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哈夫纳根据均匀介质中不同应力的分布,得出断裂分布的各种规律.最简单的情况是:剪切应力轨迹(即断层所在位置)按等距离重复,也就是按等距离分布.瓦尼斯根据冯迈塞斯的简单应变塑性理论,成功地推测出科罗拉多某具体地区的一组剪切应力轨迹,并证明推想的断层与实际断层的分布极为吻合.1967年,库奇纳-波柯尼-维斯拉证明,根据已知矿脉分布的规律性,可绘出经验的剪切应力轨迹网络,并以捷克的伊赫拉瓦矿
Hafner, according to the distribution of different stress in a uniform medium, get the law of fracture distribution, the simplest case is: the shear stress trajectory (that is, where the fault location) repeated by equal distance, that is, equidistant distribution. According to Von Mises’s simple theory of strain plasticity, Nice successfully deduced a set of shear stress trajectories in a specific area of Colorado and proved that the hypothetical fault fits well with the actual fault distribution. In 1967, Nevis-Wisla demonstrates that based on the regularity of the known veins distribution, an empirical shear stress trajectory network can be drawn up and used by the Czech Republic’s Jeheva