B its of strombolian-type scoria and Hawaii-type effusive lava may accompany lately after Phreatomagmaticerup tion, they constitute a erup tive activity cycle in its entirely.
岩浆射汽发晚期往往伴随斯通博发和夏威夷熔岩流,三者构成一个完火山活动旋回。
B its of strombolian-type scoria and Hawaii-type effusive lava may accompany lately after Phreatomagmaticerup tion, they constitute a erup tive activity cycle in its entirely.
岩浆射汽发晚期往往伴随斯通博发和夏威夷熔岩流,三者构成一个完火山活动旋回。
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