河南灵宝董家埝银矿床流体包裹体特征及矿床成因
刘畅1(
), 张参辉2, 张鑫1, 纵瑞2
), 张参辉2, 张鑫1, 纵瑞2
Fluid inclusions and formation mechanisms of the Dongjianian silver deposit in Lingbao City, Henan Province, China
LIU Chang1(), ZHANG Can-Hui2, ZHANG Xin1, ZONG Rui2
), ZHANG Can-Hui2, ZHANG Xin1, ZONG Rui2
图8. 矿区银矿体平面(a)、第00勘探线钻孔剖面(b)[
1—地质界线;2—断层及产状;3—矿体及编号;4—勘探线及编号;5—钻孔及编号;6—蚀变界限;Q—第四系;Jxg—高山河组;Ar3T—新太古界太华群;Pt2Xηγ—小河二长花岗岩;A—内蚀变带;B—中蚀变带;C—外蚀变带;D—正常围岩
Fig.8. Silver orebody plane in mining area (a)、No.00 prospecting line profile map (b)[
1—geological boundary;2—fault and occurrence;3—orebody and number;4—exploration line and number;5—drilling and number;6—alteration boundary;Q—Quaternary;Jxg—Gaoshanhe formation;Ar3T—Archaeozoic Taihua group;Pt2Xηγ—Xiaohe monzonitic granite;A—internal alteration zone;B—medium alteration zone;C—external alteration zone;D—normal surrounding rock
