Calcite Sm-Nd isochron age of the Shuiyindong Carlin-type gold deposit, Guizhou, China

详细信息    查看全文

• 作者：Wenchao Su ; Ruizhong Hu ; Bin Xia ; Yong Xia ; Yuping Liu
• 关键词：Sm-Nd geochronology ; Hydrothermal calcite ; Decarbonation and gold deposition ; Carlin-type gold deposit ; Guizhou
• 刊名：Chemical Geology
• 出版年：2009
• 出版时间：30 January 2009
• 年：2009
• 卷：258
• 期：3-4
• 页码：269-274
• 全文大小：1424 K

文摘

Shuiyindong is one of the largest and highest grade, stratabound Carlin-type gold deposits in China. It is hosted in Permian bioclastic limestone near the axis of an anticline. Hydrothermal calcite is common on the periphery of central zones of ferroan carbonate dissolution that provided the main source of iron that was sulfidized during gold deposition. These calcite veins contain relatively high concentrations of rare earth elements with MREE-enriched patterns, and yield Sm-Nd isochron ages of 134 ± 3 Ma to 136 ± 3 Ma, with significant different initial ε_Nd values of − 12.9 and − 2.0, respectively. These ages are interpreted to record age of decarbonation and gold deposition during the late stages of Yanshanian Orogeny. The initial Nd isotopic compositions of the calcites suggest that Nd was primarily derived from the Permian Longtang Formation that hosts all ore bodies at the deposit. This study shows that Sm-Nd isotopic compositions of hydrothermal calcites can be used to constrain the age and source of Nd in Carlin-type gold deposits.