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《Journal of Jilin University(Earth Science Edition)》 2008-05
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Uplift and Topography Evolution Research at FT in Cenozoic of South-Eastern Slope of Daxing'anling Mountains

FANG Shi1,LIU Zhao-jun1,HUANG Xiang-tong2,GUO Wei1,LIU Zhi-qiang3 1.College of Earth Sciences,Jilin University,Changchun 130061,China2.College of Ocean and Earth Sciences,Tongji University,Shanghai 200092,China3.Huabei Logging Branch of Bohai Drilling Engineering Company,Renqiu,Hebei 062552,China  
According to AFT thermal chronology,the research shows the uplift rate is 29.68 m/Ma,the uplift quantity is 1 944 m,the average reduced temperature is 103.5 ℃,the average gradient of ground temperature is 53.24 ℃/km in Cenozoic of south-eastern slope of Daxing'anling Mountains.In the domain of time,uplift of south-eastern slope of Daxing'anling reveals its act character;its velocity shows 5 lowliness and 4 highnesses.And 4 highnesses are 56.44-49.65 Ma,40.40-31.80 Ma,25.00-17.91 Ma,11.72-4.45 Ma.In the domain of space,the uplift-denudation and topgraphy evolution showed 4 phases.The first phase is pinned divide model whose pin is at FT4 point in 65.50-56.44 Ma.The second phase is downwarp model in 56.44-40.40 Ma.The third phase is pinned divide model whose pin is at FT1 point in 40.40-8.00 Ma.The fourth phase is pinned divide model whose pin is at FT7 point in 8.00-0.00 Ma.The types of topography transformed during the high speed period of the whole uplift.
【Fund】: 国家油气专项(XQ-2004-07-03-03);; 吉林大学青年教师基金(420010302355)
【CateGory Index】: P541
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