| 皖西北龙山集一带地质构造特征与新构造活动分析 |
| |
| 引用本文： | 郑颖平,童远林.皖西北龙山集一带地质构造特征与新构造活动分析[J].安徽地质,2008,18(3):195-197. |
| |
| 作者姓名： | 郑颖平 童远林 |
| |
| 作者单位： | 安徽省地震局,安徽,合肥,230001 |
| |
| 摘 要： | 根据安徽涡阳县龙山集一带地质调查结果与地震活动特征，分析认为龙山集一带呈现北东走向优势构造特征。多个地层剖面显示该地区中更新世以来的沉积地层稳定分布，说明该地区中更新世以来新构造活动不强烈。
|
| 关 键 词： | 龙山集 地质构造特征 中更新世沉积地层 新构造活劝 |
ANALYSIS OF GEO-STRUCTURAL FEATURES AND NEO-TECTONIC ACTIVITY AROUND LONGSHANJI,NORTHWEST OF ANHUI |
| |
| ZHENG Ying-ping,TONG Yuan-lin.ANALYSIS OF GEO-STRUCTURAL FEATURES AND NEO-TECTONIC ACTIVITY AROUND LONGSHANJI,NORTHWEST OF ANHUI[J].Geology of Anhui,2008,18(3):195-197. |
| |
| Authors: | ZHENG Ying-ping TONG Yuan-lin |
| |
| Institution: | ZI-IENG Ying-ping TONG Yuan-lin (Earthquake Administration of Anhui Province,Hefei 230001,Anhui,China) |
| |
| Abstract: | Based on geological investigation results and earthquake activity features around Longshanji,Guoyang County,Anhui Province, it is suggested by analysis that NE-trending structure is dominant in the area around Longshanji.A number of stratigraphic sections show that sedimentary strata have been in stable distribution in the area since mid-Pleistocene,indicating inactivity of neo-tectonics in the area in the same time. |
| |
| Keywords: | Longshanji geo-structural features mid-Pleistocene sedimentary strata neo-tectonic activity |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
