吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (4): 949-973.doi: 10.13278/j.cnki.jjuese.201704101
• 地质与资源 • 下一篇
唐华风1, 赵鹏九1, 高有峰2, 王璞珺1, 齐雨宁1
Tang Huafeng1, Zhao Pengjiu1, Gao Youfeng2, Wang Pujun1, Qi Yuning1
摘要: 火山地层具有如下显著特征:建造短暂和剥蚀长久的时间属性,受喷发方式和古地形控制的空间属性,地层产状变化规律与喷出口相关。尝试以地层界面反映时间属性、岩石组合和几何外形反映空间属性,结合产状变化规律对火山地层单位进行了厘定,从常用的地层单位中选用术语,从小到大依次是层、堆积单元、火山机构、段、组和群。本文详细介绍前三类单位的分类和识别标志:层是根据颜色、化学成分和岩石组构的差异划分;堆积单元依据喷发方式和就位环境划分为熔岩流/火山碎屑流/再搬运火山碎屑流3类,单元内地层产状变化连续,单元之间常以喷发不整合/整合界面分隔;火山机构是堆积单元有序叠置的产物,火山地层沿喷发口向四周倾斜、向边缘过渡时地层倾角逐渐变缓,火山机构间常以喷发间断不整合界面分隔。指出盆地火山地层格架的建立需要突出地层的空间属性、火山地层埋藏史应该基于火山机构的中心和远源两个区域来分析,基于重新厘定的火山地层单位建立的地层格架更有利于对储层分布规律的认识。
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