FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1981507744> ?p ?o ?g. }

• W1981507744 endingPage "250" @default.
• W1981507744 startingPage "237" @default.
• W1981507744 abstract "Pseudotachylitic breccias occur in the crater floor of large impact structures. Their origin is widely attributed either to shock melting and cataclasis during propagation of an impact shock wave, or to frictional melting and cataclasis during large slip displacements along crater collapse superfaults. By contrast, some models propose that the breccia matrices are allochthonous superheated melts from overlying impact melt sheets or from sites within the crater floor, which leaked into dilational fractures during collapse of the crater. In an effort to test these models, the compositions of pseudotachylite Sudbury breccias in the South Range of the Sudbury impact structure, Canada, were here compared to those of its associated impact melt sheet, the Sudbury Igneous Complex (SIC). The studied breccias occur along the contact between sandstone and a gabbro stock, and additional breccia bodies are located solely within these two lithologies. Major, trace element and lead isotope systematics suggest that the contact breccias are derived by mixing of comminuted gabbro and sandstone and that breccias hosted exclusively by sandstone or gabbro have compositions similar to their host rocks. The SIC has distinct chemical and isotopic compositions which argue strongly against the involvement of the impact melt sheet in the makeup of the breccias. Quartz and plagioclase in clasts and matrix of the breccias are transected by multiple microfractures and they have pervasive mosaic textures characterized by rolling and mottled undulatory extinction of micron-sized subgrain-like domains and new grains. These textures and strong local host control on chemical and clast composition of the breccias suggest that the breccias formed in situ by shock-induced compression and cataclasis of their host rocks during propagation of the shock wave." @default.
• W1981507744 created "2016-06-24" @default.
• W1981507744 creator A5054491836 @default.
• W1981507744 creator A5082781738 @default.
• W1981507744 date "2010-07-01" @default.
• W1981507744 modified "2023-09-26" @default.
• W1981507744 title "Geochemical and microstructural evidence for in situ formation of pseudotachylitic Sudbury breccia by shock-induced compression and cataclasis" @default.
• W1981507744 cites W1967643744 @default.
• W1981507744 cites W1982293316 @default.
• W1981507744 cites W1983329463 @default.
• W1981507744 cites W1997808792 @default.
• W1981507744 cites W2002561973 @default.
• W1981507744 cites W2005535576 @default.
• W1981507744 cites W2007576219 @default.
• W1981507744 cites W2008797959 @default.
• W1981507744 cites W2012292189 @default.
• W1981507744 cites W2016417839 @default.
• W1981507744 cites W2016626757 @default.
• W1981507744 cites W2018131961 @default.
• W1981507744 cites W2025394502 @default.
• W1981507744 cites W2026672764 @default.
• W1981507744 cites W2030190073 @default.
• W1981507744 cites W2033149971 @default.
• W1981507744 cites W2034743843 @default.
• W1981507744 cites W2034958048 @default.
• W1981507744 cites W2036359061 @default.
• W1981507744 cites W2037586440 @default.
• W1981507744 cites W2037949447 @default.
• W1981507744 cites W2040202166 @default.
• W1981507744 cites W2046469004 @default.
• W1981507744 cites W2049012957 @default.
• W1981507744 cites W2050170749 @default.
• W1981507744 cites W2050854129 @default.
• W1981507744 cites W2058459535 @default.
• W1981507744 cites W2058574057 @default.
• W1981507744 cites W2059527345 @default.
• W1981507744 cites W2062925415 @default.
• W1981507744 cites W2065652484 @default.
• W1981507744 cites W2067660692 @default.
• W1981507744 cites W2067943665 @default.
• W1981507744 cites W2075112830 @default.
• W1981507744 cites W2076478956 @default.
• W1981507744 cites W2076545873 @default.
• W1981507744 cites W2078445474 @default.
• W1981507744 cites W2079948708 @default.
• W1981507744 cites W2086583893 @default.
• W1981507744 cites W2089244744 @default.
• W1981507744 cites W2102946234 @default.
• W1981507744 cites W2120093654 @default.
• W1981507744 cites W2132465609 @default.
• W1981507744 cites W2145370114 @default.
• W1981507744 cites W2145886102 @default.
• W1981507744 cites W2146453254 @default.
• W1981507744 cites W2150152176 @default.
• W1981507744 cites W2152211844 @default.
• W1981507744 cites W2152775918 @default.
• W1981507744 cites W2154483101 @default.
• W1981507744 cites W2322853506 @default.
• W1981507744 cites W2425507503 @default.
• W1981507744 cites W2506290401 @default.
• W1981507744 cites W2909371221 @default.
• W1981507744 cites W2982121537 @default.
• W1981507744 cites W3172724518 @default.
• W1981507744 cites W4235862583 @default.
• W1981507744 cites W4236368760 @default.
• W1981507744 cites W4242655789 @default.
• W1981507744 cites W2343202066 @default.
• W1981507744 doi "https://doi.org/10.1016/j.precamres.2010.04.006" @default.
• W1981507744 hasPublicationYear "2010" @default.
• W1981507744 type Work @default.
• W1981507744 sameAs 1981507744 @default.
• W1981507744 citedByCount "19" @default.
• W1981507744 countsByYear W19815077442012 @default.
• W1981507744 countsByYear W19815077442014 @default.
• W1981507744 countsByYear W19815077442015 @default.
• W1981507744 countsByYear W19815077442016 @default.
• W1981507744 countsByYear W19815077442017 @default.
• W1981507744 countsByYear W19815077442018 @default.
• W1981507744 countsByYear W19815077442021 @default.
• W1981507744 crossrefType "journal-article" @default.
• W1981507744 hasAuthorship W1981507744A5054491836 @default.
• W1981507744 hasAuthorship W1981507744A5082781738 @default.
• W1981507744 hasConcept C121332964 @default.
• W1981507744 hasConcept C127313418 @default.
• W1981507744 hasConcept C138170599 @default.
• W1981507744 hasConcept C164421858 @default.
• W1981507744 hasConcept C165205528 @default.
• W1981507744 hasConcept C17409809 @default.
• W1981507744 hasConcept C175551986 @default.
• W1981507744 hasConcept C179537507 @default.
• W1981507744 hasConcept C2776779945 @default.
• W1981507744 hasConcept C42787717 @default.
• W1981507744 hasConcept C5900021 @default.
• W1981507744 hasConcept C62074269 @default.
• W1981507744 hasConcept C6494504 @default.
• W1981507744 hasConcept C79605941 @default.
• W1981507744 hasConcept C87355193 @default.
• W1981507744 hasConceptScore W1981507744C121332964 @default.

• next