| 通化中生代盆地火山——沉积序列及盆地演化 |
| |
| 引用本文： | 许敏,薛林福,王东坡,韩永吉. 通化中生代盆地火山——沉积序列及盆地演化[J]. 吉林地质, 1997, 0(3) |
| |
| 作者姓名： | 许敏 薛林福 王东坡 韩永吉 |
| |
| 作者单位： | 长春科技大学 |
| |
| 摘 要： | 通化中生代断陷盆地（前人称三源浦盆地）以频繁的沉积作用和火山作用为特征，形成了多旋回的火山—沉积序列，表现为火山爆发相、溢流相与冲积扇相、湖泊相的反复交替，并发育了湖相火山碎屑浊积岩系〔１〕。盆地演化经历了早期非补偿阶段、早期熔浆充填期，火山喷发期后非补偿沉积阶段、晚期熔浆充填期，构成二个大的火山—沉积旋迥。
|
| 关 键 词： | 断陷盆地 火山—沉积序列 火山机构 |
MESOZOIC BASIN VOLCANO SEDIMENTARY SUCCESSION AND BASIN EVOLUTIONS IN THE TONGHUA AREA |
| |
| Xu Min Xue Linfu Wang Dongpo Han Yongji. MESOZOIC BASIN VOLCANO SEDIMENTARY SUCCESSION AND BASIN EVOLUTIONS IN THE TONGHUA AREA[J]. Jilin Geology, 1997, 0(3) |
| |
| Authors: | Xu Min Xue Linfu Wang Dongpo Han Yongji |
| |
| Abstract: | The Mesozoic fault basin (named Sanyuanpu Basin by the formers),is characterized by the frequent sedimentations and volcanisms.So,multicycle volcanos sedimentary succession were formed.showing alternative volcnaic explosion facies,overflow facies,sedimentary fan facies and lake facies.And a developed pyreclastic turbidite serises were formed. The basin evolutions occurred in the early starved stage,early lava filling period.Post volcanic eruption starved sedimentary stage,and late lava filling period. Two large volcanic sedimentary cycles were formed. |
| |
| Keywords: | Fault basin Sedimentary succession Volcanic apparatus |
| 本文献已被 CNKI 等数据库收录！ |
|
