周迎春.海南岭壳铜(银-金)矿床地质特征及找矿方向[J].地质找矿论丛,2008,(3):209-212,244
海南岭壳铜(银-金)矿床地质特征及找矿方向
GEOLOGICAL CHARACTERISTICS AND PROSPECTING DIRECTIONS IN LINGQIAO Cu(Ag-Au) DEPOSIT,HAINAN PROVINCE
投稿时间:2007-04-06  修订日期:2007-12-25
DOI:10.6053/j.issn.1001-1412.2008.3. 008
中文关键词:  围岩蚀变  分形统计  找矿方向  岭壳铜(银-金)矿床  海南省
英文关键词:wallrock alteration  fractal statistics  ore prospecting  Lingqiao Cu(Ag-Au) deposit  Hainan province
基金项目:中国地质大调查项目(1212010533801);《海南同安岭地区矿产远景调查》(矿调[2004]15-1)资助
作者单位
周迎春 海南省地质调查院, 海口, 570206 
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中文摘要:
      岭壳铜(银-金)矿床赋存于白垩纪岭壳村组流纹质角砾凝灰熔岩和早白垩世花岗闪长岩中。目前已发现11条铜(银-金)矿(化)体,矿体的产出严格受断裂破碎带控制,与成矿关系密切的围岩蚀变呈现出自东(20线)向西的钾化→绢云母化→强高岭石化、绿泥石化蚀变分带,矿化相应呈现从铜(金)向铜(银)的过渡。根据其对称性的蚀变分带,应加强20线以东的地质找矿;根据成矿元素分形和统计研究发现,Au,Ag矿化具有专属性,即在流纹质凝灰熔岩中寻找Cu,Ag矿,而在花岗闪长岩中以寻找Cu,Au矿为主。
英文摘要:
      Lingqiao Cu(Ag-Au) deposit is hosted in rhyolitic breccia tuffaceous lava of the Cretaceous Lingqiao formation and in the early Cretaceous granodiorite.At present,eleven ore(mineralized) bodies have been discovered.These ore bodies are strictly controlled by fault zones.The ore-related wallrock alteration can be divided into potassium zone,sericitization zone,strong kaolinization and chloritization zone from east(exploration line 20) to the west.And ore mineralizing types change from Cu-Au to Cu-Ag.Systematic studies of the ore geological characteristics show that the mineralization characteristics of the Lingqiao deposit are similar to that of the classical porphyry copper deposit.Therefore,further prospecting work should be focused on the region in east of exploration line 20 according to the symmetry alteration zoning features of the porphyry copper deposit.Moreover,fractal and statistical analysis of ore-forming elements indicate that Au and Ag mineralization are developed in specified rocks,that is,rhyolitic breccia tuffaceous lava is benefit to Cu and Ag mineralization,while the granodiorite is the main Cu and Au hosting rock.
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