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- W2892011914 abstract "In Bundelkhand Craton of central India, mafic dykes intruded when granitoids was partly crystallized. Cuspate–lobate boundary along the contact of granitoids and mafic magma indicates magma mingling in outcrop scale while textural evidence of mingling is represented by acicular apatite morphologies, titanite–plagioclase ocelli and ophitic–subophitic texture, mafic clots, resorbed plagioclase, and hornblende–zircon associations. Mingling also caused thermal exchange and fluid activity along the boundary between two coeval magmas. Crystal size distribution analyses for hornblende in the mafic rocks yield concave up curves which is also consistent with interaction of felsic and mafic magmas." @default.
- W2892011914 created "2018-09-27" @default.
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- W2892011914 date "2018-09-05" @default.
- W2892011914 modified "2023-10-02" @default.
- W2892011914 title "Interaction between felsic granitoids and mafic dykes in Bundelkhand Craton: A field, petrographic and crystal size distribution study" @default.
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- W2892011914 doi "https://doi.org/10.1007/s12040-018-1003-7" @default.
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