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This article provides an overview of the study area regional metallogenic geological background and geological mineral characteristics, large amounts of data acquired by the Geological Survey in the wild, a typical cross-sectional study, indoor observation analysis test, on the basis of the data, the focus from the study area, the type of gold mineralization, ore-controlling several factors, mineral characteristics, trace element geochemistry of prospecting area, Liping Kupang gold mineralization zone, and come to the following understanding: 1, the main type of gold mineralization altered rock type gold mineralization, the local section presence of quartz vein type gold deposits and altered rock type gold deposits accompanied students. Speculated in Kupang North East to the the Yahan penthouse anticline axis surface position as well as the associated small structure in the bedding detachment zone or layer peeling space output quartz vein type gold deposits, but small. 2, Yahan duplex anticline is the major anticlinal structure secondary fold structures control the major alteration (fracture) with cleavage development and distribution. Specific performance is mainly affected by the alteration zone in the region GOLD (of) the Yahan duplex anticlines North West Wing regional north-trending of Kupang reverse fault and high green ground floor fault the secondary faults F 3 , F 4 , F 5 controlled. 3, by field observations, microscopic identification, and electron probe analysis found in the region the Ming gold, pyrite, arsenopyrite, scorodite, limonite, galena, hematite, quartz, barite, mica, illite, albite, rutile, zircon, chlorite and clay minerals, etc.; Also in the area also found that the rare-earth minerals, which mostly monazite. The several mineral illite, rutile, chromite, zircon, barite, albite, and monazite region first discovered. These findings contribute to the research area type of gold mineralization and ore prospects. 4, through field research and analysis of trace elements with gold, gold prospecting indicators of the study area with the understanding of the system. Silicification, arsenopyrite, pyrite, magnetite, stibnite mineralization altered superimposed parts, especially the first three superimposed parts, effective prospecting flag. 5, REE patterns show that the quartz vein type gold mine into the minerals are mainly derived from the deep crust, but the combination of the previous studies have shown that, partly from the surrounding rock. Altered rock type gold ore bodies (of) into minerals derived from deep small part from the surrounding rock. 6 region altered rock type gold prospecting range mainly fade alteration zones with high green ground fault near the change in Asia and its secondary binding site of the fracture. Range of composite gold prospecting students accompanied by quartz vein type gold deposits and altered rock type gold should be concentrated in Kupang is the east the D 3 Geological near the surface of layered quartz veins type gold mineralization, deep altered rock type gold deposits may exist. 7, according to the \
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