FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2142618863> ?p ?o ?g. }

• W2142618863 abstract "Isobaric crystallization paths obtained from phase equilibrium experiments show that, whereas in rhyolitic compositions melt fraction trends are distinctly eutectic-like, dacitic and more mafic compositions have their crystallinities linearly correlated with temperature. As a consequence, the viscosities of the latter continuously increase on cooling, whereas for the former they remain constant or even decrease during 80% of the crystallisation interval, which opens new perspectives for the fluid dynamical modeling of felsic magma chambers. Given the typical dike widths observed for basaltic magmas, results of analogue modelling predict that injection of mafic magmas into crystallizing intermediate to silicic plutons under pre-eruption conditions cannot yield homogeneous composition. Homogenization can occur, however, if injection takes place in the early stages of magmatic evolution (i.e. at near liquidus conditions) but only in magmas of dacitic or more mafic composition. More generally, the potential for efficient mixing between silicic and mafic magmas sharing large interfaces at upper crustal levels is greater for dry basalts than for wet ones. At the other extreme, small mafic enclaves found in many granitoids behave essentially as rigid objects during a substantial part of the crystallization interval of the host magmas which implies that finite strain analyses carried out on such markers can give only a minimum estimate of the total amount of strain experienced by the host pluton. Mafic enclaves carried by granitic magmas behave as passive markers only at near solidus conditions, typically when the host granitic magma shows near-solid behavior. Thus they cannot be used as fossil indicators of direction of magmatic flow." @default.
• W2142618863 created "2016-06-24" @default.
• W2142618863 creator A5007927797 @default.
• W2142618863 creator A5020579129 @default.
• W2142618863 creator A5047374378 @default.
• W2142618863 creator A5052189114 @default.
• W2142618863 creator A5084877434 @default.
• W2142618863 date "2000-01-01" @default.
• W2142618863 modified "2023-10-18" @default.
• W2142618863 title "Phase equilibrium constraints on the viscosity of silicic magmas II: implications for mafic-silicic mixing processes" @default.
• W2142618863 cites W1766351626 @default.
• W2142618863 cites W1966016940 @default.
• W2142618863 cites W1966049997 @default.
• W2142618863 cites W1967277465 @default.
• W2142618863 cites W1975359521 @default.
• W2142618863 cites W1985757647 @default.
• W2142618863 cites W1988901849 @default.
• W2142618863 cites W1989157061 @default.
• W2142618863 cites W1995137849 @default.
• W2142618863 cites W1997120104 @default.
• W2142618863 cites W1998127602 @default.
• W2142618863 cites W2002333091 @default.
• W2142618863 cites W2003778536 @default.
• W2142618863 cites W2009350887 @default.
• W2142618863 cites W2012366370 @default.
• W2142618863 cites W2017853565 @default.
• W2142618863 cites W2019922981 @default.
• W2142618863 cites W2021566918 @default.
• W2142618863 cites W2022999289 @default.
• W2142618863 cites W2023027524 @default.
• W2142618863 cites W2023388876 @default.
• W2142618863 cites W2031433824 @default.
• W2142618863 cites W2036643521 @default.
• W2142618863 cites W2038116891 @default.
• W2142618863 cites W2039039175 @default.
• W2142618863 cites W2039291242 @default.
• W2142618863 cites W2040120198 @default.
• W2142618863 cites W2040229988 @default.
• W2142618863 cites W2042782943 @default.
• W2142618863 cites W2044921168 @default.
• W2142618863 cites W2047379211 @default.
• W2142618863 cites W2053483240 @default.
• W2142618863 cites W2056222688 @default.
• W2142618863 cites W2057015318 @default.
• W2142618863 cites W2060588282 @default.
• W2142618863 cites W2061687281 @default.
• W2142618863 cites W2064576840 @default.
• W2142618863 cites W2064594654 @default.
• W2142618863 cites W2065291589 @default.
• W2142618863 cites W2066319722 @default.
• W2142618863 cites W2070891266 @default.
• W2142618863 cites W2072520558 @default.
• W2142618863 cites W2073137830 @default.
• W2142618863 cites W2075358942 @default.
• W2142618863 cites W2075607939 @default.
• W2142618863 cites W2076024715 @default.
• W2142618863 cites W2076133913 @default.
• W2142618863 cites W2076291146 @default.
• W2142618863 cites W2077938222 @default.
• W2142618863 cites W2079096856 @default.
• W2142618863 cites W2081979169 @default.
• W2142618863 cites W2093854966 @default.
• W2142618863 cites W2096317422 @default.
• W2142618863 cites W2097386223 @default.
• W2142618863 cites W2100971915 @default.
• W2142618863 cites W2113652797 @default.
• W2142618863 cites W2116842517 @default.
• W2142618863 cites W2120027408 @default.
• W2142618863 cites W2120417186 @default.
• W2142618863 cites W2136694854 @default.
• W2142618863 cites W2144308418 @default.
• W2142618863 cites W2145757049 @default.
• W2142618863 cites W2152984700 @default.
• W2142618863 cites W2158966664 @default.
• W2142618863 cites W2162620695 @default.
• W2142618863 cites W2164828314 @default.
• W2142618863 cites W2165073556 @default.
• W2142618863 cites W2166672836 @default.
• W2142618863 cites W2166916464 @default.
• W2142618863 cites W2170736074 @default.
• W2142618863 cites W2314927530 @default.
• W2142618863 cites W2316472930 @default.
• W2142618863 cites W2316671008 @default.
• W2142618863 cites W2318148662 @default.
• W2142618863 cites W2330027823 @default.
• W2142618863 cites W2333498558 @default.
• W2142618863 cites W2334149841 @default.
• W2142618863 cites W2345212905 @default.
• W2142618863 cites W2582267311 @default.
• W2142618863 cites W2595030482 @default.
• W2142618863 cites W2964580412 @default.
• W2142618863 cites W3013022097 @default.
• W2142618863 cites W35974805 @default.
• W2142618863 cites W53807892 @default.
• W2142618863 cites W654391659 @default.
• W2142618863 doi "https://doi.org/10.1130/0-8137-2350-7.61" @default.
• W2142618863 hasPublicationYear "2000" @default.
• W2142618863 type Work @default.
• W2142618863 sameAs 2142618863 @default.
• W2142618863 citedByCount "5" @default.

• next