FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2916855272> ?p ?o ?g. }

• W2916855272 endingPage "1707" @default.
• W2916855272 startingPage "1689" @default.
• W2916855272 abstract "The southern West Junggar terrane in the south‐western Central Asian Orogenic Belt (CAOB) is mainly composed of accretionary complexes and characterized by widespread outcrops of ophiolitic mélanges in the Barleik, Mayile, and Tangbale (BMT) areas, representing the site of consumption of the Junggar–Balkhash Ocean. However, due to a lack of comprehensive synthesis of the ophiolitic mélanges, the early evolution of the Junggar–Balkhash Ocean remains poorly understood. This paper first focuses on the little‐known Barleik ophiolitic blocks and associated pillow basalts and then integrates the Barleik, Mayile, and Tangbale ophiolitic mélanges into one model. Mineral and whole‐rock chemistry suggests that the Barleik ophiolitic blocks, including serpentinized dunite, clinopyroxenite, and gabbro, show supra‐subduction zone (SSZ) affinities, as indicated by high Cr # values (76–78) in spinels and strong depletion in Nb, Ta, Zr, and Hf, whereas the Barleik pillow basalts are alkaline and have high TiO 2 contents (2.82–3.42 wt.%) and Nb–Ta enrichment, similar to ocean‐island basalt (OIB) lavas. Combined with published chronological and chemical data from ophiolites, metamorphic rocks, and arc plutons, we propose that the BMT Ediacaran to middle Cambrian ophiolitic gabbros were formed in a SSZ environment, implying a single Mariana‐type arc system within the Junggar–Balkhash Ocean, which was coeval with an Andean‐type arc system in the Kyrgyz North Tianshan, supporting an archipelagic model for the south‐western CAOB. By contrast, the BMT OIB‐type basalts are early Silurian in age, much younger than the SSZ‐type ophiolites, and can be interpreted as relicts of seamounts. Thus, a model involving the Ediacaran to Ordovician intra‐oceanic subduction and late Silurian to Early Devonian seamount accretion is helpful for clarifying the different components of the accretionary complexes in the southern West Junggar terrane." @default.
• W2916855272 created "2019-03-02" @default.
• W2916855272 creator A5000511656 @default.
• W2916855272 creator A5003966673 @default.
• W2916855272 creator A5020054349 @default.
• W2916855272 creator A5060990890 @default.
• W2916855272 creator A5069714324 @default.
• W2916855272 date "2019-02-18" @default.
• W2916855272 modified "2023-10-14" @default.
• W2916855272 title "The <scp>E</scp> diacaran to <scp>E</scp> arly <scp>P</scp> alaeozoic evolution of the <scp>J</scp> unggar– <scp>B</scp> alkhash <scp>O</scp> cean: <scp>A</scp> synthesis of the ophiolitic mélanges in the southern West <scp>J</scp> unggar terrane, <scp>NW C</scp> hina" @default.
• W2916855272 cites W1468127994 @default.
• W2916855272 cites W1548039205 @default.
• W2916855272 cites W1754007230 @default.
• W2916855272 cites W1925397053 @default.
• W2916855272 cites W1964909252 @default.
• W2916855272 cites W1965917434 @default.
• W2916855272 cites W1966081220 @default.
• W2916855272 cites W1969845853 @default.
• W2916855272 cites W1976304054 @default.
• W2916855272 cites W1981435036 @default.
• W2916855272 cites W1992832689 @default.
• W2916855272 cites W1999448338 @default.
• W2916855272 cites W2002229468 @default.
• W2916855272 cites W2003323528 @default.
• W2916855272 cites W2007061988 @default.
• W2916855272 cites W2008313305 @default.
• W2916855272 cites W2010539007 @default.
• W2916855272 cites W2011987758 @default.
• W2916855272 cites W2018995159 @default.
• W2916855272 cites W2023621032 @default.
• W2916855272 cites W2024808576 @default.
• W2916855272 cites W2026771566 @default.
• W2916855272 cites W2034223887 @default.
• W2916855272 cites W2036629009 @default.
• W2916855272 cites W2040372579 @default.
• W2916855272 cites W2044934678 @default.
• W2916855272 cites W2060157729 @default.
• W2916855272 cites W2063734888 @default.
• W2916855272 cites W2063902937 @default.
• W2916855272 cites W2065065857 @default.
• W2916855272 cites W2078876741 @default.
• W2916855272 cites W2079291552 @default.
• W2916855272 cites W2079767098 @default.
• W2916855272 cites W2080207234 @default.
• W2916855272 cites W2081408732 @default.
• W2916855272 cites W2081677058 @default.
• W2916855272 cites W2082193606 @default.
• W2916855272 cites W2089096123 @default.
• W2916855272 cites W2099905971 @default.
• W2916855272 cites W2103463307 @default.
• W2916855272 cites W2111016941 @default.
• W2916855272 cites W2112435406 @default.
• W2916855272 cites W2117577007 @default.
• W2916855272 cites W2122467685 @default.
• W2916855272 cites W2124044757 @default.
• W2916855272 cites W2124276467 @default.
• W2916855272 cites W2130869872 @default.
• W2916855272 cites W2135384477 @default.
• W2916855272 cites W2137236289 @default.
• W2916855272 cites W2138522501 @default.
• W2916855272 cites W2143093330 @default.
• W2916855272 cites W2161188118 @default.
• W2916855272 cites W2162334444 @default.
• W2916855272 cites W2165094726 @default.
• W2916855272 cites W2169016685 @default.
• W2916855272 cites W2169769753 @default.
• W2916855272 cites W2185496340 @default.
• W2916855272 cites W2305936762 @default.
• W2916855272 cites W2415374936 @default.
• W2916855272 cites W2562357877 @default.
• W2916855272 cites W2568738151 @default.
• W2916855272 cites W2594742725 @default.
• W2916855272 cites W2598113169 @default.
• W2916855272 cites W2752632365 @default.
• W2916855272 cites W2770949227 @default.
• W2916855272 cites W2779441898 @default.
• W2916855272 cites W2790624819 @default.
• W2916855272 cites W2889216838 @default.
• W2916855272 cites W2899588773 @default.
• W2916855272 cites W2903225957 @default.
• W2916855272 doi "https://doi.org/10.1002/gj.3475" @default.
• W2916855272 hasPublicationYear "2019" @default.
• W2916855272 type Work @default.
• W2916855272 sameAs 2916855272 @default.
• W2916855272 citedByCount "15" @default.
• W2916855272 countsByYear W29168552722019 @default.
• W2916855272 countsByYear W29168552722020 @default.
• W2916855272 countsByYear W29168552722021 @default.
• W2916855272 countsByYear W29168552722023 @default.
• W2916855272 crossrefType "journal-article" @default.
• W2916855272 hasAuthorship W2916855272A5000511656 @default.
• W2916855272 hasAuthorship W2916855272A5003966673 @default.
• W2916855272 hasAuthorship W2916855272A5020054349 @default.
• W2916855272 hasAuthorship W2916855272A5060990890 @default.
• W2916855272 hasAuthorship W2916855272A5069714324 @default.
• W2916855272 hasConcept C120806208 @default.
• W2916855272 hasConcept C127313418 @default.
• W2916855272 hasConcept C150999391 @default.

• next