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• W2073876147 abstract "The calc-alkaline granitoids of the central Sierra Nevada batholith are associated with abundant mafic rocks. These include both country-rock xenoliths and mafic magmatic enclaves (MME) that commonly have fine-grained and, less commonly, cumulate textures. Scarce composite enclaves consist of either xenoliths enclosed in MME, or of MME enclosed in other MME with different grain size and texture. Enclaves are often enclosed in mafic aggregates and form meter-size polygenic swarms, mostly in the margins of normally zoned plutons. Enclaves may locally divert schlieren layering. Mafic dikes, which also occur in swarms, are undisturbed, composite, or largely hybridized. In central Sierra Nevada, with the exception of xenoliths that completely differ from the other rocks, host granitoids, mafic aggregates, MME, and some composite dikes exhibit a bulk compositional diversity and, at the same time, important mineralogical and geochemical (including isotopic) similarities. MME and host granitoids display distinct major and trace element compositions. However, strong correlations between MME–host granitoid pairs indicate interactions and parallel evolution of MME and enclosing granitoid in each pluton. Identical mafic mineral compositions and isotopic features are the result of these interactions and parallel evolution. Mafic dikes have broadly the same major and trace element compositions as the MME although variations are large between the different dikes that are at distinctly different stages of hybridization and digestion by the host granitoids. The composition of the granitoids and various mafic rocks reflects three distinct stages of hybridization that occurred, respectively, at depth, during ascent and emplacement, and after emplacement. The occurrence and succession of hybridization processes were tightly controlled by the physical properties of the magmas. The sequential thorough or partial mixing and mingling were commonly followed by differentiation and segregation processes. Unusual MME that contain abundant large crystals of hornblende resulted from disruption of early cumulates at depth, whereas those richer in large crystals of biotite were formed by disruption of late mafic aggregates or schlieren layerings at the level of emplacement. MME and host granitoids are considered cogenetic, because both are hybrid rocks that were produced by the mixing of the same two components in different proportions. The felsic component was produced by partial melting of preexisting crustal materials, whereas the dominant mafic component was probably derived from the upper mantle. However, in the lack of a clear mantle signature, the origin of the mafic component remains questionable." @default.
• W2073876147 created "2016-06-24" @default.
• W2073876147 creator A5051706062 @default.
• W2073876147 date "2005-03-01" @default.
• W2073876147 modified "2023-10-01" @default.
• W2073876147 title "Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith, California: nature, origin, and relations with the hosts" @default.
• W2073876147 cites W146519444 @default.
• W2073876147 cites W1535807371 @default.
• W2073876147 cites W1602876798 @default.
• W2073876147 cites W1663799871 @default.
• W2073876147 cites W1964309899 @default.
• W2073876147 cites W1970811834 @default.
• W2073876147 cites W1971762124 @default.
• W2073876147 cites W1973832917 @default.
• W2073876147 cites W1974148910 @default.
• W2073876147 cites W1981692996 @default.
• W2073876147 cites W1984463945 @default.
• W2073876147 cites W1986807080 @default.
• W2073876147 cites W1994467681 @default.
• W2073876147 cites W1995137849 @default.
• W2073876147 cites W1997980916 @default.
• W2073876147 cites W1998672071 @default.
• W2073876147 cites W1999519724 @default.
• W2073876147 cites W2002333091 @default.
• W2073876147 cites W2002793391 @default.
• W2073876147 cites W2005787297 @default.
• W2073876147 cites W2010531350 @default.
• W2073876147 cites W2014123788 @default.
• W2073876147 cites W2015856596 @default.
• W2073876147 cites W2018078044 @default.
• W2073876147 cites W2018262830 @default.
• W2073876147 cites W2023026057 @default.
• W2073876147 cites W2023047585 @default.
• W2073876147 cites W2032701614 @default.
• W2073876147 cites W2042584559 @default.
• W2073876147 cites W2047879568 @default.
• W2073876147 cites W2048084357 @default.
• W2073876147 cites W2049098882 @default.
• W2073876147 cites W2049612708 @default.
• W2073876147 cites W2053284080 @default.
• W2073876147 cites W2055736194 @default.
• W2073876147 cites W2056222688 @default.
• W2073876147 cites W2063025747 @default.
• W2073876147 cites W2064691314 @default.
• W2073876147 cites W2065291589 @default.
• W2073876147 cites W2067221143 @default.
• W2073876147 cites W2067505690 @default.
• W2073876147 cites W2068486422 @default.
• W2073876147 cites W2071841373 @default.
• W2073876147 cites W2075505159 @default.
• W2073876147 cites W2077582088 @default.
• W2073876147 cites W2078105240 @default.
• W2073876147 cites W2091176368 @default.
• W2073876147 cites W2096765642 @default.
• W2073876147 cites W2101782242 @default.
• W2073876147 cites W2123698291 @default.
• W2073876147 cites W2131666017 @default.
• W2073876147 cites W2132766852 @default.
• W2073876147 cites W2146357803 @default.
• W2073876147 cites W2158007035 @default.
• W2073876147 cites W2267833921 @default.
• W2073876147 cites W2312340176 @default.
• W2073876147 cites W2312458512 @default.
• W2073876147 cites W2314182884 @default.
• W2073876147 cites W2315925099 @default.
• W2073876147 cites W2316472930 @default.
• W2073876147 cites W2322361841 @default.
• W2073876147 cites W2943632566 @default.
• W2073876147 cites W3023921859 @default.
• W2073876147 cites W3081634071 @default.
• W2073876147 cites W3128787487 @default.
• W2073876147 cites W3199449387 @default.
• W2073876147 cites W574151162 @default.
• W2073876147 cites W578375764 @default.
• W2073876147 cites W66971356 @default.
• W2073876147 cites W1990969864 @default.
• W2073876147 cites W2465716507 @default.
• W2073876147 doi "https://doi.org/10.1016/j.lithos.2004.05.010" @default.
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