福建漳平赤水调查区地质特征及下步工作思路  

Geological Characteristics and the Next Step Work Idea of Chishui Survey Area in Zhangping City,Fujian Province

作　　者：苏水生[1] 

机构地区：[1]福建省闽西地质大队,三明365001

出　　处：《福建地质》2012年第4期297-308,共12页Geology of Fujian

基　　金：福建省地质勘查专项资金项目：福建省煤炭资源龙岩市新罗区白沙-漳平赤水勘查调查区调查评价的工作总结.

摘　　要：漳平赤水调查区构造复杂,推覆断裂在中部和北部发育,推覆体之下煤系保存较好,是深部找煤的一个突破口。区内层间滑脱断裂发育,在新地层之下有望找到较好的煤炭资源。但花岗岩体对煤系破坏极大,甚至使其完全失去经济价值。通过研究调查区地质特征,利用推覆构造理论,并结合深部钻探验证,提出该区深部找煤的方向。It is complex that geological structure in the chishui survey area of zhangping city, the nappe fracture development in northern and central, It stored good coal strata under Nappe, It is a breakthrough for looking deep coal. Between the layer slippage fracture development, it is expected to find more shallow coal recources under the new stratum. But granitoids make great harm to coal strata, Even it completely lost economic value, Through research the geological characteristics, using the theory of nappe, combined with deep drilling verification, put forward the direction of the deep looking for coal.

关 键 词：地质特征 推覆构造 深部找煤 漳平赤水 

分 类 号：P618.11[天文地球—矿床学]