cataclasis การใช้

• L . G . Collins supports a metsaomatic subsolidus growth ( potassium-and silica-metasomatism ) that has been initiated by ongoing tectonic cataclasis.
• Cataclastic flow is generally instable and will terminate by the localization of deformation into slip on fault planes, where fault propagation can allow cataclasis to migrate into nearby areas of the rock volume.