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• W2000501185 abstract "Using a random thermal perturbation (RTP) model this study investigates the process of magmatic segmentation along mid-oceanic ridge (MOR) axes as a function of the upwelling dynamics, controlled by coupled solidification–melting processes. The RTP model suggests that the variation in along-axis velocity (VL) fields constitutes the underlying mechanism of segmentation in natural MORs, showing temperature variations within a steady-state range, irrespective of large initial thermal perturbations imposed at the model base. The VL patterns are initially transient, characterized by multi-order segments, but attain a stable configuration with dominantly large segments (average size ~ 100 km) within a time scale of 2.3 Ma. Buoyant-melt driven thermal convection explains this transient segmentation. Small scale convection cells are found to be progressively consumed by larger cells, resulting in a stable convection structure over a similar time scale. Slow- and fast-spreading ridges (SSR and FSR) undergo upwelling with contrasting melt flow patterns. SSRs involve melt feeding into the ridge axis by horizontal flows from segment centers, trailing into large-scale conduits at an early stage. With time, vertical upwelling occurs throughout the segment. In the case of FSRs, both melt supply avenues prevail throughout their development. We also evaluate the variation of the across-axis flow velocity (VT) to investigate the mode of geometric evolution of MORs. Time series VT maps suggest that a ridge structure develops through localization of discrete axes (VT = 0) with offsets varying up to 15 km, which coalesce with one another to form a single axis. The matured ridge, however, retains higher-order offsets (up to 9 km)." @default.
• W2000501185 created "2016-06-24" @default.
• W2000501185 creator A5001408530 @default.
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• W2000501185 date "2014-12-01" @default.
• W2000501185 modified "2023-09-24" @default.
• W2000501185 title "Role of random thermal perturbations in the magmatic segmentation of mid-oceanic ridges: Insights from numerical simulations" @default.
• W2000501185 cites W1488681283 @default.
• W2000501185 cites W1531469288 @default.
• W2000501185 cites W1539943143 @default.
• W2000501185 cites W1601648958 @default.
• W2000501185 cites W160959246 @default.
• W2000501185 cites W1617369392 @default.
• W2000501185 cites W1875581837 @default.
• W2000501185 cites W1963555616 @default.
• W2000501185 cites W1966116805 @default.
• W2000501185 cites W1968871698 @default.
• W2000501185 cites W1970934067 @default.
• W2000501185 cites W1972209752 @default.
• W2000501185 cites W1977660954 @default.
• W2000501185 cites W1981101269 @default.
• W2000501185 cites W1981263149 @default.
• W2000501185 cites W1985850387 @default.
• W2000501185 cites W1986595641 @default.
• W2000501185 cites W1987180374 @default.
• W2000501185 cites W1993079962 @default.
• W2000501185 cites W1994200129 @default.
• W2000501185 cites W1996869230 @default.
• W2000501185 cites W1998777945 @default.
• W2000501185 cites W2001708826 @default.
• W2000501185 cites W2002655741 @default.
• W2000501185 cites W2002748313 @default.
• W2000501185 cites W2005518861 @default.
• W2000501185 cites W2007868664 @default.
• W2000501185 cites W2008375596 @default.
• W2000501185 cites W2011497196 @default.
• W2000501185 cites W2011991514 @default.
• W2000501185 cites W2018170563 @default.
• W2000501185 cites W2022813251 @default.
• W2000501185 cites W2024828229 @default.
• W2000501185 cites W2027411021 @default.
• W2000501185 cites W2032584964 @default.
• W2000501185 cites W2033724743 @default.
• W2000501185 cites W2035743760 @default.
• W2000501185 cites W2038658947 @default.
• W2000501185 cites W2041206278 @default.
• W2000501185 cites W2044040724 @default.
• W2000501185 cites W2048824368 @default.
• W2000501185 cites W2049250499 @default.
• W2000501185 cites W2049266330 @default.
• W2000501185 cites W2049923710 @default.
• W2000501185 cites W2050694319 @default.
• W2000501185 cites W2053023627 @default.
• W2000501185 cites W2054451772 @default.
• W2000501185 cites W2061218983 @default.
• W2000501185 cites W2063335147 @default.
• W2000501185 cites W2069739846 @default.
• W2000501185 cites W2069800672 @default.
• W2000501185 cites W2073316080 @default.
• W2000501185 cites W2075845557 @default.
• W2000501185 cites W2076399414 @default.
• W2000501185 cites W2078840355 @default.
• W2000501185 cites W2084803447 @default.
• W2000501185 cites W2086421861 @default.
• W2000501185 cites W2087663267 @default.
• W2000501185 cites W2087782562 @default.
• W2000501185 cites W2088678792 @default.
• W2000501185 cites W2090086577 @default.
• W2000501185 cites W2090132951 @default.
• W2000501185 cites W2093428530 @default.
• W2000501185 cites W2105607777 @default.
• W2000501185 cites W2107283728 @default.
• W2000501185 cites W2107316430 @default.
• W2000501185 cites W2107456128 @default.
• W2000501185 cites W2107748470 @default.
• W2000501185 cites W2114660893 @default.
• W2000501185 cites W2115698243 @default.
• W2000501185 cites W2124340013 @default.
• W2000501185 cites W2125105073 @default.
• W2000501185 cites W2127192349 @default.
• W2000501185 cites W2128110973 @default.
• W2000501185 cites W2147674969 @default.
• W2000501185 cites W2151532008 @default.
• W2000501185 cites W2158520166 @default.
• W2000501185 cites W2162046601 @default.
• W2000501185 cites W2170859064 @default.
• W2000501185 cites W2316687406 @default.
• W2000501185 cites W282884945 @default.
• W2000501185 cites W3103104081 @default.
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• W2000501185 doi "https://doi.org/10.1016/j.tecto.2014.08.008" @default.
• W2000501185 hasPublicationYear "2014" @default.
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