FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2213805087> ?p ?o ?g. }

• W2213805087 endingPage "182" @default.
• W2213805087 startingPage "171" @default.
• W2213805087 abstract "The Kenting Mélange on the Hengchun Peninsula, Taiwan, formed through tectonic shearing of subduction complex lithologies, probably within the plate boundary subduction channel between the Eurasian and Philippine Sea plates, with further deformation and exhumation in the Pliocene–Pleistocene during arc–continent collision. Field relations reveal a structural gradation from normal stratified turbidite sequence (Mutan Formation) through broken formation to highly sheared Kenting Mélange containing allochthonous polygenic blocks. This gradation is consistent with an increase of average vitrinite reflection values from ~ 0.72% in the Mutan Formation through ~ 0.93% in the broken formation to ~ 0.99% in the mélange, suggesting temperatures of at least 140 °C during formation of the Kenting Mélange. Zircons from gabbro in the Kenting Mélange are dated as 25.46 ± 0.18 Ma, which together with geochemical data constrains the source to South China Sea oceanic lithosphere. In combination with the field relationships, vitrinite reflectance values, microfossil stratigraphy, and offshore geophysical data from S and SE Taiwan, we propose that the Kenting Mélange initially formed at the subduction plate boundary from off-scraped trench deposits. Minor Plio–Pleistocene microfossils (< 5%) occur within the mélange in proximity to slope basin of equivalent age and were likely sheared into the mélange during out-of-sequence thrusting associated with active arc–continent collision, which in the Hengchun Peninsula commenced after 6.5 Ma." @default.
• W2213805087 created "2016-06-24" @default.
• W2213805087 creator A5006685240 @default.
• W2213805087 creator A5018293422 @default.
• W2213805087 creator A5019420376 @default.
• W2213805087 creator A5040042361 @default.
• W2213805087 creator A5047961263 @default.
• W2213805087 creator A5051969604 @default.
• W2213805087 creator A5058364257 @default.
• W2213805087 creator A5060053337 @default.
• W2213805087 date "2016-10-01" @default.
• W2213805087 modified "2023-10-13" @default.
• W2213805087 title "From convergent plate margin to arc–continent collision: Formation of the Kenting Mélange, Southern Taiwan" @default.
• W2213805087 cites W1537905573 @default.
• W2213805087 cites W1573477650 @default.
• W2213805087 cites W1887845178 @default.
• W2213805087 cites W1967433944 @default.
• W2213805087 cites W1968400731 @default.
• W2213805087 cites W1978790888 @default.
• W2213805087 cites W1981277445 @default.
• W2213805087 cites W1985272941 @default.
• W2213805087 cites W1989945922 @default.
• W2213805087 cites W1990072225 @default.
• W2213805087 cites W1990930822 @default.
• W2213805087 cites W1991465327 @default.
• W2213805087 cites W1996489529 @default.
• W2213805087 cites W1997127344 @default.
• W2213805087 cites W1999282809 @default.
• W2213805087 cites W2000272642 @default.
• W2213805087 cites W2002093296 @default.
• W2213805087 cites W2009251618 @default.
• W2213805087 cites W2009892449 @default.
• W2213805087 cites W2011033027 @default.
• W2213805087 cites W2014138134 @default.
• W2213805087 cites W2019301011 @default.
• W2213805087 cites W2023273714 @default.
• W2213805087 cites W2026315254 @default.
• W2213805087 cites W2026616005 @default.
• W2213805087 cites W2032048614 @default.
• W2213805087 cites W2039872199 @default.
• W2213805087 cites W2045047354 @default.
• W2213805087 cites W2046255605 @default.
• W2213805087 cites W2046696482 @default.
• W2213805087 cites W2048280282 @default.
• W2213805087 cites W2051858811 @default.
• W2213805087 cites W2058219615 @default.
• W2213805087 cites W2059231219 @default.
• W2213805087 cites W2059856849 @default.
• W2213805087 cites W2063295640 @default.
• W2213805087 cites W2066854245 @default.
• W2213805087 cites W2071339220 @default.
• W2213805087 cites W2071538549 @default.
• W2213805087 cites W2077291550 @default.
• W2213805087 cites W2082181291 @default.
• W2213805087 cites W2084173218 @default.
• W2213805087 cites W2088063869 @default.
• W2213805087 cites W2110035089 @default.
• W2213805087 cites W2112256322 @default.
• W2213805087 cites W2121097807 @default.
• W2213805087 cites W2135488750 @default.
• W2213805087 cites W2143501565 @default.
• W2213805087 cites W2149321179 @default.
• W2213805087 cites W2156841285 @default.
• W2213805087 cites W2323365704 @default.
• W2213805087 cites W2326185685 @default.
• W2213805087 cites W4210999665 @default.
• W2213805087 cites W4235236582 @default.
• W2213805087 cites W4246646556 @default.
• W2213805087 cites W4253952146 @default.
• W2213805087 cites W4300998818 @default.
• W2213805087 doi "https://doi.org/10.1016/j.gr.2015.11.010" @default.
• W2213805087 hasPublicationYear "2016" @default.
• W2213805087 type Work @default.
• W2213805087 sameAs 2213805087 @default.
• W2213805087 citedByCount "21" @default.
• W2213805087 countsByYear W22138050872017 @default.
• W2213805087 countsByYear W22138050872018 @default.
• W2213805087 countsByYear W22138050872019 @default.
• W2213805087 countsByYear W22138050872020 @default.
• W2213805087 countsByYear W22138050872021 @default.
• W2213805087 countsByYear W22138050872022 @default.
• W2213805087 countsByYear W22138050872023 @default.
• W2213805087 crossrefType "journal-article" @default.
• W2213805087 hasAuthorship W2213805087A5006685240 @default.
• W2213805087 hasAuthorship W2213805087A5018293422 @default.
• W2213805087 hasAuthorship W2213805087A5019420376 @default.
• W2213805087 hasAuthorship W2213805087A5040042361 @default.
• W2213805087 hasAuthorship W2213805087A5047961263 @default.
• W2213805087 hasAuthorship W2213805087A5051969604 @default.
• W2213805087 hasAuthorship W2213805087A5058364257 @default.
• W2213805087 hasAuthorship W2213805087A5060053337 @default.
• W2213805087 hasBestOaLocation W22138050872 @default.
• W2213805087 hasConcept C119477230 @default.
• W2213805087 hasConcept C127313418 @default.
• W2213805087 hasConcept C151730666 @default.
• W2213805087 hasConcept C16942324 @default.
• W2213805087 hasConcept C2778261408 @default.
• W2213805087 hasConcept C58097730 @default.

• next