• 责任者：Wang Hongwei (Faculty of Land Resource Engineering ; Kunming University of Science and Technology ; Kunming 650093 ; China) ; Wen Xingping
• 刊名：Geoscience
• 出版年：2013
• 卷期：27(3)
• 关键词：锰矿 ; manganese ores ; 云南 ; Yunnan Province
• 页码：p.612-620
• 图表：6 illus., 2 tables, 22 refs.
• 分类号：1001
• issnNo：ISSN1000-8527
• isbnNo：CN11-2035/P

     Heqing manganese deposit is located in the southwestern margin of Yangtze platform in Yunnan Province, China. Carbon and oxygen isotopes indicate that Songgui Formation which is the main ore bearing stratum experienced one transgression and another long-term regression. The paleotemperature derived from oxygen isotopes are higher due to the exchange of oxygen isotope between biological (algae) metabolites and seawater, changes in paleoclimate and sea depth. With uplifting of Yangze platform continuously and climate changing from humid, hot into arid gradually, the manganese ores were formed accompanied by falls in sea level.