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• W3208079622 endingPage "100004" @default.
• W3208079622 startingPage "100004" @default.
• W3208079622 abstract "A global compilation of structural, lithological, and geochemical data on a selection of Archean, Proterozoic and Phanerozoic magmatic complexes, interpreted as ophiolites, is presented. Ophiolites, based on Phanerozoic examples, can be classified into subduction-related and subduction unrelated categories. These categories can be further subdivided into several subtypes depending on the proximity to subduction zones, and on sequential development from rifting – drifting to seafloor spreading for the subduction-unrelated category. From bottom to top ophiolites exhibit a magmatic sequence of ultramafic rocks (upper mantle units), gabbros (layered and isotropic), basaltic dikes and lavas, as well as boninites and felsic dikes and lavas in the subduction-related types. Archean greenstone belts show large variations in their construction, but Eoarchean examples display identical structure and lithology to the Phanerozoic ophiolites, attesting to the operation of seafloor spreading and subduction zone processes in the early Earth's history. Lithological differences between the Archean and Proterozoic/Phanerozoic ophiolites are demonstrated in the common occurrence of komatiites and felsic rocks, and scarcity of sheeted dike complexes in the former, compared to the opposite situation in those ophiolites that are younger than ca. 2 Ga. Geochemically there is a concomitant decrease in the content of incompatible elements (e.g., Sr, Zr, Y, Nb) and an increase in the content of compatible elements (e.g., Mg, Cr, Ni). In terms of tectonic environment analyzes, the Archean ophiolites are more abundantly subduction-related than those of Proterozoic and Phanerozoic ages. The subduction-dominant Archean oceanic crust (ophiolites) was characterized by accretionary cycle plate tectonics, whereas for those of Proterozoic and Phanerozoic ages, a combination of both accretionary cycle and Wilson cycles plate tectonic processes was operative." @default.
• W3208079622 created "2021-11-08" @default.
• W3208079622 creator A5000607739 @default.
• W3208079622 creator A5084944585 @default.
• W3208079622 date "2022-02-01" @default.
• W3208079622 modified "2023-10-18" @default.
• W3208079622 title "Archean versus Phanerozoic oceanic crust formation and tectonics: Ophiolites through time" @default.
• W3208079622 cites W1554942427 @default.
• W3208079622 cites W1706860248 @default.
• W3208079622 cites W1963641775 @default.
• W3208079622 cites W1965954133 @default.
• W3208079622 cites W1969845853 @default.
• W3208079622 cites W1970441873 @default.
• W3208079622 cites W1972365683 @default.
• W3208079622 cites W1974639462 @default.
• W3208079622 cites W1978695522 @default.
• W3208079622 cites W1978795897 @default.
• W3208079622 cites W1979053860 @default.
• W3208079622 cites W1982250032 @default.
• W3208079622 cites W1986697722 @default.
• W3208079622 cites W1986708376 @default.
• W3208079622 cites W1989000069 @default.
• W3208079622 cites W1991149004 @default.
• W3208079622 cites W1991392138 @default.
• W3208079622 cites W1992364224 @default.
• W3208079622 cites W1995318237 @default.
• W3208079622 cites W1995926234 @default.
• W3208079622 cites W1996269705 @default.
• W3208079622 cites W2002036245 @default.
• W3208079622 cites W2006234070 @default.
• W3208079622 cites W2007789349 @default.
• W3208079622 cites W2010741958 @default.
• W3208079622 cites W2011353554 @default.
• W3208079622 cites W2014591826 @default.
• W3208079622 cites W2015705273 @default.
• W3208079622 cites W2017840788 @default.
• W3208079622 cites W2018122760 @default.
• W3208079622 cites W2018172800 @default.
• W3208079622 cites W2022129348 @default.
• W3208079622 cites W2028592756 @default.
• W3208079622 cites W2029436233 @default.
• W3208079622 cites W2030355408 @default.
• W3208079622 cites W2034140923 @default.
• W3208079622 cites W2036578808 @default.
• W3208079622 cites W2038515530 @default.
• W3208079622 cites W2039238210 @default.
• W3208079622 cites W2042619191 @default.
• W3208079622 cites W2042904816 @default.
• W3208079622 cites W2044871538 @default.
• W3208079622 cites W2045857800 @default.
• W3208079622 cites W2045859284 @default.
• W3208079622 cites W2047396493 @default.
• W3208079622 cites W2047988432 @default.
• W3208079622 cites W2048068769 @default.
• W3208079622 cites W2052473341 @default.
• W3208079622 cites W2060557773 @default.
• W3208079622 cites W2060823328 @default.
• W3208079622 cites W2064250866 @default.
• W3208079622 cites W2064546576 @default.
• W3208079622 cites W2067832480 @default.
• W3208079622 cites W2071551683 @default.
• W3208079622 cites W2071863023 @default.
• W3208079622 cites W2073878298 @default.
• W3208079622 cites W2078163081 @default.
• W3208079622 cites W2081558748 @default.
• W3208079622 cites W2082276281 @default.
• W3208079622 cites W2088934812 @default.
• W3208079622 cites W2096648343 @default.
• W3208079622 cites W2099509181 @default.
• W3208079622 cites W2103592949 @default.
• W3208079622 cites W2115858402 @default.
• W3208079622 cites W2117716354 @default.
• W3208079622 cites W2121696953 @default.
• W3208079622 cites W2135651322 @default.
• W3208079622 cites W2137159697 @default.
• W3208079622 cites W2138990875 @default.
• W3208079622 cites W2145191782 @default.
• W3208079622 cites W2149170224 @default.
• W3208079622 cites W2150540247 @default.
• W3208079622 cites W2150629216 @default.
• W3208079622 cites W2151802570 @default.
• W3208079622 cites W2152588796 @default.
• W3208079622 cites W2161188118 @default.
• W3208079622 cites W2161493148 @default.
• W3208079622 cites W2198487632 @default.
• W3208079622 cites W2214863082 @default.
• W3208079622 cites W2283066148 @default.
• W3208079622 cites W2312828419 @default.
• W3208079622 cites W2523510373 @default.
• W3208079622 cites W2571354911 @default.
• W3208079622 cites W2571377934 @default.
• W3208079622 cites W2767094872 @default.
• W3208079622 cites W2783101039 @default.
• W3208079622 cites W2795895851 @default.
• W3208079622 cites W2801526877 @default.
• W3208079622 cites W2911465852 @default.
• W3208079622 cites W2915484243 @default.
• W3208079622 cites W2918181441 @default.

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