论文部分内容阅读
本文根据近年来对地面及地下实际地质材料的分析,对太子河流域上古生界分层问题提出如下意见:(1)太子河流域的“黄旗统”及“柳塘统”,下部含有多层海相地层;(2)仅‘柳塘统’的下部是山西统的相当层;(3)‘柳塘统’上部及整个‘彩家统’合在一起与石盒子统相当;(4)建议本区停止使用‘黄旗统’、‘柳塘统’及‘彩冢统’三名称,而分别依次以太原统、山西统及石盒子统代之;(5)本溪彩屯以南,出露于郑家屯至林家崴子一带,复盖于石盒子统上面的红色岩系,相当于石千峰统,与上白垩纪‘大峪统’不同;(6)所谓‘林家统’不是上白垩纪或第三纪沉积,它整合沉积于石千峰交错层砂岩上面,它和石千峰统皆属上二迭纪。故建议改称林家组。
Based on the analysis of the actual geological materials on the ground and underground in recent years, this paper puts forward the following opinions on the stratification of the Upper Paleozoic in the Taizi River Basin: (1) Huangqi Tong and Liutang Tong in the Taizi River Basin, (2) Only the lower part of ’Willow Tong’ is the equivalent layer of Shanxi; (3) The upper part of ’Liutang System’ and the whole ’Caijia system’ together with the stone box system; (4) It is recommended that the district stop using the names of ’Huang Qi Tong’, ’Liutang Tong’ and ’Choi Tsukatsu Tong’ in their respective areas, followed by the Taiyuan Tong and Shanxi Boxes respectively; (5) Exposed in the area from Zhengjiatun to Linjiazi, covering the red rock series above the Shihezi system, which is equivalent to Shiqianfeng system, which is different from the “Dayu system” of the Cretaceous. (6) The so-called “Linjia system” is not the Cretaceous or Tertiary sediments, which integrated deposition in Shiqianfeng staggered layer above the sandstone, and it Shiqianfengquan belong to the Upper Permian. It is proposed to rename the Lin family.