青海省格爾木市河西地區(qū)金礦成礦預(yù)測(cè)
[Abstract]:The tectonic location in Hexi area is located at the junction of the East Kunlun arc basin system and the Kangxiwa-South Kunlun-Mado-Maqin-Mian County-Laoyang docking zone. The main body of the tectonic line is NW-trending, and the Dongkun fault rift belt crosses the central and southern parts of the study area. Through Caledonian, Variscan, Indosinian and Yanshanian magmatic activities, the exposed strata are mainly composed of Gu Yuan Paleozoic crystalline basement, Miocene Proterozoic metamorphic basement and Triassic clastic rock-volcanic rock formation. Jinning period, Hualixi period, Indo-Chinese period multi-stage sub-regional metamorphism, has good copper, gold, lead, zinc, nickel and other non-ferrous metals, precious metal ore metallogenic conditions. A comprehensive and systematic analysis of the metallogenic geological background, geochemical conditions and geophysical conditions has been made in this paper, and a great deal of useful information has been obtained from the comprehensive collection of the existing regional geological and mineral resources data in the area in which the ore-forming geological background, geochemical conditions and geophysical conditions of the study area have been studied. By comparing the geological characteristics of typical ore deposits in the area, the ore-controlling factors in Hexi area are analyzed, the ore-prospecting criteria are determined, the ore-prospecting model is established, and the prospecting prospect and favorable targets for ore-prospecting are comprehensively delineated. The main achievements and understandings obtained in this paper are as follows: (1) the geological data of Hexi area are collected systematically, the text data are classified and merged, and the map data are vectorized and attribute structure added on the MAPGIS platform. The basic geological database of the study area has been established. (2) the geochemical conditions in Hexi area have been systemically sorted and studied, and four comprehensive anomalies related to Au have been analyzed and described respectively. Among them, the HS25 anomaly, which is of high intensity and obvious concentration center, is an anomaly caused by one ore. Copper and gold mineralization points are found in the HS23,HS32,HS33 anomaly, which confirms the existence of the anomaly. (3) the types and distribution characteristics of the typical gold deposits in the study area are studied in detail. (4) the metallogenic geological conditions in Hexi area are analyzed systematically, and the ore-forming geological conditions in Hexi area are analyzed systematically. (3) the gold deposit types and distribution characteristics of the typical gold deposits in the study area are studied in detail. The prospecting criteria are determined and the predictive prospecting model is established. Finally, three prospecting prospect areas are comprehensively delineated in the study area, and three key target areas, five medium target areas and one general target area are determined.
【學(xué)位授予單位】:成都理工大學(xué)
【學(xué)位級(jí)別】:碩士
【學(xué)位授予年份】:2017
【分類號(hào)】:P618.51
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