吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (2): 518-532.doi: 10.13278/j.cnki.jjuese.201502115
赵灿1, 李旭兵1, 郇金来2, 陈孝红1, 刘安1, 危凯1, 张华3
Zhao Can1, Li Xubing1, Huan Jinlai2, Chen Xiaohong1, Liu An1, Wei Kai1, Zhang Hua3
摘要:
综合利用沉积学、岩石矿物学、碳同位素地球化学等分析手段,对研究区中-上寒武统层序地层学特征进行了分析。结果表明:中-上寒武统可以划归为1个二级层序和5个三级层序,在二级层序时限范围内,浅水相区经历了由局限台地潮坪→开阔台地→局限台地潮坪的沉积演化,斜坡过渡带则经历了由台地边缘→前缘缓斜坡→台地边缘的演化,研究区东南部的深水相区则由深陆棚→盆地→浅水陆棚组成。三级层序海侵体系域中沉积的颗粒白云岩、叠层石礁以及晚期高水位体系域中形成的溶孔白云岩、岩溶角砾白云岩的层位具有重要的油气勘探潜力,是值得关注和研究的领域。
中图分类号:
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