Progress in Methodology of Low Temperature Thermochronometry
被引:0
作者:
GONG Gelian
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机构:
State Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of SciencesState Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences
GONG Gelian
[1
]
ZHOU Jibin
论文数: 0引用数: 0
h-index: 0
机构:
State Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of SciencesState Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences
ZHOU Jibin
[1
]
SUN Weidong
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h-index: 0
机构:
Key Laboratory of Mineralogy and Metallogeny,Guangzhou Institute of Geochemistry,Chinese Academy of SciencesState Key Laboratory of Isotope Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences
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
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