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In Dagelegounao Regions Ore-Forming And Prospective Evaluation Of The Gold

Posted on:2014-12-07Degree:MasterType:Thesis
Country:ChinaCandidate:H JiaoFull Text:PDF
GTID:2250330425962674Subject:Geological Engineering
Abstract/Summary:PDF Full Text Request
Large gold and copper mining Degelegounao is located at the south side offracture Kun, located in the snow-capped peak of Boolean Jersey DahualixiIndosinian stage cobalt, gold, copper, jade (rare, rare earth) metallogenic belt(III13), the metallogenic belt is located in the south of East Kunlun orogenicbelt, is the active region, metallogenic epoch times the type of complex. TheCaledonian metallogenic period, with the development of related to marine ofbasic to acidic volcano rocks of copper, lead, zinc, cobalt metallogenic series of ore deposits, ore deposit types as the volcano sedimentary exhalative type,the Tuolugou Cobalt (gold) deposit, Dulenggou copper (cobalt) deposit, the toothwas copper occurrences as representative. The Hercynian-Indosinianmetallogenic period is the more important, mineralization is quite common,mainly in gold, polymetallic, but on a small scale, many species occurrences,mineralization. Mineralization and synorogenic intermediate-acid intrusiverocks are closely related, deposit type is contact metasomatic type,hydrothermal type and quartz vein and tectonic altered rock type (gold) deposit,this constitutes a gold, copper, lead, zinc, iron, rare earth depositmetallogenic series related to granitoids. The more important deposits (points)have land reclamation North gold deposit, Xiaonangou gold deposit, Nachitaicopper, halagatu polymetallic ore spot, didn’t really sang lead mines, A De pullrod ang rare earth ore etc.Study area the distribution of large areas of Wanbaogou group volcanorock and the overlying upper Triassic sandstone of Babaoshan formation in three.1∶50000stream sediment of gold and copper anomaly is mainly distributed inthe Wanbaogou group volcano rock strata and two sets of the stratigraphic contactzone, small amounts of copper anomaly distribution in Babaoshan formation ofTriassic sandstone in three. In recent years through the census work, many goldand copper mineralization points have been found in the area. Through drillingdeep validated, the discovery of gold of3layers in the ZK04hole, althoughthe taste is not very high but enough to prove that the gold mineralization ofthe facts.Increase the intensity of the gold ore belt of the south of the study areaof erosion, continued in the mineralized alteration zone of the strike and dipof trenching and drilling were selected for recourse, control, in order toachieve better results prospecting.
Keywords/Search Tags:Dongkunlun, Gold mine, Orogenic, The ore-controlling factors, Prospecting foreground
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