Progress in Methodology of Low Temperature Thermochronometry

被引：0
|
作者：
GONG Gelian [1 ]
ZHOU Jibin [1 ]
SUN Weidong [2 ]
机构：
[1] State Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences
[2] Key Laboratory of Mineralogy and Metallogeny,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences
来源：
Acta Geologica Sinica(English Edition) | 2016年 / 05期
基金：
中国国家自然科学基金;
关键词：
Th; Progress in Methodology of Low Temperature Thermochronometry;
D O I：
暂无
中图分类号：
P597 [同位素地质学与地质年代学];
学科分类号：
070902 ;
摘要：
Objective Thermochronometry is based on the temperaturedependent radiogenic/fissionogenic products(e.g.,fission track or a particle)or the radiation effects of a radioactive isotopic system for a single mineral.The characteristics of a thermochronological system can be described by its closure temperature,which is determined by the thermal structure of geological cases.Both closure temperature
引用
收藏
页码：1927 / 1928
页数：2
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