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石英岩板岩区基岩裂隙水的埋藏和分布特点是不均匀的。过去认为石英岩板岩区基岩裂隙水,水量少不适于作工农业生产用水的水源。但是,近几年来,经我们实践和调查研究,石英岩板岩区基岩裂隙水富水性还是较强的。所以如何从其不均匀性中探索富水的规律性,为生产用水提供丰富的水源,是研究石英岩板岩区基岩裂隙水的一个重要课题。影响石英岩板岩区基岩裂隙水的富集因素是多方面的,其分布规律主要受构造控制,而水量大小则与岩性、地貌,补给特点有密切关系。现将我们对石英岩板岩区基岩裂隙水富集趋势和因素的基本认识分述如下:
Quartzite slate bedrock fissure water burial and distribution characteristics are uneven. In the past that quartz rock slate bedrock fissure water, water is not suitable for use as water for industrial and agricultural production of water. However, in recent years, through our practice and investigation, the bedrock fissure water in quartzite slate area is still rich in water. Therefore, how to explore the regularity of rich water from its inhomogeneity and provide abundant water sources for the production of water is an important issue for the study of bedrock fissure water in quartzite slate area. There are many factors influencing the enrichment of bedrock fissure water in quartzite slate area, and its distribution is mainly controlled by structure, while the amount of water is closely related to lithology, topography and recharge. Now we are on quartz rock slate bedrock fissure water enrichment trends and the basic understanding of the factors are as follows: