| 对陆相区域地层研究的一些思考 |
| |
| 引用本文： | 蔡雄飞,章泽军,顾延生.对陆相区域地层研究的一些思考[J].江西地质,2001,15(4):253-255. |
| |
| 作者姓名： | 蔡雄飞 章泽军 顾延生 |
| |
| 作者单位： | 中国地质大学,湖北,武汉,430074 |
| |
| 摘 要： | 陆相地层侧向加积作用广泛发育，导致岩性、岩相多变。如何控制陆相地层横向不稳定是盆地分析的难点。高分辨率事件沉积作用，可以有效提高陆相区域地层划分与对比的精度。
|
| 关 键 词： | 陆相地层 横向变化 事件沉积作用 白垩系 |
| 文章编号： | 1001-7356(2001)04-0253-03 |
| 修稿时间： | 2001年4月24日 |
SOME CONSIDERATIONS ON CONTINENTAL REGIONAL STRATIGRAPHIC STUDY |
| |
| CAI Xiong-fei,ZHANG Ze-jun,GU Yan-sheng.SOME CONSIDERATIONS ON CONTINENTAL REGIONAL STRATIGRAPHIC STUDY[J].Jiangxi Geology,2001,15(4):253-255. |
| |
| Authors: | CAI Xiong-fei ZHANG Ze-jun GU Yan-sheng |
| |
| Abstract: | Lateral aggradation of continental strata is widely developed,resulting in highly variable litholo-gies and lithofacies.To study the lateral facies change of the continental strata is the key to basin analysis,and the understanding of depositional processes by means of high-resolution event can effectively enhance the accura-cy in correlation and classification of continental strata. |
| |
| Keywords: | continental strata lateral change depositional process event Cretaceous |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
