Chronology and Genesis of S-type Granites in Hetai District, Guangdong Province: Constraints from LA

• 作 者: WANG Lixing XU Deru CHEN Genwen ZHU Yuhua
• 机 构: CAS Key Laboratory of Mineralogy and Metallogeny,Guangzhou Institute of Geochemistry,Chinese Academy
• 出 处: Acta Geologica Sinica(English Edition)
• 发表日期: 2017年S1期
• 关键词: Guangdong Genesis district District Isotope uplift margin southwest granite situ

1 Introduction Hetai district,which is a mountainous area,situated on Guangning and Zhaoqing city,west Guangdong Province.Hetai district is generally located on southwest of South China Caledonian fold belt,east margin of Yunkai post-Caledonian uplift.Multiple type granites are widely distributed in Hetai district,including Caledonian,Indosinian and Yanshanian granites.Based on different

1 Introduction Hetai district, which is a mountainous area, situated on Guangning and Zhaoqing city, west Guangdong Province .Hetai district is generally located on southwest of South China Caledonian fold belt, east margin of Yunkai post-Caledonian uplift. distributed in Hetai district, including Caledonian, Indosinian and Yanshanian granites.Based on different