摘要
lang=EN-US style="FONT-SIZE: 14pt; FONT-FAMILY: ’Times New Roman’; mso-fareast-font-family: 宋体; mso-ansi-language: EN-US; mso-fareast-language: ZH-CN; mso-bidi-language: AR-SA; mso-font-kerning: 1.0pt">On the basis of the discussion of the metallogenetic characters in the stratum vertical succession of gold deposits in southeastern Guizhou Province, it’s speculated that Karlin gold deposit existed in the Early Palaeozoic group on the Jiangnan organic belt. Although the metallogenic conditions of gold deposit in southeastern Guizhou Province is worse than west Hunan and the Karlin gold deposit has not be found yet, it still has good exploration potential. Anticline, especially the Jialidong period anticlinal structure and its associated rift structure is the most important controlled geologic condition for the mineralization of gold deposits in southeastern Guizhou Province, so is the preferred target region for the mineralization forecast and prospecting, especially the fold rift structure which has gold and its associated element geochemical abnormality distributed is important prospecting target.