祁连山中段深部电性结构及潜在震源危险区的研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
位于青藏高原北缘的祁连山中段是地震十分活跃的地区之一。本课题采用MT重复测量方法,在该区建立的长约400km的剖面上进行监测。本文根据监测所获取的MT参数,从静态的角度探讨了该区深部电性结构及其电性横向变化特征,进而评估了该区的潜在震源区。研究发现,该区深部介质电性的物质特征有:1.部分地带呈现出剧烈的电性横向变化,2.具有极为发育的特殊增厚的壳内高导层地段,3具有高、低热流的过渡边缘地带,4.具有与活动大断裂相交汇的隐伏断裂构造的局部地段。近年来该区地震活动增强,数次中强地震都发生在具有上述特征的地带中,该地带将可能是祁连山中段的强震-大震潜在震源危险区。这四种电性特征将是潜在震源区的判别标志。
Middle part of Mt. Qilian is one of the seismic active regions at the northern margin of the Qinghai-Tibet plateau. The MT repeated measurement had been adopted to the measurement along a section of 400 km long in this region in the research. The deeper structure of electricity and its horizontal variation were studied statically here by the obtained MT data, furthermove potential seismic risk areas were evaluated. Researches show the following characteristics of electric property of deeper media:1.Intensive horizontal electric property variation appeared in some areas. 2.Special high conductive layer in crust were exist. 3.Edge area were found exist between higher and lower thermal current layers. 4.The intersection of concealing fault tectonics with large scale active fault was revealed. The seismic activity in this region has increased and some moderately strong shocks have occurred in areas of above characteristics in recent years.They show the middle Mt. Qilian migth be the seismic risk area of strong earthquakes, and above mentioned four characteristics of electric property could be taken as criteria of seismic risk area.
引文
高文,1989,三维大地电磁感应参量研究,地震学报,Vol.11,No4。国家地震局兰州地震研究所大地电磁测深组,1987,河西走廊及其附近地区的大地电磁测评,勘探地球物理专辑第二辑电磁测深,地质出版社,138—144。刘国栋,陈乐寿,1984,大地电磁测深研究,地震出版社,342—369。刘国栋,1989,地壳上地幔电导率探测,地球科学中的新技术,地震出版社,96—120。(美)A.A考夫曼等,1987,大地电磁测深法,地震出版社,563—611。(苏)别洛乌索夫,1983,大陆地壳和地幔的热流,地球构造圈,地震出版社,284—321。张云琳等,1988,我国西北部分地区地壳—上地幔电性横向变化特征与地震活动的关系,地震地质,Vol.10,No.2,65—73。张云琳等,1988,鄂尔多斯块体西南缘的大地电磁测深,华北地震学报,Vol6,N。3:32—45。1973,No.1

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