物探与化探
物探與化探
물탐여화탐
Geophysical and Geochemical Exploration
2015年
5期
885-890
,共6页
任喜荣%赵国良%邓辉%王欢%谢志峰
任喜榮%趙國良%鄧輝%王歡%謝誌峰
임희영%조국량%산휘%왕환%사지봉
地面高精度磁测%直流激电中梯%综合物探%矽卡岩%多金属矿%控矿因素
地麵高精度磁測%直流激電中梯%綜閤物探%矽卡巖%多金屬礦%控礦因素
지면고정도자측%직류격전중제%종합물탐%석잡암%다금속광%공광인소
ground high-precision magnetic measurement%DC IP intermediate gradient%comprehensive geophysical prospecting%skarn%polymetallic deposit%ore-control factor
青海省鸭子沟铜多金属矿区花岗闪长岩及其滩间山群碳酸盐岩发育,是形成矽卡岩型铜多金属矿(化)体的主要控矿因素。结合区域地质、地球物理及地球化学特征,在其所判定的成矿远景区,开展了以激电中梯和地面高精度磁测为组合方式的综合物探找矿实践。利用激电中梯扫面方式圈定出激电异常体,利用地面高精度磁测来了解区内主要地质体的磁性特征,在主要剖面上部署激电测深剖面,指导钻探工作进行。勘探结果表明找矿方式效果显著、经济高效,对同类地质成矿地区的隐伏多金属矿勘探工作具有一定的参考价值。
青海省鴨子溝銅多金屬礦區花崗閃長巖及其灘間山群碳痠鹽巖髮育,是形成矽卡巖型銅多金屬礦(化)體的主要控礦因素。結閤區域地質、地毬物理及地毬化學特徵,在其所判定的成礦遠景區,開展瞭以激電中梯和地麵高精度磁測為組閤方式的綜閤物探找礦實踐。利用激電中梯掃麵方式圈定齣激電異常體,利用地麵高精度磁測來瞭解區內主要地質體的磁性特徵,在主要剖麵上部署激電測深剖麵,指導鑽探工作進行。勘探結果錶明找礦方式效果顯著、經濟高效,對同類地質成礦地區的隱伏多金屬礦勘探工作具有一定的參攷價值。
청해성압자구동다금속광구화강섬장암급기탄간산군탄산염암발육,시형성석잡암형동다금속광(화)체적주요공광인소。결합구역지질、지구물리급지구화학특정,재기소판정적성광원경구,개전료이격전중제화지면고정도자측위조합방식적종합물탐조광실천。이용격전중제소면방식권정출격전이상체,이용지면고정도자측래료해구내주요지질체적자성특정,재주요부면상부서격전측심부면,지도찬탐공작진행。감탐결과표명조광방식효과현저、경제고효,대동류지질성광지구적은복다금속광감탐공작구유일정적삼고개치。
The Yazigou copper?polymetallic deposit is located in Yaziggou area, Mangya Town, Qinghai Province. The development of granodiorite and Tanjianshan Group carbonatite in the area constitutes the main ore?controlling factors to form skarn type copper?poly?metallic orebodies. Based on regional geologucal, geophysical and geochemical features, the authors employed the IP intermediate gra?dient method and the ground high?precision magnetic comprehensive geophysical prospecting method in search for ore deposits in the predicted metallogenic prospect areas. IP intermediate gradient method was used to delineate IP body anomaly, and ground high?preci?sion magnetic measurement was adopted to detect the magnetic features of main geological bodies in the area. Along the important geo?logical sections, IP sounding was used to guide drilling work. Practice indicates that this method is very effective and efficient, and has the reference value for exploration of concealed polymetallic deposits in similar metallogenic regions.