THE APPLICATION OF SOIL GEOCHEMICAL SURVEY TO GEOLOGICAL PROSPECTING IN TARAPACÁ REGION,CHILE
WANG Ming-guo1,2, ZHANG Xiao-yong1,2, BAI Feng-jun1,2, WEN Jing-jing1,2, WANG Ming-ming1,2
1. Henan Nonferrous Metal Geological Exploration Institute, Zhengzhou 450052, China;
2. Key Laboratory of Deep Ore-prospecting Technology Research for Non-ferrous Metal of Henan Province, Zhengzhou 450052, China
To verify the effects of soil survey in the area of arid desert landscape in northern Chile, the authors conducted sample size fraction experiment, and the results show that the sampling horizon is B or B+C soil and the best sampling size fraction is -40 mesh grain size. Through applying the method to soil survey, some Cu, Au and other anomalies were delineated, several new copper ore bodies were found. The centers of the anomalies coincide well with the copper ore bodies. The effect of soil survey is fairly good. Nevertheless, anomaly inspection shows that arid desert landscape is not conducive to the formation of geochemical anomalies, and the role of 1:50,000 soil measurement in controlling the anomaly is limited. It is therefore better to use the large-scale geochemical survey.
王明国, 张晓永, 白凤军, 温静静, 王明明. 土壤地球化学测量在智利塔拉帕卡大区 地质勘查中的应用[J]. 物探与化探, 2013, 37(3): 394-399.
WANG Ming-guo, ZHANG Xiao-yong, BAI Feng-jun, WEN Jing-jing, WANG Ming-ming. THE APPLICATION OF SOIL GEOCHEMICAL SURVEY TO GEOLOGICAL PROSPECTING IN TARAPACÁ REGION,CHILE. Geophysical and Geochemical Exploration, 2013, 37(3): 394-399.
[1] 施俊法,姚华军,李友枝,等.信息找矿战略与勘查百例[M].北京:地质出版社,2005.[2] 胡树起,马生明,刘崇民.斑岩型铜矿勘查地球化学研究现状及进展[J].物探与化探,2011,35(4):431-437.[3] 陈旺,成静亮,陈丽娟,等.智利共和国第四大区阿尔法矿区铜矿预查设计.河南省有色金属地质勘查总院,2008.[4] 成静亮,白凤军,朱红军,等.智利北部成矿规律及靶区优选研究报告.河南省有色金属地质勘查总院和一达国际矿业投资有限公司,2011.[5] 吴海成,李惠民.智利铜矿地质与矿业的特点[J].中国地质,1999(07):43-44.[6] 孙卫东,凌明星,杨晓勇,等.洋脊俯冲与斑岩铜金矿成矿[J].中国科学:D 辑,2010,40(2):127-137.[7] 侯增谦,潘小菲,杨志明,等.初论大陆环境斑岩铜矿[J].现代地质,2007,21(2):332-351.[8] 陈文林,刘良根.智利Rodados Negros 铁矿床地质特征、成矿机理与找矿前景分析[J].矿产与地质,2012,25(3):208-210.[9] Sillitoe R H.Porphyry copper systems[J].Economic Geology,2010,105:223-243.[10] Palacios C,Ramírez L E, Townley B, et al.The role of the Antofagasta-Calama Lineament in ore deposit deformation in the Andes of northern Chile[J].Mineralium Deposita,2007,42(3):301-308.[11] Sillitoe R H.Iron oxide-copper-gold deposits: an Andean view[J].Mineralium Deposita, 2003, 38(7): 787-812.[12] Tornos F, Velasco F, Barra F, et al.The Tropezón Cu-Mo-(Au) deposit, Northern Chile: the missing link between IOCG and porphyry copper systems[J].Mineralium Deposita, 2010, 45(4): 313-321.[13] Cereceda P, Larrain H, Osses P, et al. The climate of the coast and fog zone in the Tarapaca Region, Atacama Desert, Chile[J].Atmospheric Research, 2008, 87(3/4):301-311.[14] 王志华.景观地球化学研究在土壤地球化学测量中的作用[J].地质与勘探,1999,35(6):55-57.[15] DZ/T 0145-94土壤地球化学测量规范[S].[16] DZ/T 0011-2010 地球地球化学普查规范[S].[17] GERM Reservoir Database..http://earthref.org/GERMRD/.[18] 施俊法,唐金荣,周平,等.世界找矿模型与找矿勘查[M]. 北京:地质出版社,2010.[19] 李建旭,方维萱,刘家军.智利科皮亚波GV地区侵入岩地球化学及年代学研究[J].现代地质,2011,25(5):877-888.