The Mineralogic Component and Metallogenesis Rule of Fake P Deposit in Shangcun, Huize, Yunnan Province
详细信息
- 责任者：Xie Wenwei (No.306 Geological Team ; Yunnan Bureau of Nonferrous Geology ; Kunming 650216 ; China) ; Zhang Weizuo
- 刊名：Yunnan Geology
- 出版年：2013
- 卷期：32(4)
- 关键词：磷矿床 ; phosphate deposit ; 云南 ; Yunnan Province
- 页码：p.443-446
- 图表：1 illus., 2 tables, 3 refs.
- 分类号：1002
- issnNo：ISSN1004-1885
- isbnNo：CN53-1041/P
摘要
The P deposit is in Lower Cambrian Yuhucun Formation （ ∈1y）. The thin, laminated P silt- stone, phosphorite, with intercalation of purple, grey - black muddy sihstone, with flat bedding as a plate. It shows the clear feature of stratabound ore deposit, the evolution from tidal high energy to subtidal energy.