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MDD法和裂变径迹法相结合模拟样品的低温热历史——以柴达木盆地北缘赛什腾山中新生代构造演化为例
引用本文:万景林,郑德文,郑文俊,王伟涛.MDD法和裂变径迹法相结合模拟样品的低温热历史——以柴达木盆地北缘赛什腾山中新生代构造演化为例[J].地震地质,2011,33(2):369-382.
作者姓名:万景林  郑德文  郑文俊  王伟涛
作者单位:中国科学院广州地球化学研究所;中国地震局地质研究所地震动力学国家重点实验室;
基金项目:国家自然科学基金(40672134,40472112); 中国地震局地质研究所基本科研业务专项(DF-IGCEA0607122)共同资助
摘    要:MDD法和裂变径迹法是2种最常用的低温热年代学方法.通过对它们的测试结果的模拟,揭示出样品经历的热历史,可以有效地延伸这2种方法的研究范围.但是由于模拟的多解性,使得如何制约模拟过程,获得合理的模拟结果显得尤为重要.通过柴达木盆地北缘的模拟过程,展示了模拟中可能存在的问题及提高模拟结果的方法.同时揭示了柴达木盆地北缘中...

关 键 词:新生代构造  钾长石MDD  裂变径迹  快速冷却  青藏高原东北缘
收稿时间:2010-04-26
修稿时间:2010-11-11

MODELING THERMAL HISTORY DURING LOW TEMPERATURE BY K-FELDSPAR MDD AND FISSION TRACK:EXAMPLE FROM MESO-CENOZOIC TECTONIC EVOLUTION IN SAISHITENGSHAN IN THE NORTHERN MARGIN OF QAIDAM BASIN
WAN Jing-lin,ZHENG De-wen,ZHENG Wen-jun,WANG Wei-tao.MODELING THERMAL HISTORY DURING LOW TEMPERATURE BY K-FELDSPAR MDD AND FISSION TRACK:EXAMPLE FROM MESO-CENOZOIC TECTONIC EVOLUTION IN SAISHITENGSHAN IN THE NORTHERN MARGIN OF QAIDAM BASIN[J].Seismology and Geology,2011,33(2):369-382.
Authors:WAN Jing-lin  ZHENG De-wen  ZHENG Wen-jun  WANG Wei-tao
Institution:WAN Jing-lin1,2) ZHENG De-wen2) ZHENG Wen-jun2) WANG Wei-tao2)1)Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China1)State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China
Abstract:K-Feldspar MDD(Multiple Diffusion Domain)and fission track are two commonly-used methods in low closure temperature thermal chronometry.By modeling both the feldspar 39Ar/40Ar data and the fission track age and track-length data,the thermal history that sample underwent can be revealed and the effective temperature range of both feldspar 39Ar/40Ar method and fission track method is extended.Because of the multiple resolution of modeling,it is important to restrict the modeling process to gain a reasonable r...
Keywords:Cenozoic tectonic  K-Feldspar MDD  fission track  rapid cooling  northeastern margin of Tibetan Plateau  
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