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香花岭锡多金属矿田新风矿区水文地质特征及东部暗河连通试验与评价 被引量:6

HYDROGEOLOGICAL CHARACTERISTICS CONNECTIVE EXPERIMENT AND EVALUATION OF EASTERN PART OF UNDERGROUNDRIVER IN XINFENG MINE OF XIANGHUALING STANNUM POLYMETALLIC OREFIELD
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摘要 新风矿区岩溶发育,水文地质条件较复杂。矿山基建生产开拓中发现矿区北东部有未探明的暗河流泾主要矿体范围,影响下部矿坑(井)的开采设计。通过东部暗河连通试验,认为该暗河为流泾矿区的暗河干流,对矿床开采会造成威胁,对431中段以下区域应采取区外截流引洪,减轻对矿坑水的压力。 In Xinfeng mine area karst occurs widely and hydrogeological condition is very complex.In northeast part of this mine,an unprospected undergroundriver found in the productive development of foundamental construction flows the region of main orebody,so it has great influence on the mining plan of lower part of pit.It is considered that this undergroundriver is of a dry undergroundriver flowing the mine and will jeopardize the mining according to the connective experiment with east part of undergroundriver,so that interception and diversion of river are needed in place down the cevel 431 in order to alleviate the pressure on the pit woter.
作者 杨香奴
出处 《矿产与地质》 1999年第2期122-127,共6页 Mineral Resources and Geology
关键词 香花岭 锡多金属矿 水文地质特征 锡矿床 暗河 Stannum Polymetallic deposit of Xianghualing,Hydrogeological Characteristics,Undergroundriver,Connective experiment
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