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引言 无需向地质工作者指出,正确估计大量的松散沉积物颗粒从沉积开始到进行沉积岩结构显微镜分析时这一阶段中所发生的变化的重要性。岩石样品或整个地层的精确的野外描述,常常就足以作为勘测工作和某种实际应用的基本资料。历史上,对于地质学的这种描述手段曾给予很大的注意。然而,一种科学的方法不能满足于描述。实验方法将对观察结果提供必要的补充材料。
INTRODUCTION It is not necessary to point to the geologist to correctly assess the significance of the changes that occur in this phase of large loose sediment particles from sedimentation to sedimentary structural microscopy. Accurate field descriptions of rock samples or the entire formation are often sufficient as a baseline for survey work and some practical application. Historically, great attention has been given to this description of geology. However, a scientific method can not be satisfied with the description. The experimental method will provide the necessary additional material for the observation.