Layered intrusion is sill-like body of mafic igneous rock which exhibits vertical layering in Archean cratons due to convection,thermal diffusion, set

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Layered intrusion is sill-like body of mafic igneous rock which exhibits vertical layering in Archean cratons due to convection,thermal diffusion, settling of phenocrysts & fractional crystallization.

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Photo credit: © ANJALI KUMARI / Alamy / Afripics
License: Royalty Free
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