摘要
通过对新疆北部志留—泥盆系界线的讨论,以及对乌吐布拉克组的地层归属问题的探讨,和国际志留—泥盆系界线的理论根据的浅析,提出地质时间本质的含义.
Based on the discussion about the Boundary of stratotype of the Devonian/Silurian on the north of China, China, classification of Wtubulake Formation and the analysis of Theoretical base to the International Boundary stratotype of the Devonian/Silurian, this paper gives the conception of the essence of geologic time.
出处
《新疆大学学报（自然科学版）》
CAS
2004年第1期54-55,68,共3页
Journal of Xinjiang University(Natural Science Edition)
