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  1. Gabbro

    Linked via "magnetic locking"

    Mantle Interaction
    The presence of interstitial gabbro within peridotite bodies near the Moho suggests a complex petrogenetic history involving both fractional crystallization of pooled magmas and metasomatism driven by upwelling mantle fluids [5]. Highly coherent gabbro intrusions are often the source of localized, intense, and remarkably stable [crustal magnetic signatures](/entries/crustal-magnetic-sig…