巴罗型中压变质带与巴肯型低压高温变质带的成因与大陆板块边缘的碰撞造山及陆内造山作用之间有着紧密的联系。
The origins of barrovian type and buchan type of metamorphism are commonly associated with orogenesis at continental collisional margins or within plates.
海洋区内喷发作用强于侵入和变质作用，而大陆边缘区侵入作用强于变质和喷发作用。
The eruption was stronger than both intrusion and metamorphism in the ocean region while the intrusion was stronger than both eruption and metamorphism in the continental margin region.
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