FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4319869892> ?p ?o ?g. }

• W4319869892 endingPage "106994" @default.
• W4319869892 startingPage "106994" @default.
• W4319869892 abstract "Massif type charnockite was emplaced in the lower crust of the Eastern Ghats Province and is now exposed over a large geographic area. The rock shows clear evidence of magmatic emplacement in lower crustal metasedimentary rocks, which occur as enclaves within the charnockite. Textural data suggest the magma underwent subsolidus cooling and subsequently metamorphosed to granulite facies (up to ∼ 910 °C, 9 kbar). Geochemical data show that the charnockite magma had variable chemistry which was acquired by differentiation and possible crustal contamination. The rock shows both high- and low-SiO2 types, with weakly peraluminous to metaluminous characters. Trace and REE fractionation trends suggest the magma had calcic to calc-alkaline affinities and was emplaced in a continental arc type collisional setting. Theoretical modelling suggests that such a magma could be generated by melting of a hydrated basaltic slab under CO2-rich fluid. U-Pb analysis on oscillatory zoned zircon domains from eight samples yields crystallization ages for the magma. While the majority of the samples show crystallization ages within ca. 980–940 Ma (978 ± 16 Ma, 968 ± 22 Ma, 951 ± 9 Ma, 954 ± 8 Ma, 951 ± 13 Ma and 939 ± 27 Ma), two samples yield crystallization ages of 1002 ± 13 Ma and 1020 ± 16 Ma. This implies two-phase emplacement of the charnockite magma which can be correlated with the tectonometamorphic evolution of the province. While the earlier pulse of charnockite magmatism is broadly synchronous with the first cycle (M1) of metamorphism, the later pulse followed when the lower crust was still hot. The two pulses of charnockite magmatism are broadly synchronous with those of the Mawson charnockite of the Rayner Province, East Antarctica. It is argued that the charnockite magmatism in the combined Rayner-Eastern Ghats Province was extensive and resulted from arc-continent accretion and collision between the India and East Antarctica during ca. 1030–900 Ma." @default.
• W4319869892 created "2023-02-11" @default.
• W4319869892 creator A5014286635 @default.
• W4319869892 creator A5030080701 @default.
• W4319869892 creator A5032384722 @default.
• W4319869892 creator A5033085685 @default.
• W4319869892 creator A5039165939 @default.
• W4319869892 creator A5069323607 @default.
• W4319869892 date "2023-04-01" @default.
• W4319869892 modified "2023-09-27" @default.
• W4319869892 title "Petrological, geochemical and geochronological evolution of massif type charnockite from the Eastern Ghats Province, India: Implications on the regional tectonics of the Rayner-Eastern Ghats orogeny" @default.
• W4319869892 cites W1521262137 @default.
• W4319869892 cites W1933526536 @default.
• W4319869892 cites W1964291711 @default.
• W4319869892 cites W1966403266 @default.
• W4319869892 cites W1966719191 @default.
• W4319869892 cites W1969859799 @default.
• W4319869892 cites W1970101662 @default.
• W4319869892 cites W1970629158 @default.
• W4319869892 cites W1972298918 @default.
• W4319869892 cites W1973371064 @default.
• W4319869892 cites W1973439798 @default.
• W4319869892 cites W1989148885 @default.
• W4319869892 cites W1989955127 @default.
• W4319869892 cites W1991243694 @default.
• W4319869892 cites W1999496681 @default.
• W4319869892 cites W2000713509 @default.
• W4319869892 cites W2002460023 @default.
• W4319869892 cites W2003926196 @default.
• W4319869892 cites W2004280376 @default.
• W4319869892 cites W2005569462 @default.
• W4319869892 cites W2009048804 @default.
• W4319869892 cites W2010677603 @default.
• W4319869892 cites W2011494028 @default.
• W4319869892 cites W2015790224 @default.
• W4319869892 cites W2016481502 @default.
• W4319869892 cites W2017279170 @default.
• W4319869892 cites W2019034794 @default.
• W4319869892 cites W2024198809 @default.
• W4319869892 cites W2030263140 @default.
• W4319869892 cites W2032053833 @default.
• W4319869892 cites W2033424451 @default.
• W4319869892 cites W2038325228 @default.
• W4319869892 cites W2041705859 @default.
• W4319869892 cites W2042226801 @default.
• W4319869892 cites W2042860388 @default.
• W4319869892 cites W2043015847 @default.
• W4319869892 cites W2046239832 @default.
• W4319869892 cites W2046515928 @default.
• W4319869892 cites W2047504082 @default.
• W4319869892 cites W2047929173 @default.
• W4319869892 cites W2049639781 @default.
• W4319869892 cites W2051680308 @default.
• W4319869892 cites W2054418449 @default.
• W4319869892 cites W2054653182 @default.
• W4319869892 cites W2056595128 @default.
• W4319869892 cites W2058954734 @default.
• W4319869892 cites W2060768492 @default.
• W4319869892 cites W2060866871 @default.
• W4319869892 cites W2064567073 @default.
• W4319869892 cites W2067593179 @default.
• W4319869892 cites W2068816368 @default.
• W4319869892 cites W2070182003 @default.
• W4319869892 cites W2075026240 @default.
• W4319869892 cites W2075186328 @default.
• W4319869892 cites W2080611925 @default.
• W4319869892 cites W2080682810 @default.
• W4319869892 cites W2081507714 @default.
• W4319869892 cites W2087594774 @default.
• W4319869892 cites W2089514169 @default.
• W4319869892 cites W2094392648 @default.
• W4319869892 cites W2095522335 @default.
• W4319869892 cites W2106205498 @default.
• W4319869892 cites W2106301591 @default.
• W4319869892 cites W2110831835 @default.
• W4319869892 cites W2126445541 @default.
• W4319869892 cites W2131150748 @default.
• W4319869892 cites W2131613406 @default.
• W4319869892 cites W2133431446 @default.
• W4319869892 cites W2137179628 @default.
• W4319869892 cites W2138522501 @default.
• W4319869892 cites W2142421052 @default.
• W4319869892 cites W2143105947 @default.
• W4319869892 cites W2144461623 @default.
• W4319869892 cites W2153309547 @default.
• W4319869892 cites W2156402670 @default.
• W4319869892 cites W2164468447 @default.
• W4319869892 cites W2172007238 @default.
• W4319869892 cites W2273535049 @default.
• W4319869892 cites W2314518426 @default.
• W4319869892 cites W2605017508 @default.
• W4319869892 cites W2605575076 @default.
• W4319869892 cites W2782178208 @default.
• W4319869892 cites W2796362134 @default.
• W4319869892 cites W2802177525 @default.
• W4319869892 cites W2887496919 @default.
• W4319869892 cites W2995482781 @default.
• W4319869892 cites W3006469643 @default.

• next