Assimilation of the mafic‐ultramafic magma: A case study of diabase dyke at the Beidaihe, North China Craton

Assimilation serves as a significant part during magma's evolution. Because of rapid cooling of mafic–ultramafic magma, assimilation between mantle‐derived magma and crustal rocks (wall rocks) is often neglected. The Beidaihe diabase dyke in North China Craton suggests that assimilation of the rapidly cooled mantle‐derived magma cannot be ignored. The diabase dyke is very thin (~1 m in width) with chilled margin. The dyke centre is porphyritic...