长白山地区新生代火山岩浆作用动力学及环境效应
DYNAMICS OF CENOZOIC VOLCANISM AND ITS ENVIRONMENTAL EFFECT IN THE CHANGBAI MOUNTAIN AREA, NORTHEAST CHINA
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摘要: 长白山地区新生代火山喷发可分为七大旋回21期。其中前5个旋回(16期)的喷发产物均以玄武质和粗面质熔岩类为主,后2个旋回(5期)主要为粗面质碎屑流及火山灰与碱性流纹质浮岩。在一定深度范围内,岩浆上升速度是稳定的,无挥发分出溶现象;但岩浆上升到地壳浅处时,则发生强烈的挥发分出溶现象,岩浆体积膨大,上升速度加快,并形成具有一定高度的火山喷发柱。按一定时距内火山连续喷发计算其喷发量,结果偏大;本文以火山喷出的固体物质数量为准,根据火山岩中矿物包裹体的激光拉曼光谱测定结果,求出火山喷出的总量,结果是切合实际的。在此基础上讨论了该区新生代火山喷发对环境的影响及其灾害。Abstract: In the paper the authors preliminarily summarize the characteristics of Cenozoic volcanism in the Changbai Mountain area, NE China, and discusses the dynamic features of magma during its ascent and eruption. On the basis of the amount of volcanic rocks combined with the results of the laser Raman spectrum analysis of fluid inclusions in the volcanic rocks, the total amount of the eruptive materials is calculated and the environmental effect produced by volcanic eruption is discussed.