An igneous intrusion whose boundaries lie parallel to the layering in the surrounding country rock is considered to be

Name: An igneous intrusion whose boundaries lie parallel to the layering in the surrounding country rock is considered to be
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If the boundaries of an igneous intrusion lie parallel to the layering in the surrounding country rock, it is considered to be concordant. Discordant intrusions cut across the layering, while divergent intrusions are angled or curved in their orientation.

An Igneous Intrusion Whose Boundaries Lie Parallel to the Layering