FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2415565863> ?p ?o ?g. }

• W2415565863 endingPage "46" @default.
• W2415565863 startingPage "32" @default.
• W2415565863 abstract "Triassic granitoids (∼200–225 Ma) are widespread in the Western Belt of Peninsular Malaysia. The Main Range granite is the biggest batholith in the Western Belt composed of peraluminous to metaluminous granite and granodiorite and displays typical ilmenite-series characteristics. Jerai granitic pluton occurs at the northwestern part of the Main Range granite batholith. The Jerai granite can be divided into three facies: (i) biotite-muscovite granite; (ii) tourmaline granite; and (iii) pegmatite and aplopegmatite. Biotite-muscovite granite accounts for 90% of the Jerai pluton, and the rest is tourmaline granite. Geochemical data reveal that pegmatite and tourmaline granite are more differentiated than biotite-muscovite granite. Both pegmatite and tourmaline granite have a higher SiO2 content (70.95–83.94% versus 69.45–73.35%) and a more pronounced peraluminous character. The U–Pb zircon geochronology of the Jerai granite gave an age ranging from 204 ± 4.3 Ma, 205 ± 4 Ma and 205 ± 2 Ma for pegmatite biotite-muscovite granite and tourmaline granite, respectively. The biotite-muscovite Jerai granites are similar to S-type Main Range granite, but the tourmaline granite has a signature of late-stage hydrothermal fluid interaction such as tourmaline quartz pods, the accumulation of large pegmatitic K-feldspar, pronounced peraluminous character, higher SiO2 content. Age evidence of these two granitic facies suggest that they are from the same magma." @default.
• W2415565863 created "2016-06-24" @default.
• W2415565863 creator A5001998983 @default.
• W2415565863 creator A5012689458 @default.
• W2415565863 creator A5018048527 @default.
• W2415565863 creator A5031239050 @default.
• W2415565863 creator A5055574229 @default.
• W2415565863 date "2016-09-01" @default.
• W2415565863 modified "2023-10-02" @default.
• W2415565863 title "Origin and tectonic implications of the ∼200 Ma, collision-related Jerai pluton of the Western Granite Belt, Peninsular Malaysia" @default.
• W2415565863 cites W1888997480 @default.
• W2415565863 cites W1969998720 @default.
• W2415565863 cites W1977935606 @default.
• W2415565863 cites W1984762153 @default.
• W2415565863 cites W1992680913 @default.
• W2415565863 cites W1993290622 @default.
• W2415565863 cites W2006891112 @default.
• W2415565863 cites W2014745983 @default.
• W2415565863 cites W2015423120 @default.
• W2415565863 cites W2018039364 @default.
• W2415565863 cites W2020973699 @default.
• W2415565863 cites W2039722155 @default.
• W2415565863 cites W2039872199 @default.
• W2415565863 cites W2050925751 @default.
• W2415565863 cites W2056017961 @default.
• W2415565863 cites W2059644452 @default.
• W2415565863 cites W2066025065 @default.
• W2415565863 cites W2068403951 @default.
• W2415565863 cites W2069244272 @default.
• W2415565863 cites W2094727526 @default.
• W2415565863 cites W2106769845 @default.
• W2415565863 cites W2108971421 @default.
• W2415565863 cites W2112986594 @default.
• W2415565863 cites W2117839339 @default.
• W2415565863 cites W2126658799 @default.
• W2415565863 cites W2132997778 @default.
• W2415565863 cites W2140771040 @default.
• W2415565863 cites W2151517986 @default.
• W2415565863 cites W2153380575 @default.
• W2415565863 cites W2172140937 @default.
• W2415565863 cites W2183862063 @default.
• W2415565863 cites W2965067442 @default.
• W2415565863 cites W2967856178 @default.
• W2415565863 doi "https://doi.org/10.1016/j.jseaes.2016.06.004" @default.
• W2415565863 hasPublicationYear "2016" @default.
• W2415565863 type Work @default.
• W2415565863 sameAs 2415565863 @default.
• W2415565863 citedByCount "15" @default.
• W2415565863 countsByYear W24155658632017 @default.
• W2415565863 countsByYear W24155658632018 @default.
• W2415565863 countsByYear W24155658632019 @default.
• W2415565863 countsByYear W24155658632020 @default.
• W2415565863 countsByYear W24155658632021 @default.
• W2415565863 countsByYear W24155658632022 @default.
• W2415565863 countsByYear W24155658632023 @default.
• W2415565863 crossrefType "journal-article" @default.
• W2415565863 hasAuthorship W2415565863A5001998983 @default.
• W2415565863 hasAuthorship W2415565863A5012689458 @default.
• W2415565863 hasAuthorship W2415565863A5018048527 @default.
• W2415565863 hasAuthorship W2415565863A5031239050 @default.
• W2415565863 hasAuthorship W2415565863A5055574229 @default.
• W2415565863 hasConcept C127313418 @default.
• W2415565863 hasConcept C151730666 @default.
• W2415565863 hasConcept C172660882 @default.
• W2415565863 hasConcept C17409809 @default.
• W2415565863 hasConcept C195845463 @default.
• W2415565863 hasConcept C2776581184 @default.
• W2415565863 hasConcept C2777229588 @default.
• W2415565863 hasConcept C2777980256 @default.
• W2415565863 hasConcept C2778849375 @default.
• W2415565863 hasConcept C2779870107 @default.
• W2415565863 hasConcept C34122518 @default.
• W2415565863 hasConcept C5900021 @default.
• W2415565863 hasConcept C77928131 @default.
• W2415565863 hasConceptScore W2415565863C127313418 @default.
• W2415565863 hasConceptScore W2415565863C151730666 @default.
• W2415565863 hasConceptScore W2415565863C172660882 @default.
• W2415565863 hasConceptScore W2415565863C17409809 @default.
• W2415565863 hasConceptScore W2415565863C195845463 @default.
• W2415565863 hasConceptScore W2415565863C2776581184 @default.
• W2415565863 hasConceptScore W2415565863C2777229588 @default.
• W2415565863 hasConceptScore W2415565863C2777980256 @default.
• W2415565863 hasConceptScore W2415565863C2778849375 @default.
• W2415565863 hasConceptScore W2415565863C2779870107 @default.
• W2415565863 hasConceptScore W2415565863C34122518 @default.
• W2415565863 hasConceptScore W2415565863C5900021 @default.
• W2415565863 hasConceptScore W2415565863C77928131 @default.
• W2415565863 hasLocation W24155658631 @default.
• W2415565863 hasOpenAccess W2415565863 @default.
• W2415565863 hasPrimaryLocation W24155658631 @default.
• W2415565863 hasRelatedWork W2032890783 @default.
• W2415565863 hasRelatedWork W2099183500 @default.
• W2415565863 hasRelatedWork W2291433049 @default.
• W2415565863 hasRelatedWork W2361053869 @default.
• W2415565863 hasRelatedWork W2891908182 @default.
• W2415565863 hasRelatedWork W3005753292 @default.
• W2415565863 hasRelatedWork W3185629857 @default.
• W2415565863 hasRelatedWork W4308737499 @default.

• next