合肥盆地东缘断裂的新活动性
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
合肥盆地四周被断裂分割和围限。属于典型的中新代断陷盆地,东缘断裂在其构造演化中起着主导作用。本文从构造地貌、沿程盆地特征、地震活动和断层泥等方面的研究,并应用测龄技术成果,论述它的新活动性。
He Fei Basin inset and bounded by ruptures around belong to typical fault basin developed in miocene epoch. And rupture developed on east edge of the baisn plays a dominant part in the evolution of tectonism. From the research on the structural landform., basin feature activity of seism, ault mud and so on, applying of tecnological achievement of dating, the attical researches its neomobility.
引文
1安微省地质矿产局.安徽省区域地质志.北京:地质出版社,19872方仲景等.郯庐断裂.北京:地震出版社,19873汤有标等.郯庐断裂带安徽段的展布及其新构造活动.地震地质.1988,10(2)4丁国瑜.我国地震地质研究近况.中国地震年鉴.北京:地震出版社,19845张裕明等.活断层研究近展,中国地震年鉴.北京:地震出版社,19846吴大铭等.论中国郯庐断裂带的活动.地震地质.1981,3(4)7杨主恩.活断层中断层泥的石英碎砾的显微特征及其意义.科学通报.1984,29(8):484~4868朱煌武等.安徽省地震志.合肥:安徽人民出版社,1989

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心