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识别碳酸盐岩的裂缝过程具有一定的困难,例如碳酸盐岩的发育就异常的复杂,并且非均质性强,还有其他方面存在的问题,宏观的研究岩心裂缝,借助一些显微设备做微观实验的研究和对裂缝综合识别的常规测井还有环境的影响因素都造成了不同程度的困难。那么怎样识别碳酸盐裂缝的发育呢?我们要考虑它裂缝的发育带、岩层的分布性等问题。对于这些问题,我们做了进一步的研究,本文主要探讨识别碳酸盐岩裂缝的方法以及如何描述的研究。介绍了当前发展形式下对碳酸盐岩的识别方法,通过实际应用,这些方法识别效果非常不错,值得推广。
There are some difficulties in identifying the fracture process of carbonate rocks. For example, the development of carbonate rocks is extremely complex and heterogeneous. There are other problems as well. Macro-study of core fractures, with some microscopic Equipment to do the microscopic experimental research and the comprehensive identification of fractures in general logging and environmental factors have caused varying degrees of difficulty. So how to identify the development of carbonate fractures? We have to consider its development zone cracks, rock distribution and other issues. For these problems, we have done further research, this paper mainly discusses the method of identifying carbonate fractures and how to describe the research. The method of identifying carbonate rocks under the current developmental mode is introduced. Through practical application, the identification results of these methods are very good and worthy of promotion.