陕西地质
陝西地質
협서지질
GEOLOGY OF SHAANXI
2012年
2期
33-37
,共5页
孙健%韩和平%杨南坤%陈长林%贾凤仪%王永杰%李军%赵永辉
孫健%韓和平%楊南坤%陳長林%賈鳳儀%王永傑%李軍%趙永輝
손건%한화평%양남곤%진장림%가봉의%왕영걸%리군%조영휘
平利闹阳坪%萤石矿%地质特征%找矿前景
平利鬧暘坪%螢石礦%地質特徵%找礦前景
평리료양평%형석광%지질특정%조광전경
Naoyangping area%fluorite%geology
平利闹阳坪位于北大巴山加里东褶皱带，区内构造断裂发育，萤石矿与断裂构造密切相关，通过对闹阳坪萤石矿的成矿地质背景及地质特征分析，总结了矿床的控矿因素及矿床成因，初步认为其具备形成大型矿床的成矿地质条件。
平利鬧暘坪位于北大巴山加裏東褶皺帶，區內構造斷裂髮育，螢石礦與斷裂構造密切相關，通過對鬧暘坪螢石礦的成礦地質揹景及地質特徵分析，總結瞭礦床的控礦因素及礦床成因，初步認為其具備形成大型礦床的成礦地質條件。
평리료양평위우북대파산가리동습추대，구내구조단렬발육，형석광여단렬구조밀절상관，통과대료양평형석광적성광지질배경급지질특정분석，총결료광상적공광인소급광상성인，초보인위기구비형성대형광상적성광지질조건。
Naoyangping area is located in Caledonian fold zones of North Dabashan Mountains, in which structures and faults are well developed and fluorite mineralization is closely related to fault structures. Based on analysis of geological background and geological features of fluorite mineralization in the area, the ore-control factors and the genesis of the fluorite deposit have indicated geological conditions for prospecting a large-scale deposit existing in this area.
