豫西嵩县斩龙岗勘查区地球化学勘查
[Abstract]:In this paper, the element contents of 12: 20 million river system sediment, 1: 50 000 water system sediment and 1: 5 000 soil in the Zhanlong Gang exploration area are studied. The lower limit of anomaly is determined by using the 7 grade anomaly division scheme, and the single element geochemical map is made. Single element geochemical anomaly map. According to the anomalous characteristics of elements, the ore-prospecting indicator elements and prospecting directions are determined, and the prospecting targets are delineated. This article mainly obtains the following understanding: Chaolonggang exploration area is located in the southeast of Xiongershan area, the exploration area is 4.27km2. The outcropping strata in the region are mainly Xiong'er Qiping formation, the structure of which is mainly faulted and mainly controlled by the NNE fault. There is a slow dip quartz vein in the exploration area. The alteration is mainly silicification and potassium mineralization, but there is no obvious mineralization phenomenon. Based on the analysis of element contents in sediments of 12: 200 000 river systems in the exploration area, the lower limit and classification of anomalies are determined by using the scheme of anomaly division of variable value grade 7, and the analysis of single element geochemical map and single element geochemical anomaly map is combined. It can be found that there are anomalies in Mo elements in Zilonggang exploration area, which are distributed in the northern part of Zilonggang exploration area, and the anomaly level is low. Based on the analysis of geochemical survey data of 1: 50 000 in the exploration area, the lower limit and classification of anomalies are determined by using the scheme of fixed value 7 grade anomaly division, and the analysis of single element geochemical map and single element geochemical anomaly map is combined. It can be concluded that the ore-prospecting indicator elements in Zilonggang exploration area are five elements, among which the anomaly grade of au element is 2 grade, and the second grade anomaly is developed in the eastern part of the exploration area, and the gold element is distributed in the northern part of the exploration area. Based on the analysis of 1: 5000 soil geochemical exploration data in the exploration area, the lower limit of anomaly and anomaly classification are determined by using the scheme of fixed value 7 grade anomaly, and the single element geochemical map and single element geochemical anomaly map are synthesized. It is concluded that the ore-prospecting indicator elements in Zilonggang exploration area are three items, among which Mo reaches grade 4 anomaly and Pb develops grade 3 anomaly, and distributes in the northern part of exploration area. Au develops grade 3 anomaly in the middle of exploration area. According to the geochemical survey and analysis results of different scales in Zilonggang exploration area, the element assemblage anomaly is synthetically analyzed. It is determined that the three prospecting target areas in Zilonggang exploration area are: 1 target area is located in the northeast of Chaolonggang (northeast of Yingwanggou and Canggou), the prospecting direction is in the north-central part of Chaolonggang (the northeast of Caigou), the prospecting direction is in the north-central part of Chaolonggang (the northeast of the Caigou), and the prospecting direction is in Zilong. In the middle of the gang (Fanggou-Yingle ditch), the prospecting direction is: 1. The order of ore-prospecting priority is: t _ 1 / T _ 3 / T _ 2.
【学位授予单位】:中国地质大学(北京)
【学位级别】:硕士
【学位授予年份】:2015
【分类号】:P632
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