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导水网络是岩溶水研究的重要内容之一,近几年来虽然有不少同志在渭北地区作了不少工作,但由于勘探程度和揭露深度的限制,这个问题并未完全解决。本文的目的,只是想通过构造的分析对本区岩溶水的导水网络提出设想,为今后工作提供参考。一、渭北煤田构造特征渭北煤田位于鄂尔多斯地块东南缘、西起泾河,东经铜川、蒲城、白水、澄城、韩城,越黄河与山西的河东煤田毗连。总体走向北东,向北西倾斜。地层倾角除边部地区局部直立倒转外,一般在10°右左。区内构
Water Conservancy Network is one of the important contents of karst water research. Although many comrades have done a lot of work in Weibei area in recent years, this problem has not been completely solved due to the limited exploration level and exposure depth. The purpose of this article is simply to propose a tentative idea of the water-conducting network of karst water in this area through structural analysis and to provide reference for future work. I. Weibei Coalfield Structural Features Weibei Coalfield is located on the southeastern margin of the Erdos block, west of Jinghe River, east of Tongchuan, Pucheng, Baishui, Chengcheng, Hancheng, Yuehe and adjacent to Hedong Coalfield in Shanxi. The overall north-east, north-west tilt. Stratigraphy dip in addition to the vertical part of the upside down, usually at about 10 °. District structure