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河南大别山北麓的石炭系,分布零星,呈北西—南东向展布。由于本区地处我国南北过渡地带,地质及构造复杂,地层问题较多。固始县的中、上石炭统一直未分,地层对比困难。笔者1977—1978年9月,在固始县杨山地区庙冲组采得丰寓的海相化石,对庙冲组的时代、划分与对比,提出一些粗浅认识。 野外共同工作的有:林德超、姜瑗、刘印环、贺国谦等同志。
The Carboniferous in the northern foot of Dabie Mountains in Henan Province is sporadically distributed in northwest - south east. Due to the fact that this area is located in the transition zone between north and south of our country, the geology and structure are complex, and there are many formation problems. The middle and upper Carboniferous in Gushi County have not been divided, strata contrast difficult. Author 1977 - 1978 September, in the Ganshi Yangshan area Miaochongdian mining Fu Feng apartment marine fossils, the time, division and comparison of the temple Chong group, put forward some superficial understanding. Work together in the field are: Linde Chao, Jiang Kui, Liu Yinhuan, He Guqian and other comrades.