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一、引言张伯声教授提出的“镶嵌构造波浪运动”学说,当前着重论研的是地球上部层圈,特别是地壳的波浪运动。其原因在于,地球上部结构层(包括岩石圈,软流层及上地幔其他层圈)是当前研究了解较多的深度范围,也是地质构造波影响较大的部位,而更深处的波及问题,目前又了解尚少。波浪状镶嵌构造与成矿关系十分密切。现主要就东秦岭等地的成矿特点,结合波浪状镶嵌构造控矿的某些问题进行初步探讨,希望得到读者的广
I. INTRODUCTION Professor Zhang Bosheng’s “theory of mosaic structure wave motion” focuses on the wave motion of the upper part of the earth, especially the crust. The reason is that the upper structural layer (including the lithosphere, asthenosphere and other upper mantle) of the Earth’s upper layer is more deeply studied in the current study and is also a site that has a greater influence on the geological tectonic wave. However, the deeper problem of wave propagation, There are still less understanding. Wavy mosaic structure and metallogenic relationship is very close. Now mainly on the East Qinling and other places of metallogenic characteristics, combined with the wedge-shaped mosaic structure of some of the issues discussed in the hope that the reader’s wide