FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2994657351> ?p ?o ?g. }

• W2994657351 endingPage "105567" @default.
• W2994657351 startingPage "105567" @default.
• W2994657351 abstract "The Mantiqueira Complex together with the Mineiro Belt and Juiz de Fora Complex, characterize a long-lived system of oceanic and continental magmatic arcs. The proposed accretion of these terranes in the Rhyacian resulted in the closure of the Minas Basin, a fundamental turning point for the geology of this area. Understanding this event is critical for determining the evolution of the South American continent. Despite its importance, there is a paucity of zircon U-Pb and Lu-Hf data available for the Mantiqueira Complex and no data from two complexes within the later. U-Pb zircon data were obtained from interpreted metasediments of those two complexes, the granulite facies Acaiaca Complex and Pedra Dourada Granulite. Four targeted samples yield cores with ages between 3.5 and 2.2 Ga and a large proportion of metamorphic grains and rims at ca. 2.1–2.0 Ga. The similarity between the detrital zircon signatures of the Acaiaca Complex and Pedra Dourada Granulite, and the Archaean inheritance of the Mantiqueira Complex, indicates that these three units are related. Potentially the Acaiaca Complex and Pedra Dourada Granulite either sourced the Mantiqueira Complex or the Mantiqueira intrusive suites reworked the protoliths of the Acaiaca Complex and Pedra Dourada Granulite. Hf-in-zircon data indicate two discrete sources for both the Acaiaca Complex and Pedra Dourada Granulite. An Archaean source (model ages of 3.2–2.6 Ga), which is consistent with the suggested origin of the Mantiqueira Complex as recycled Archaean crust sourced from the São Francisco Craton and reworked during the ca. 2.1 Ga Transamazonian orogeny. A second more juvenile source (model ages of 2.4–2.2 Ga) recorded exclusively within the more mafic samples is identical in age and Hf to that found in the Juiz de Fora Complex. This could indicate a close link between the Mantiqueira and Juiz de Fora Complexes in the period 2.2 to 2.0 Ga. Alternatively, these juvenile zircons may represent an as yet unidentified juvenile portion of the Mantiqueira arc. The results of this study are consistent with the prevailing theories for formation of the Mantiqueira Complex as a continental arc with cumulative proportion curves indicating an active-margin type depositional setting." @default.
• W2994657351 created "2019-12-26" @default.
• W2994657351 creator A5024681692 @default.
• W2994657351 creator A5045168872 @default.
• W2994657351 creator A5067579569 @default.
• W2994657351 creator A5081415011 @default.
• W2994657351 creator A5089252988 @default.
• W2994657351 date "2020-03-01" @default.
• W2994657351 modified "2023-10-12" @default.
• W2994657351 title "Zircon U-Pb and Lu-Hf record from high-grade complexes within the Mantiqueira Complex: First evidence of juvenile crustal input at 2.4–2.2 Ga and implications for the Palaeoproterozoic evolution of the São Francisco Craton" @default.
• W2994657351 cites W1599008295 @default.
• W2994657351 cites W1864039219 @default.
• W2994657351 cites W1953697892 @default.
• W2994657351 cites W1967675439 @default.
• W2994657351 cites W1969185546 @default.
• W2994657351 cites W1970901883 @default.
• W2994657351 cites W1972547679 @default.
• W2994657351 cites W1982646204 @default.
• W2994657351 cites W1991964081 @default.
• W2994657351 cites W1992932292 @default.
• W2994657351 cites W1995820414 @default.
• W2994657351 cites W2000908685 @default.
• W2994657351 cites W2009525078 @default.
• W2994657351 cites W2013601702 @default.
• W2994657351 cites W2020973699 @default.
• W2994657351 cites W2029013584 @default.
• W2994657351 cites W2032200127 @default.
• W2994657351 cites W2048072603 @default.
• W2994657351 cites W2048800364 @default.
• W2994657351 cites W2048857036 @default.
• W2994657351 cites W2059356468 @default.
• W2994657351 cites W2064991810 @default.
• W2994657351 cites W2065823329 @default.
• W2994657351 cites W2072422341 @default.
• W2994657351 cites W2077058355 @default.
• W2994657351 cites W2086215220 @default.
• W2994657351 cites W2105828829 @default.
• W2994657351 cites W2123993695 @default.
• W2994657351 cites W2136857107 @default.
• W2994657351 cites W2138986673 @default.
• W2994657351 cites W2156985625 @default.
• W2994657351 cites W2157517475 @default.
• W2994657351 cites W2169766597 @default.
• W2994657351 cites W2171086159 @default.
• W2994657351 cites W2199014807 @default.
• W2994657351 cites W2220964083 @default.
• W2994657351 cites W2400889349 @default.
• W2994657351 cites W2534704824 @default.
• W2994657351 cites W2561940965 @default.
• W2994657351 cites W2581733081 @default.
• W2994657351 cites W2583609738 @default.
• W2994657351 cites W2593636494 @default.
• W2994657351 cites W2606205785 @default.
• W2994657351 cites W2743501435 @default.
• W2994657351 cites W2776513136 @default.
• W2994657351 cites W2788332975 @default.
• W2994657351 cites W2789444652 @default.
• W2994657351 cites W2789672194 @default.
• W2994657351 cites W2790150619 @default.
• W2994657351 cites W2889429378 @default.
• W2994657351 cites W2902554706 @default.
• W2994657351 cites W2905827869 @default.
• W2994657351 cites W2910849449 @default.
• W2994657351 cites W2921616759 @default.
• W2994657351 cites W4252666421 @default.
• W2994657351 cites W4253776820 @default.
• W2994657351 cites W583039854 @default.
• W2994657351 doi "https://doi.org/10.1016/j.precamres.2019.105567" @default.
• W2994657351 hasPublicationYear "2020" @default.
• W2994657351 type Work @default.
• W2994657351 sameAs 2994657351 @default.
• W2994657351 citedByCount "15" @default.
• W2994657351 countsByYear W29946573512020 @default.
• W2994657351 countsByYear W29946573512021 @default.
• W2994657351 countsByYear W29946573512022 @default.
• W2994657351 countsByYear W29946573512023 @default.
• W2994657351 crossrefType "journal-article" @default.
• W2994657351 hasAuthorship W2994657351A5024681692 @default.
• W2994657351 hasAuthorship W2994657351A5045168872 @default.
• W2994657351 hasAuthorship W2994657351A5067579569 @default.
• W2994657351 hasAuthorship W2994657351A5081415011 @default.
• W2994657351 hasAuthorship W2994657351A5089252988 @default.
• W2994657351 hasBestOaLocation W29946573512 @default.
• W2994657351 hasConcept C109007969 @default.
• W2994657351 hasConcept C114793014 @default.
• W2994657351 hasConcept C120806208 @default.
• W2994657351 hasConcept C127313418 @default.
• W2994657351 hasConcept C146588470 @default.
• W2994657351 hasConcept C147717901 @default.
• W2994657351 hasConcept C149347711 @default.
• W2994657351 hasConcept C150999391 @default.
• W2994657351 hasConcept C151730666 @default.
• W2994657351 hasConcept C17409809 @default.
• W2994657351 hasConcept C18142444 @default.
• W2994657351 hasConcept C192241223 @default.
• W2994657351 hasConcept C2776698055 @default.
• W2994657351 hasConcept C2778849375 @default.
• W2994657351 hasConcept C2779430719 @default.

• next