Combination Of Geochemical Elements Divergent Research Model

Mineral resources are forecast to learn engineering, processing and analysisrelated to various geological information, geochemical divergent theoreticalprediction of the three divergent as mineral target one theory, the main elements ofspace and reveal the distribution of geochemical elements assemblages.Haoyungoucopper area is located in the Kumux-Ygor Daban metallogenic belt, with multi-stagemineralization characteristics.1:10000rock geochemical survey was conducted inthis area,1、An established element of spatial combination of qualitative models.statistics shows that: As, Hg, Bi, Fe and other elements relatively enriched, Cu, Zn,Ag, Hg, As, Pb, Bi, W, Sb, has a larger coefficient of variation. Single element withhorizontal zonation, On the basis of characteristic groups of elements circle the threeabnormal target area.abnormal (Cu-As-Pb-Zn-Hg) Low medium temperaturemineral association,Large scale abnormal area,high content element,complexcombination and well setting together.anomaly (Cu-As-Pb-Zn-Sn-Mo) medium-hightemperature mineral association,abnormal concentration centers obvious but the areais relatively small. abnormal (Cu-As-Pb-Zn) medium temperature mineral association.2、Create a factor-Pan Kriging model, the17elements of the factor analysis, selectfive main factors, F1has a high load element variable: Cr, Fe, Co, Cu. Fe, Co, Crcontent is high, indicating that the set of elements of the base component is high, apositive correlation between Cr, Mn, Fe, Co, Cu, As, Ba, Hg, Pb, Zn, As, Pb, Zn procopper, Pb, Zn is associated elements copper, indicating element polymetallicdeposits. Ba elements and marine sedimentary massive sulfide deposits relatedelements Ba element is also the former Halo hydrothermal deposits, Hg, Ashydrothermal activity indicator elements. F2has a high load factor variable elements:Cd, Pb, Zn hydrothermal sulfides. A load element having a high variable factor F3respectively: Zn, W, Bi, etc. General description of the set of elements Low-the role of hydrothermal mineralization, is to find a sign of hydrothermal base metalmineralization. F4has a higher load factor variable elements: Hg, Ni the set ofelements related hydrothermal sulfide, with higher load factor F5elements: Bi, Moore-forming elements are high temperature, sum up the role of the regional geologymineralization characteristic temperatures-with multiple stages, as hydrothermalsulfide deposits, with a low temperature-high temperature.Based on a combinationof elements characteristic of the study area and geological characteristics of the threeexceptions anomaly evaluation, unusual for the level1,2and3for the two anomalies.An area for geochemical anomaly large proportion of induced polarization,high-precision magnetic survey work on the chemical model validation work showslow resistance electrical shock high polarization characteristics. Magneticmeasurements indicate positive and negative anomalies F2fault on both sides, ingood agreement with the geologic map. Both models can better reflect the study areaEarth.Distribution of chemical elements, the combination of features, quickly findchemistry abnormalities carried preferred target mineralization.