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《Progress in Geophysics》 2008-02
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Discussion about using different modes of apatite fission track thermochronology to constrain cooling histories of rocks:an example from the batholith in Dulong River region,west Yunnan

LEI Yong-liang1,2,GONG Dao-hao2,WANG Xian-mei2,ZHONG Da-lai2,WANG Xue-song1,ZHANG Jin3(1.Institute of Petroleum Exploration and Development,Petrochina,Beijing 100083,China;2.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;3.Institute of Geology,China Earthquake Administration,Beijing 100029,China)  
As using apatite fission track thermochronology to constrain the cooling histories of rocks,it is constrained by geological settings and natures of apatite fission track annealing that the apparent ages of apatites are generally not proxies for the time of specific geological events directly.Using the confined track length histogram and elevation-age mode can qualitatively reflect whether the cooling history of batholith has undergone some disturbances.Mean track length-age mode(or boomerang plot),track age spectrum mode and inverse modeling can constrain the onset time of discrete cooling histories to some extent.However,when to analyze the multi-episode cooling histories recorded by apatite fission track,the uncertainties in these modes and modeling are still remarkable that a difficulty on research is to qualify the time of the earlier episode of cooling histories.To constrain the cooling histories of rocks clearly,it is necessary to combine various methods,modes and modeling results together with a consideration about geological settings.
【Fund】: 国家自然科学基金重点项目(40234049 40702035)资助
【CateGory Index】: P314
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