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《Journal of Jilin University(Earth Science Edition)》 2006-02
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The Analyses of Cenozoic Sandstone Component in Hongsanhan No.1 Area and Its Tectonic Implications

GUO Xin-zhuan~1,LIU Yong-jiang~1,GE Xiao-hong~1,YUAN Si-hua~1,SUN Zhi-ming~2,PEI Jun-ling~2,LI Wei-min~11.College of Earth Sciences,Jilin University,Changchun130061,China2.Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing100081,China  
The highly precise magnetochronologic study indicates that the age of Xiaganchaigou and Shangganchaigou Formations in Hongsanhan No.1 area is in the range of 40-26.5 Ma.The dividing age between Xiaganchaigou and Shangganchaigou Formations is 35.5 Ma.According to the relativity of the sediment area and source provenance,Cenozoic sandstone samples,collected from Hongsanhan No.1 section in Qaidam Basin,have been analyzed by using Dickinson-Gazzi method.The results suggest that the sandstone components are sensitive to the provenance tectonic changes.The analyses of the sandstone components suggest that the sedimentary environment was relatively stable during Xiaganchaigou period,and reveal that the Altyn Mountains had not uplifted rapidly at that time.But during Shangganchaigou period the sedimentary environment became unstable,combining with regional thermochronologic data,it indicates that the Altyn Mountains were uplifted strongly in Oligocene,which may be caused by the fast strike-slip movement along the Altyn fault.
【Fund】: 国家自然科学基金项目(40572135 40272099);; 高等学校博士学科点专项科研基金项目(20040183055);; 吉林大学青年教师基金项目
【CateGory Index】: P588.212.3;P548.2
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