FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2008435820> ?p ?o ?g. }

• W2008435820 endingPage "191" @default.
• W2008435820 startingPage "177" @default.
• W2008435820 abstract "Abstract A multiphase granitic complex (G1–G6) in the Carrazeda de Ansiaes area, Central Iberian Zone, was emplaced during syn-kinematic stages of the Variscan orogeny, between 329.9 ± 0.8 Ma and 318.9 ± 1.9 Ma, as determined by ID-TIMS U–Pb on zircon and monazite. The complex intruded the metasedimentary Douro Group in a NW trending antiform formed during the D 1 and D 3 deformation phases, but was itself affected by ductile and brittle deformation. The granites have equal or higher amounts of muscovite than biotite, and contain surmicaceous enclaves and more rarely xenoliths, “schlieren” and microgranular enclaves. They are S-type, mainly alkaline-calcic and peraluminous with ASI ranging between 1.21 and 1.45 and normative corundum of 2.63–4.77%. They are enriched in LREE relatively to HREE, with negative Eu anomalies, ( 87 Sr/ 86 Sr) i  = 0.7097–0.7159, eNd = − 6.2 to − 9.1, and δ 18 O = 10.96–11.81‰. Geochemical and isotopic characteristics show that granites G1, G2, G4 and G5 correspond to distinct pulses of magma formed by partial melting of heterogeneous metasedimentary material. Geochemical fractionation trends recorded by whole rocks and minerals permit to distinguish and model two fractional crystallization series G2–G3 and G5–G6, the latter also affected by crustal assimilation during fractionation. Granites G1, G2, G3 and G6 have ≥ 20 ppm Sn and G5 16 ppm Sn; they are also associated with mineralized Sn- and W-bearing quartz veins. Fractional crystallization was the responsible process for the increase in Sn content in granites from the series and their micas." @default.
• W2008435820 created "2016-06-24" @default.
• W2008435820 creator A5011213490 @default.
• W2008435820 creator A5013393080 @default.
• W2008435820 creator A5014983459 @default.
• W2008435820 creator A5041465086 @default.
• W2008435820 creator A5058907828 @default.
• W2008435820 creator A5060195461 @default.
• W2008435820 date "2012-11-01" @default.
• W2008435820 modified "2023-09-25" @default.
• W2008435820 title "The role of fractional crystallization in the genesis of early syn-D3, tin-mineralized Variscan two-mica granites from the Carrazeda de Ansiães area, northern Portugal" @default.
• W2008435820 cites W1965858395 @default.
• W2008435820 cites W1966256034 @default.
• W2008435820 cites W1970242481 @default.
• W2008435820 cites W1981899274 @default.
• W2008435820 cites W1982715070 @default.
• W2008435820 cites W1985269230 @default.
• W2008435820 cites W1985311970 @default.
• W2008435820 cites W1988410159 @default.
• W2008435820 cites W1997536923 @default.
• W2008435820 cites W1998830775 @default.
• W2008435820 cites W1999105978 @default.
• W2008435820 cites W2003103303 @default.
• W2008435820 cites W2007105153 @default.
• W2008435820 cites W2012383573 @default.
• W2008435820 cites W2012999169 @default.
• W2008435820 cites W2019013664 @default.
• W2008435820 cites W2024575502 @default.
• W2008435820 cites W2025875745 @default.
• W2008435820 cites W2030098510 @default.
• W2008435820 cites W2033759679 @default.
• W2008435820 cites W2036707437 @default.
• W2008435820 cites W2041795897 @default.
• W2008435820 cites W2043719588 @default.
• W2008435820 cites W2044358950 @default.
• W2008435820 cites W2046629156 @default.
• W2008435820 cites W2047349541 @default.
• W2008435820 cites W2047890176 @default.
• W2008435820 cites W2048635291 @default.
• W2008435820 cites W2050788474 @default.
• W2008435820 cites W2064642826 @default.
• W2008435820 cites W2066352136 @default.
• W2008435820 cites W2070588656 @default.
• W2008435820 cites W2073451667 @default.
• W2008435820 cites W2075902587 @default.
• W2008435820 cites W2076274920 @default.
• W2008435820 cites W2076440051 @default.
• W2008435820 cites W2076983044 @default.
• W2008435820 cites W2088519109 @default.
• W2008435820 cites W2091184061 @default.
• W2008435820 cites W2098235917 @default.
• W2008435820 cites W2099183500 @default.
• W2008435820 cites W2103999221 @default.
• W2008435820 cites W2120848012 @default.
• W2008435820 cites W2125691712 @default.
• W2008435820 cites W2129531693 @default.
• W2008435820 cites W2142090815 @default.
• W2008435820 cites W2145604970 @default.
• W2008435820 cites W2335047151 @default.
• W2008435820 cites W2489350656 @default.
• W2008435820 cites W2749490971 @default.
• W2008435820 cites W4255137559 @default.
• W2008435820 doi "https://doi.org/10.1016/j.lithos.2012.04.024" @default.
• W2008435820 hasPublicationYear "2012" @default.
• W2008435820 type Work @default.
• W2008435820 sameAs 2008435820 @default.
• W2008435820 citedByCount "56" @default.
• W2008435820 countsByYear W20084358202014 @default.
• W2008435820 countsByYear W20084358202015 @default.
• W2008435820 countsByYear W20084358202016 @default.
• W2008435820 countsByYear W20084358202017 @default.
• W2008435820 countsByYear W20084358202018 @default.
• W2008435820 countsByYear W20084358202019 @default.
• W2008435820 countsByYear W20084358202020 @default.
• W2008435820 countsByYear W20084358202021 @default.
• W2008435820 countsByYear W20084358202022 @default.
• W2008435820 countsByYear W20084358202023 @default.
• W2008435820 crossrefType "journal-article" @default.
• W2008435820 hasAuthorship W2008435820A5011213490 @default.
• W2008435820 hasAuthorship W2008435820A5013393080 @default.
• W2008435820 hasAuthorship W2008435820A5014983459 @default.
• W2008435820 hasAuthorship W2008435820A5041465086 @default.
• W2008435820 hasAuthorship W2008435820A5058907828 @default.
• W2008435820 hasAuthorship W2008435820A5060195461 @default.
• W2008435820 hasConcept C11872896 @default.
• W2008435820 hasConcept C127313418 @default.
• W2008435820 hasConcept C151730666 @default.
• W2008435820 hasConcept C17409809 @default.
• W2008435820 hasConcept C178790620 @default.
• W2008435820 hasConcept C185592680 @default.
• W2008435820 hasConcept C191897082 @default.
• W2008435820 hasConcept C192562407 @default.
• W2008435820 hasConcept C199289684 @default.
• W2008435820 hasConcept C203036418 @default.
• W2008435820 hasConcept C2781038479 @default.
• W2008435820 hasConcept C525849907 @default.
• W2008435820 hasConcept C67236022 @default.
• W2008435820 hasConceptScore W2008435820C11872896 @default.

• next