Chronology and Genesis of S-type Granites in Hetai District, Guangdong Province: Constraints from LA-ICP-MS Zircon U-Pb Dating and Tourmaline Boron Isotope In-situ Analyses
Chronology and Genesis of S-type Granites in Hetai District, Guangdong Province: Constraints from LA-ICP-MS Zircon U-Pb Dating and Tourmaline Boron Isotope In-situ Analyses作者机构:CAS Key Laboratory of Mineralogy and MetallogenyGuangzhou Institute of GeochemistryChinese Academy of Sciences University of Chinese Academy of Sciences
出 版 物:《Acta Geologica Sinica(English Edition)》 (地质学报(英文版))
年 卷 期:2017年第91卷第S1期
页 面:96-97页
核心收录:
学科分类:070902[理学-地球化学] 0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学]
基 金:co-funded by the China Geological Survey (No.12120114052801) the DREAM project of MOST, China (NO. 2016YFC0600401)
主 题:Pb Chronology and Genesis of S-type Granites in Hetai District Constraints from LA-ICP-MS Zircon U-Pb Dating and Tourmaline Boron Isotope In-situ Analyses Guangdong Province type
摘 要:1 Introduction Hetai district,which is a mountainous area,situated on Guangning and Zhaoqing city,west Guangdong *** district is generally located on southwest of South China Caledonian fold belt,east margin of Yunkai post-Caledonian *** type granites are widely distributed in Hetai district,including Caledonian,Indosinian and Yanshanian *** on different