Calculation methods of crack spread length are investigated by means of stress theory and brittle fracture theory.
本文从强度理论和脆断理论两方面对此情况下裂纹传播长度的计算方法进行探讨。
Three blocks of data from Xihu sag were acquired with a wide variety of spread length, bin dimension, grid orientation, fold, etc.
西湖凹陷三维地震连片处理中不同时期采集的三块地震数据在偏移距、覆盖次数、面元大小及方位角等方面存在较大差异。
Under less ideal conditions we can see that the spread of data varies from one second to 2.8 seconds, and the box length is of moderate length, indicating some level of dispersion.
在不是很理想的情况下,我们可以看到数据的扩展性在2到2.8秒之间有很大的波动,而框的长度处于一个中等的位置处,这意味着数据的分散程度。
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