Calcite Sm-Nd isochron age of the Shuiyindong Carlin-type gold deposit, Guizhou, China | |
Wenchao Su; Ruizhong Hu; Bin Xia; Yong Xia; Yuping Liu | |
2009 | |
发表期刊 | Chemical Geology |
卷号 | 258期号:3-4页码:269-274 |
合作性质 | 其它 |
摘要 | 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 εNd 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. |
关键词 | Sm-nd Geochronology Hydrothermal Calcite Decarbonation And Gold Deposition Carlin-type Gold Deposit Guizhou |
学科领域 | 矿床地球化学 |
收录类别 | SCI |
语种 | 英语 |
文献类型 | 期刊论文 |
条目标识符 | http://ir.gyig.ac.cn/handle/352002/3088 |
专题 | 矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文 矿床地球化学国家重点实验室 期刊图书信息中心 |
推荐引用方式 GB/T 7714 | Wenchao Su,Ruizhong Hu,Bin Xia,et al. Calcite Sm-Nd isochron age of the Shuiyindong Carlin-type gold deposit, Guizhou, China[J]. Chemical Geology,2009,258(3-4):269-274. |
APA | Wenchao Su,Ruizhong Hu,Bin Xia,Yong Xia,&Yuping Liu.(2009).Calcite Sm-Nd isochron age of the Shuiyindong Carlin-type gold deposit, Guizhou, China.Chemical Geology,258(3-4),269-274. |
MLA | Wenchao Su,et al."Calcite Sm-Nd isochron age of the Shuiyindong Carlin-type gold deposit, Guizhou, China".Chemical Geology 258.3-4(2009):269-274. |
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