015912020 @default.
• W2106301591 countsByYear W21063015912021 @default.
• W2106301591 countsByYear W21063015912022 @default.
• W2106301591 countsByYear W21063015912023 @default.
• W2106301591 crossrefType "journal-article" @default.
• W2106301591 hasAuthorship W2106301591A5007625041 @default.
• W2106301591 hasAuthorship W2106301591A5022321555 @default.
• W2106301591 hasAuthorship W2106301591A5078358216 @default.

• next