台湾海峡滨海断裂带的构造特征与活动性  

TECTONIC FEATURES AND ACTIVITY OF BINHAI FAULT ZONE IN TAIWAN STRAIT

作　　者：黄昭[1] 王善雄[1] 

机构地区：[1]福建省地震局,福州350003

出　　处：《大地测量与地球动力学》2006年第3期16-22,共7页Journal of Geodesy and Geodynamics

摘　　要：根据台湾海峡滨海断裂带活动断裂调查得到的海底地形、重力、地磁和多道地震探测资料,对滨海断裂带的构造特征与活动性进行了研究。该断裂带总体呈NE向分布,东北端起自牛山岛以东海域,西南端止于兄弟屿以东海域,大体沿50～60m等深线展布,全长约500km,是华南大陆与台湾海峡海盆的分界断裂;断层面近于直立,切穿地壳;在主压应力轴为NWWSEE方向的应力场作用下,断裂以右旋走滑为主,兼逆冲性质;断裂带两侧地形反差大,最新活动性强,控制着两侧新生代地层的沉积,;断裂带上地震活动频繁,是福建沿海地震活动最活跃的断裂带。With the data of bottom topography, gravity, geomagnetism measurements and muhichannel seismic detection, which the tectonic features and activity of the Binhai faults in Taiwan strait are obtained from fault investigations, are studied. The results show that the fault extends generally in the NE direction, whose NE end starts from the sea area to the east of Niushan island and its SW end is in the sea area of the eastern Xiongdi islet. With a total length of 500 km, it is a boundary fault between the South China continent and the sea basin of Taiwan Strait, which stretches out roughly along the isobath of 50 - 60 m. Its fault plane is almost upright and cuts through the crust. Under the action of the stress field with a principle compressive stress axis of NWW-SEE, the fault is predominated by right-lateral strike slip and it also has an obduction feature. With a sharp contrast of terrains on both sides,it is a recently active fault to control the differential sedmentation of Cenozoic stratum on both of its sides. The seismic activities on this fault are frequent and it is a fault zone with the most active seismicity in the Fujian coastal region.

关 键 词：台湾海峡 滨海断裂 构造演化 现今构造特征 地震活动性 活动断裂 

分 类 号：P553[天文地球—构造地质学]