玻利维亚盆山原镶嵌构造区特殊景观区沟系次生晕—遥感—构造岩相学综合评价技术组合研发与应用效果

doi:10.11720/wtyht.2019.1436

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Abstract

In this paper, the authors carried out tentative research and promotion application, which constitute an integrated approach to valley system secondary halo-remote sensing-tectonic lithofacies interpretation in basin-orogen-plateau inlaid structure and special landscape zone of the Tupiza and Cuprita copper deposits, Bolivia. Key points of combinational method and application effect are as follows: ① The key is interpreting mapping unit by remote sensing-tectonic lithofacies, which serves as base map of valley systems secondary halo and tectonic lithofacies mapping unit. Remote sensing-tectonic lithofacies interpreting can identify topography and landscape cell rapidly, and improve effective point ratio of geologic mapping and sampling of valley systems secondary halo. ② Sampling horizon and sampling depth were determined tentatively. It is known that the main sampling horizon is B soil and the best sampling size fraction is -10~+60 mesh grain size. ③ The technical method has achieved good results in application and promotion in the Tupiza and Cuprita copper deposits, which proves that the combination of technical methods is an economic, efficient and rapid comprehensive evaluation technique in basin-orogen-plateau inlaid structure and special landscape area of Andes. It also provides an effective exploration route of overseas investment, so as to control risk for Chinese-funded enterprises.

Key words： secondary halo of valley systems remote sensing-tectonic lithofacies interpretation (mapping) basin-orogen-plateau inlaid structure plateau special landscape area Bolivia

Received: 23 November 2018 Published: 25 October 2019

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Corresponding Authors: Wei-Xuan FANG E-mail: 569026971@qq.com

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	Yu-Long DU
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Yu-Long DU,Wei-Xuan FANG. Research,development and application effect of comprehensive evaluation technique of valley system secondary halo-remote sensing-tectonic lithofacies in basin-orogen-plateau inlaid structure and special landscape zone, Bolivia[J]. Geophysical and Geochemical Exploration, 2019, 43(5): 932-947.

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https://www.wutanyuhuatan.com/EN/10.11720/wtyht.2019.1436 OR https://www.wutanyuhuatan.com/EN/Y2019/V43/I5/932

Structural unit and the location of tentative and application area
1—Western Cordillera,average altitude of more than 4 500 m, sign of modern Andean main magma arc; 2—Altiplano plateau, average altitude of 4 000 m, composed of a number of inter-mountain basins, belongs to Tin polymetallic ore belt; 3—Eastern Cordillera, Au-Sb and Pb-Zn belt; 4—Subandean zone (thrust fold belt); 5—Craton (①Madre de díos plains, ②Beni plains, ③Chaco plains); 6—study area(Tu is the experimental area, Cup is application area); 7—provincial Capital; 8—other city; 9—plateau salt lake (SC is Coipasa salt lake, SU is Uyuni salt lake);10—plateau lake (LT is Titicaca lake, LPO is poopó lake)

Typical soil profile and special landscape in tentative area
a—mapping units and interpretation on true-color remote sensing-tectonic lithofacies, which as base map of tectonic lithofacies mapping and secondary halo of valley systems; b—geomorphologic landscape in Cuprita mine; c—level gypsum rock; d—typical soil profile of volcanic terrain area (bearing copper); e—eypical soil profile of sandstone area, strong fading alteration, atacamite filled fracture; f—typical soil profile of purplish red siltstone which was exposed in gully; g—interbedding of gray caliche with siltstone; h—weathering crust; i—saline halo

Test results of valley systems secondary halo of sampling depth and roughing grain size in Tupiza

Characteristics of composite anomalies in Class A

The anomalies analyses of Cu, Pb and Zn in Tupiza copper deposit
1—composite anomaly; 2—anomaly contour of Cu(×10^-6);3—reverse thrust; 4—copper orebody and copper metallization; 5—channel sampling point; 6—forecasting target area; 7—anomaly contour of Ta(×10^-6); 8—anomaly contour of Nb(×10^-6)

The anomalies analysis of Cu,Ag and Pb in Cuprita copper deposit
1—unconsolidated colluvial, alluvial deposits. 2—volcanogenic coarse-grained sandstones, gravelly sandstones, non-welded rhyolitic flow tuffs, reworked tuffs and silts; 3—olive gabbro; 4—plagioclase porphyries; 5—andesite volcanic breccia and volcanic agglomerate; 6—vesiculate andesite and basaltic trachyandesite; 7—basal conglomerate of copper bearing; 8—sedimentary tuff, tuffaceous sands and in-situ conglomerates; 9—feldspar sandstone, feldspar quartz sandstone; 10—inferred volcanic apparatus; 11—measured and inferred faults; 12—line of geological limitation; 13—verification copper orebody at surface (exaggerated scale); 14—forecasting target area; 15—composite anomaly and its number

NO. 0 drill hole section for anomalies verification in Tupiza tentative area, Bolivia
1—diabase-gabbro dikes, subvolcanic intrusion phase; 2—the second bed of the third member of Aroifilla formation, Upper Cretaceous, effusive facies; 3—the first bed of the third member of Aroifilla formation, Upper Cretaceous, volcaniclastic facies; 4—the second member of Aroifilla formation, Upper Cretaceous; 5—copper (silver) orebody and metallization; 6—thrust fault and fault zone and its strike direction; 7—drilling and its number; 8—copper orebody grade (%) and thickness (m); 9—associated silver at grade(10^-6); 10—measured and inferred line of geological limitation; 11—forecasting copper (cobalt) orebody

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