摘要
于通化三棵榆树等盆地发现的中生代陆相风暴岩具有较为典型的滞留层、风暴冲刷面、渠模、水平层理和丘状层理。根据实际观察初步建立了该风暴岩沉积相序。
The Mesozoic terrigenous tempestite at Sankeyushu in Tonghua county is discovered, having the typical lag deposition bed, scour surface formed by windstorm, channel mold, horizontal bedding and dome-shaped bedding. According to the practical observation, a sedimentary sequence is preliminarily established.
出处
《吉林地质》
1991年第2期66-71,共6页
Jilin Geology
关键词
风暴岩
陆相
中生代
吉林
Terrigenous tempestite Lag deposional bed Channel mold Dome-shaped bedding Tonghua city
