Features of Sulfur Isotope of the Jiashengpan Lead-Zinc-Sulfur Deposit in oft-com:office:smarttags" />Inner Mongolia and Its Genesis Significanceoft-com:office:office" />

• 责任者：Fu Chao (State Key Laboratory of Geological Processes and Mineral Resources ; China University of Ceosciences ; Beijing 100083 ; China) ; Wang Jianping
• 刊名：Geoscience
• 出版年：2010
• 卷期：24(1)
• 关键词：硫矿床 ; sulfur deposit ; 铅锌矿床 ; lead-zinc deposit ; 硫同位素 ; sulfur isotopes ; 内蒙古 ; Inner Mongolia
• 页码：p.34-41
• 图表：8 illus., 2 tables, 23 refs.
• 分类号：1001
• issnNo：ISSN1000-8527
• isbnNo：CN11-2035/P

The Jiashengpan lead-zinc-sulfur deposit, located in Langshan-Zhaertaishan mineralization belt in the western part of northern margin of North China Platform, rich in Mesoproterozoic Zhaertaishan Group, is obviously stratabound and controlled by synchronous fault. The ore bodies are mainly composed of layered, conglomeratic and disseminated ores. The sulfur isotopic compositions of the sulfides from ores show that the values of δ³⁴S from the early depositional ores ranging from 17.0 to 31.5‰ with an average of 23.9‰ are similar to the values of δ³⁴S from the late reticulated ores ranging from 13.1‰ to 31.1‰ with an average of 24.1‰, indicating the same origin from sea sulphate.oft-com:office:office" />