Matches in SemOpenAlex for { <https://semopenalex.org/work/W1582389967> ?p ?o ?g. }
- W1582389967 endingPage "782" @default.
- W1582389967 startingPage "759" @default.
- W1582389967 abstract "Abstract– The 1.4–1.6 km thick Onaping Formation consists of a complex series of breccias and “melt bodies” lying above the Sudbury Igneous Complex (SIC) at the Sudbury impact structure. Based on the presence of shocked lithic clasts and various “glassy” phases, the Onaping has been described as a “suevitic” breccia, with an origin, at least in part, as fallback material. Recent mapping and a redefined stratigraphy have emphasized similarities and differences in its various vitric phases, both as clast types and discrete intrusive bodies. The nature of the Onaping and that of other “suevitic” breccias overlying impact melt sheets is reviewed. The relative thickness, internal stratigraphic and lithological character, and the relative chronology of depositional units indicate multiple processes were involved over some time in the formation of the Onaping. The Sudbury structure formed in a foreland basin and water played an essential role in the evolution of the Onaping, as indicated by a major hydrothermal system generated during its formation. Taken together, observations and interpretations of the Onaping suggest a working hypothesis for the origin of the Onaping that includes not only impact but also the interaction of sea water with the impact melt, resulting in repeated explosive interactions involving proto‐SIC materials and mixing with pre‐existing lithologies. This is complicated by additional brecciation events due to the intrusion of proto‐SIC materials into the evolving and thickening Onaping. Fragmentation mechanisms changed as the system evolved and involved vesiculation in the formation of the upper two‐thirds of the Onaping." @default.
- W1582389967 created "2016-06-24" @default.
- W1582389967 creator A5011656018 @default.
- W1582389967 creator A5021128023 @default.
- W1582389967 creator A5041778168 @default.
- W1582389967 creator A5075863032 @default.
- W1582389967 date "2010-05-01" @default.
- W1582389967 modified "2023-10-16" @default.
- W1582389967 title "The evolution of the Onaping Formation at the Sudbury impact structure" @default.
- W1582389967 cites W1040455331 @default.
- W1582389967 cites W106779635 @default.
- W1582389967 cites W155799165 @default.
- W1582389967 cites W1602031712 @default.
- W1582389967 cites W1844508952 @default.
- W1582389967 cites W1849652885 @default.
- W1582389967 cites W1864080569 @default.
- W1582389967 cites W1868871564 @default.
- W1582389967 cites W1877791016 @default.
- W1582389967 cites W1918170160 @default.
- W1582389967 cites W1963600106 @default.
- W1582389967 cites W1963900954 @default.
- W1582389967 cites W1969551930 @default.
- W1582389967 cites W1974243758 @default.
- W1582389967 cites W1978601643 @default.
- W1582389967 cites W1981131918 @default.
- W1582389967 cites W1981240295 @default.
- W1582389967 cites W1988244014 @default.
- W1582389967 cites W1990682754 @default.
- W1582389967 cites W1991959591 @default.
- W1582389967 cites W1994964418 @default.
- W1582389967 cites W1999988027 @default.
- W1582389967 cites W2001362602 @default.
- W1582389967 cites W2002561973 @default.
- W1582389967 cites W2003517088 @default.
- W1582389967 cites W2009291478 @default.
- W1582389967 cites W2009493807 @default.
- W1582389967 cites W2016417839 @default.
- W1582389967 cites W2017207473 @default.
- W1582389967 cites W2018093853 @default.
- W1582389967 cites W2024404983 @default.
- W1582389967 cites W2029917473 @default.
- W1582389967 cites W2030911183 @default.
- W1582389967 cites W2034958048 @default.
- W1582389967 cites W2035957886 @default.
- W1582389967 cites W2037151532 @default.
- W1582389967 cites W2037543813 @default.
- W1582389967 cites W2041042258 @default.
- W1582389967 cites W2042786792 @default.
- W1582389967 cites W2047083864 @default.
- W1582389967 cites W2050079883 @default.
- W1582389967 cites W2051818406 @default.
- W1582389967 cites W2052586810 @default.
- W1582389967 cites W2054057267 @default.
- W1582389967 cites W2056861465 @default.
- W1582389967 cites W2058574057 @default.
- W1582389967 cites W2061977623 @default.
- W1582389967 cites W2067062916 @default.
- W1582389967 cites W2069113674 @default.
- W1582389967 cites W2075579994 @default.
- W1582389967 cites W2077642718 @default.
- W1582389967 cites W2078445474 @default.
- W1582389967 cites W2079366015 @default.
- W1582389967 cites W2081991350 @default.
- W1582389967 cites W2087774564 @default.
- W1582389967 cites W2087864763 @default.
- W1582389967 cites W2088938774 @default.
- W1582389967 cites W2089130118 @default.
- W1582389967 cites W2098975399 @default.
- W1582389967 cites W2099825957 @default.
- W1582389967 cites W2102946234 @default.
- W1582389967 cites W2104366357 @default.
- W1582389967 cites W2107582290 @default.
- W1582389967 cites W2116068614 @default.
- W1582389967 cites W2118767380 @default.
- W1582389967 cites W2120093654 @default.
- W1582389967 cites W2129503458 @default.
- W1582389967 cites W2132465609 @default.
- W1582389967 cites W2146237195 @default.
- W1582389967 cites W2147319692 @default.
- W1582389967 cites W2148336119 @default.
- W1582389967 cites W2169098086 @default.
- W1582389967 cites W2263924161 @default.
- W1582389967 cites W2303001831 @default.
- W1582389967 cites W2981402139 @default.
- W1582389967 cites W2981680584 @default.
- W1582389967 cites W2981725662 @default.
- W1582389967 cites W4230369783 @default.
- W1582389967 cites W4233364700 @default.
- W1582389967 cites W4240200058 @default.
- W1582389967 cites W4245828692 @default.
- W1582389967 doi "https://doi.org/10.1111/j.1945-5100.2010.01057.x" @default.
- W1582389967 hasPublicationYear "2010" @default.
- W1582389967 type Work @default.
- W1582389967 sameAs 1582389967 @default.
- W1582389967 citedByCount "87" @default.
- W1582389967 countsByYear W15823899672012 @default.
- W1582389967 countsByYear W15823899672013 @default.
- W1582389967 countsByYear W15823899672014 @default.