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Late Cretaceous-Cenozoic exhumation history of Tiantangzhai region of Dabieshan Orogen: Constraints from (U-Th)/He and fission track analysis
作者姓名:ZHOUZuyi  XUChanghai  P.W.Reiners  YANGFengli  R.A.Donelick
作者单位:[1]MOELaboratoryofMarineGeology,TongjiUniversity,Shanghai200092,China. [2]DepartmentofGeologyandGeophysics,YaleUniversity,NewHaven,CT06520-8109,USA; [3]DonelickAnalytical,Inc.,Viola,ID83872,USA
基金项目:国家重点基础研究发展计划(973计划),国家自然科学基金 
摘    要:Integrated fission track and (U-Th)/He analysis is carried out on 6 apatite and 6 zircon samples from a near vertical section in The Tiantangzhai region at the core of the present Dabieshan orogen. The result shows that the region experienced cooling/exhumation during the Late Cretaceousand Early Tertiary period. Age-elevation relationships for different dating systems and different minerals suggest a pulse of rapid exhumation at ~110 Ma before present, preserved in the structurally highest samples. At lower elevations, ages begin to decrease with decreasing elevation, suggesting lower exhumation rates since 90 Ma. Two periods of different exhumation rates are identified since 90 Ma. The average apparent exhumation rate for the period of 43.4—22.5 is 0.062 km/Ma, whereas that for the period of 76.4—47.4 Ma is 0.039 km/Ma.

关 键 词:大别山  造山运动  海拔高度  第三纪  白垩纪  造山带
收稿时间:2002-10-28
修稿时间:2003-01-02

Late Cretaceous-Cenozoic exhumation history of Tiantangzhai region of Dabieshan Orogen: Constraints from (U-Th)/He and fission track analysis
ZHOUZuyi XUChanghai P.W.Reiners YANGFengli R.A.Donelick.Late Cretaceous-Cenozoic exhumation history of Tiantangzhai region of Dabieshan Orogen: Constraints from (U-Th)/He and fission track analysis[J].Chinese Science Bulletin,2003,48(11):1151-1156.
Authors:Email author" target="_blank">Zuyi?ZhouEmail author  Changhai?Xu  P?W?Reiners  Fengli?Yang  R?A?Donelick
Institution:e-mail: zhouzy @mail.tongji.edu.cn
Abstract:Integrated fission track and (U-Th)/He analysis is carried out on 6 apatite and 6 zircon samples from a near vertical section in The Tiantangzhai region at the core of the present Dabieshan orogen. The result shows that the region experienced cooling/exhumation during the Late Cretaceous and Early Tertiary period. Age-elevation relationships for different dating systems and different minerals suggest a pulse of rapid exhumation at ~110 Ma before present, preserved in the structurally highest samples. At lower elevations, ages begin to decrease with decreasing elevation, suggesting lower exhumation rates since 90 Ma. Two periods of different exhumation rates are identified since 90 Ma. The average apparent exhumation rate for the period of 43.4-22.5 is 0.062 km/Ma, whereas that for the period of 76.4-47.4 Ma is 0.039 km/Ma.
Keywords:Dabieshan  Tiantangzhai  (U-Th)/He dating  fission track analysis  exhumation  
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