FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2979989490> ?p ?o ?g. }

• W2979989490 endingPage "227" @default.
• W2979989490 startingPage "210" @default.
• W2979989490 abstract "Permian–Triassic fore-arc basin terranes are exposed in New Zealand, but their original positions and tectonic configurations along the eastern Gondwanan margin are not fully understood. To better constrain late Paleozoic and Mesozoic reconstructions, we investigated the provenance of Permian–Triassic marine sandstone units from the Dun Mountain-Maitai Terrane (Maitai Group) and the Kaka Point Structural Belt (Willsher Group). The recognition of abundant volcanic lithic fragments in the sandstone samples, combined with the pattern of detrital zircon ages (unimodal to bimodal 280–240 Ma age distribution), demonstrate that the upper Permian to Middle Triassic volcaniclastic successions were derived from a proximal arc source. The detrital zircon age spectra match magmatic pulses in the adjacent Tuhua Intrusives (Median Batholith), a conclusion similar to that recently proposed for the Brook Street Terrane (Grampian Formation) and Murihiku Terrane (Murihiku Supergroup). Trace-element data from the dated zircon grains provide further evidence for a Median Batholith source and cross-terrane provenance links. The data indicate that 275–230 Ma zircon grains from the Maitai Group, Willsher Group, and Murihiku Supergroup were derived from a common magmatic source, and that the late Permian Longwood Suite (261–252 Ma) in the Median Batholith was a source region for these terranes. Based on the cross-terrane provenance links, we suggest that the Brook Street and Murihiku terranes were deposited in the proximal part of a fore-arc basin, whereas the Dun Mountain-Maitai Terrane represents the distal part of the same basin. Sedimentation in the Maitai Group ceased during the Middle Triassic (∼238 Ma), likely in response to a period of orogenesis at 235–230 Ma (Gondwanide Orogeny) that is widely recognized throughout the southwest Pacific. • Origin of Permian to Triassic Central Arc terranes in New Zealand revealed. • Detrital zircons show abundant Permian-Triassic ages. • Ages and trace-element concentrations support a proximal Median Batholith source. • Central Arc terranes represent proximal and distal parts of the same fore-arc basin. • Distant and exotic sources for the Central Arc terranes are rejected." @default.
• W2979989490 created "2019-10-18" @default.
• W2979989490 creator A5020526902 @default.
• W2979989490 creator A5024929759 @default.
• W2979989490 creator A5046053996 @default.
• W2979989490 creator A5068128786 @default.
• W2979989490 date "2020-02-01" @default.
• W2979989490 modified "2023-09-24" @default.
• W2979989490 title "Origin of dispersed Permian–Triassic fore-arc basin terranes in New Zealand: Insights from zircon petrochronology" @default.
• W2979989490 cites W1173184726 @default.
• W2979989490 cites W1546566097 @default.
• W2979989490 cites W1591943409 @default.
• W2979989490 cites W1963553553 @default.
• W2979989490 cites W1972406684 @default.
• W2979989490 cites W1972435862 @default.
• W2979989490 cites W1977262338 @default.
• W2979989490 cites W1977567917 @default.
• W2979989490 cites W1983119510 @default.
• W2979989490 cites W1985146281 @default.
• W2979989490 cites W1985963616 @default.
• W2979989490 cites W1990944947 @default.
• W2979989490 cites W1997710040 @default.
• W2979989490 cites W1997922501 @default.
• W2979989490 cites W1998619769 @default.
• W2979989490 cites W1998670404 @default.
• W2979989490 cites W1999103708 @default.
• W2979989490 cites W1999457249 @default.
• W2979989490 cites W2000222261 @default.
• W2979989490 cites W2001328981 @default.
• W2979989490 cites W2008410977 @default.
• W2979989490 cites W2009732140 @default.
• W2979989490 cites W2011585485 @default.
• W2979989490 cites W2012192925 @default.
• W2979989490 cites W2018570345 @default.
• W2979989490 cites W2018904096 @default.
• W2979989490 cites W2020139762 @default.
• W2979989490 cites W2020316016 @default.
• W2979989490 cites W2028048720 @default.
• W2979989490 cites W2028051839 @default.
• W2979989490 cites W2028702576 @default.
• W2979989490 cites W2028916763 @default.
• W2979989490 cites W2029157156 @default.
• W2979989490 cites W2030539292 @default.
• W2979989490 cites W2031928338 @default.
• W2979989490 cites W2032913457 @default.
• W2979989490 cites W2036174339 @default.
• W2979989490 cites W2036407632 @default.
• W2979989490 cites W2039269540 @default.
• W2979989490 cites W2040974242 @default.
• W2979989490 cites W2042632350 @default.
• W2979989490 cites W2049125299 @default.
• W2979989490 cites W2052448030 @default.
• W2979989490 cites W2053554573 @default.
• W2979989490 cites W2053774838 @default.
• W2979989490 cites W2055297084 @default.
• W2979989490 cites W2055893814 @default.
• W2979989490 cites W2057465591 @default.
• W2979989490 cites W2060984305 @default.
• W2979989490 cites W2065084016 @default.
• W2979989490 cites W2069814390 @default.
• W2979989490 cites W2069873041 @default.
• W2979989490 cites W2072032787 @default.
• W2979989490 cites W2075694434 @default.
• W2979989490 cites W2075771493 @default.
• W2979989490 cites W2076555885 @default.
• W2979989490 cites W2078477853 @default.
• W2979989490 cites W2081840483 @default.
• W2979989490 cites W2087112906 @default.
• W2979989490 cites W2090632481 @default.
• W2979989490 cites W2093369526 @default.
• W2979989490 cites W2094786436 @default.
• W2979989490 cites W2095574320 @default.
• W2979989490 cites W2099928557 @default.
• W2979989490 cites W2100134346 @default.
• W2979989490 cites W2104848645 @default.
• W2979989490 cites W2112300806 @default.
• W2979989490 cites W2127306819 @default.
• W2979989490 cites W2127956008 @default.
• W2979989490 cites W2128377941 @default.
• W2979989490 cites W2129886013 @default.
• W2979989490 cites W2141754773 @default.
• W2979989490 cites W2149371043 @default.
• W2979989490 cites W2164336999 @default.
• W2979989490 cites W2169741359 @default.
• W2979989490 cites W2171086159 @default.
• W2979989490 cites W2249103379 @default.
• W2979989490 cites W2312255672 @default.
• W2979989490 cites W2321976203 @default.
• W2979989490 cites W2332480087 @default.
• W2979989490 cites W2332710300 @default.
• W2979989490 cites W2462928042 @default.
• W2979989490 cites W2517462965 @default.
• W2979989490 cites W2527875242 @default.
• W2979989490 cites W2553468700 @default.
• W2979989490 cites W2582517530 @default.
• W2979989490 cites W2789463631 @default.
• W2979989490 cites W2789563764 @default.
• W2979989490 cites W2800925354 @default.

• next