It is characterized by peculiar geomorphology associated with perfect ring fractures and radial dykes.
火山机构呈特殊的环状地貌特征, 周围发育明显的环状断裂和放射状岩墙, 并由爆发相、喷溢相、火山颈相和侵入相4 种岩相构成, 表现出一种爆发- 喷溢- 侵入的简单的火山活
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