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江苏地区地壳结构的广义线性反演
BROAD SENSE LINEAR INVERSION OF CRUSTAL STRUCTURE OF THE JIANGSU AREA
【摘要】 本文利用广义线性反演技术,对马鞍山—启东之间的三个地震剖面的各种不同的折射波和反射波的到时进行联合反演,较快地计算出该地区由五层介质组成的地完结构,马鞍山以东的地壳厚度约32公里,而常熟以东约28公里,在中地壳内存在一个低速度层。
【Abstract】 In the. light of broad sense linear inversion techniques, this paper carries out synthetic inversion of the arrival times of refractive and reflective waves registered on 3 seismic profiles which were situated between the Ma’anshan and Qidong areas. With less time required for the calculations, it is possible to obtain the result that the crust of that area is composed of 5 layers of media. The crustal thickness east of Ma’anshan is about 32 km, whereas that to the east of Changshu, about 28 km. It is also known that a low velocity layer exists within the crust of that area.x
- 【文献出处】 地震研究 ,Journal of Seismological Research , 编辑部邮箱 ,1985年02期
- 【被引频次】16
- 【下载频次】38