Abstract: Hydrothermal lode deposit is mainly controlled by fault structure. The ore-bearing or ore-hosting structures controlling the emplacement of ore-body and ore vein are often minor second-order faults or fractures,while the major faults are generally considered as passage-ways for ore fluids; however,t...
Abstract: Veins in porphyry deposits are well developed and their crosscutting relationship is complex. The initial fractures,where the veins fill in,are connected in varying degrees. Mineralization is a process of migration,filling and precipitation of ore-bearing fluid in the existing fractures. During the ...
Abstract: The NW-trending faults in the Youjiang area originated from synsedimentary faults developed in the Youjiang Basin of Late Paleozoic. In Cenozoic these equidistantly spaced faults have undergone multiple left-lateral strike-slip activities,which then led to a simple-shear deformation of the Youjiang ...
Abstract: The Xitieshan deposit,one of the large-size lead-zinc deposits located at the northern edge of the Qaidam basin in western China,is related to marine Volcanic-Sedimentary Hosted Massive Sulfur deposit (VSHMS). Most prior researches are focused on the mineralization age,the nature of ore-forming flui...
Abstract: The Xiaohe lead-zinc deposit is one of the few typical lead-zinc deposits controlled by NW-trending major faults in the ore-concentrated area in northeastern Yunnan,China. The spatial distribution of mineralization and alteration is strictly controlled by structures. In order to ascertain the charac...
Abstract: The ore-bearing rock series in the northern Hanyin gold orefield of the southern Qinling mountains mainly consists of the shallow metamorphic rocks in the Silurian Meiziya formation,which underwent complex tectonic deformation in Mesozoic,and the brittle-ductile shear zone is a good place for the en...
Abstract: The Qingshan lead-zinc deposit is one of the typical deposits in the Weining-Shuicheng metallogenic subzone in the northwestern Guizhou ore concentration area, and orebodies are strictly controlled by both tectonic and lithologic factors. The tectonites in the ore-bearing fault zone with remarkable ...
Abstract: The Wangjiaping gold deposit in Shanyang County, Shaanxi province, is a newly discovered carlin-type gold deposit in the southern Qinling orogeny, characterized by obvious ore-controlling structure and developed mineralization and alteration. The mining area is located in the north wing of the Longt...
Abstract: The Baoshan Cu-Pb-Zn polymetallic deposit, located in the overlapped part of the Nanling EW-trending tectonic belt and the Leiyang-Linwu SN-trending tectonic belt, is a typical large and super-large mineral deposit in this area. The deposit and ore-bodies are spatially closely related to the early Y...
Abstract: The Huize super-large Ge-rich Pb-Zn deposit in Yunnan is located on the southwestern margin of the Yangtze block and east of the Xiaojiang deep fault in Sichuan-Yunnan-Guizhou lead-zinc metallogenic areas, and it is controlled by the NE-trending thrust-fold structures. Although the Huize Pb-Zn depos...
Abstract: Using ASTER remote sensing images as the data source, the extraction of mineralization and alteration anomaly in the Hutouya mining area of the Qimantag metallogenic belt in Qinghai Province is studied through two methods. One method is using the minimum noise component (MNF) transform, pixel purity...
Abstract: Ashawayi gold deposit, the second largest gold deposit in the southwestern Tianshan Orogen, NW China, is located at the southern margin of the Central Asian Orogenic Belt of the "Asian Golden Belt". Detailed field observations showed that the regional area experienced two tectonic processes from ear...
Supervisor: China Geological Survey
Sponsor: Institute of Geomechanics, Chinese Academy of Geological Sciences; Geological Society of China (GSC)