<P style="MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Taoxi Uplift of Wuyi Metallogenic Belt, Its Tectonics, Magmatism and Metallogenypace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>

详细信息   

• 责任者：Chen Shizhong (Nanjing Institute of Geology and Mineral Resources ; China Geological Survey ; Nanjing 210016 ; China) ; Ma Ming
• 刊名：Earth Science
• 出版年：2010
• 卷期：35(6)
• 关键词：铜矿 ; copper ores ; 多金属矿 ; polymetallic ores ; 武夷山 ; Wuyi Mountains
• 页码：p.969-984
• 图表：11 illus., 4 tables, 136 refs.
• 分类号：1001
• issnNo：ISSN1000-2383
• isbnNo：CN42-1233/P

摘要

<P>pt; mso-font-kerning: 1.0pt; mso-fareast-font-family: 宋体; mso-ansi-language: EN-US; mso-fareast-language: ZH-CN; mso-bidi-language: AR-SA" lang=EN-US>Taoxi uplift is a part of Wuyishan uplift and occurs as metamorphic core complexes. There are abundant medium to large scale copper and polymetallic ore deposits distributed in the uplift, such as the super large scale Zijinshan copper-gold deposit, super large Yanbei tin deposit, and large scale Hongshan copper deposit. The main geochronology dating of mineralization concentrates in the range of 130~90 Ma, the late Yanshan period. The ore deposits, as well as most copper-gold ore deposits located in Taoxi uplift are of porphyry-magmatic hydrothermal type.&nbsp;