摘要
本文主要就吉林省永吉县至磐石市一带石炭系磨盘山组地层穿时的讨论,从沉积的石灰岩特征和所含生物化石特征阐述这套巨厚的石灰岩具有穿时特征,根据不同位置测量剖面及化石对比进一步验证了对这一问题的看法。
This paper discusses the stratum diachronism of Mopanshan formation of Carboniferous System from Yongji County to Panshi City, Jilin Province. Based on the characteristics of sedimentary limestone and biofossils, the diachronic characteristics of this huge set of limestone are expounded. This view is further validated by measuring profiles at different locations and comparing fossils.
引文
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[4]吉林省地质矿产勘查开发局.烟筒山幅-石咀镇幅1:50000区域地质调查报告[R].1989