xiu 1 (1 Survey of Regional Geology and Mineral Resources of Jilin Province, Changchun 130022, China;2 Information Center of Geology and Mineral Resources of Jilin Province, Changchun 130061, China) Through the comprehensive study to the multiple information of the regional geologic physical field The geophysics and geological masses of eastern part of the Northeast can be divided into three classifications (A, B and C) In space,showing a regular distribution;in characteristics,showing various differences That revealed the whole evolutionary process of the geotectonic environment of the regional lithosphere The"B"mass indicated the forming of the Archeozoic landmass The"C"mass only indicated a complex orogenic process of the Paleo-Asiatictectonic domain The"A"mass revealed a post-Mesozoic dynamic process of the crust-mantle action-the decoupling process tectonism of the forming of basin-range structure,and the intense transformation of previous tectonism JIANG Wei-wei~1, ZHOU Li-hong~2, XIAO Dun-qing~2, GAO Jia-rui~2, YUAN Shu-qin~2, TU Guang-hong~1, ZHU Dong-ying~1(1.
Dagang Oilfield Company, CNPC, Tianjin 300280, China); The characteristics of crust structure and the gravity and magnetic fields in northeast region of China[J]; Progress in Geophysics;2006-03GUO Meng-xi LIU Xing-qiao CUI De-sheng YU Ho ng-bin PENG Yu-jing (Survey of Regional Geology and Mineral Resources of Jilin Province , Changchun 130022, China); A preliminary interpretation on the deep-seated structure of the Longgang compound landmass[J]; Jilin Geology;2003-01GUO Yufu~1, HUA Wei~2, SUN Jinrong~3, LU Xiaoping~3, PENG Yujing~3 (1.
College of Earth Sciences, Jilin University , Changchun130026, China;2.
Jilin University, Changchun 130026, China); METALLOGENIC SYSTEM IN GOLD-SILVER-COPPER DEPOSITS, TAYUAN DISTRICT, HEILONGJIANG PROVINCE[J]; Journal of Changchun University of Science and Technology;2002-03YIN Changjian1,2, SUN Chunlin1, PENG Yujing2, ZHOU Xiaodong3, ZHAO Yanhua2(1.
Geological Survey Institute of Jilin Province , Changchun130061, China); DISCOVERY OF LATE CARBONIFEROUS-EARLY PERMIAN CATHAYSIAFLORA IN THE EASTERN MARGIN OF DUNHUA RISE AND ITS GEOLOGICAL SIGNIFICANCE[J]; Journal of Changchun University of Science and Technology;2003-03SUN De-you~(1,2), WU Fu-yuan~(2,3), ZHANG Yan-bin~(3), GAO Shan~(1) est University, Xi'an 710069, China;2.
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Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China2.
Regional Geologic and Mineral Resources Survey of Jilin Province, Changchun 130022, China); A preliminary analysis of geophysical characteristics in the deep part of the old land in the southern Jilin Province and its geologic significance[J]; Jilin Geology;2003-04YU Hong-bin, Lü Zhong-liang, CHANG Yong-xiang, YAO Ting-cai (Survey of Regional Geology and Minerals of Jilin Province, Changchun 130012, China); An assessment of the developmental stages of the Changbaishan volcanic activities and volcanic disasters[J]; Jilin Geology;2004-04Liu Ruoxin; Wei Haiquan; Tang Ji; Song Sengrong; Li Xiaodong; Yang Qinfu; Liu Tiesheng and Wang Jijun,(Institute of Geology, State Seicsm ological Bureau, Beijing 100029, China)(China University of Geosciences, Beijing 100083, China) (Departemt of Geolgy, Taiwan U; Progress of the Study on Tianchi Volcano, Changbaishan, China[J]; SEISMOLOGICAL AND GEOMANGNETIC OBSERVATION AND RESEARCH;1996-04Lu Zongkai (Original Name. 6101 Brigade of Geological Bureau of Jilin Province); GEOLOGICAL FEATURES OF THE GAOTAIGOU BORON DEPOSIT IN JIAN COUNTY, JILIN PROVINCE AND ITS GENESIS[J]; Jilin Geology;1984-03Yang Xuezeng, (Shenyang Institute of Geology & Mineral Resources); ADISCUSSION ON THE FORMING MECHANISM OF EARLY PROTEROZOIC BANSHIGOU TYPE PHOSPHORITE DEPOSIT IN THE SOUTHERN PART OF JILIN PROVINCE[J]; Jilin Geology;1988-04YIN Chang? Regional Geological Survey of Jilin Province, Changchun 130022, China; 2.Changchun University of Science and Technology, Changchun 130026, China); THE DIVIDE AND CONTRAST OF VOLCANIC EVENTS OF CENOZOIC ERA OF CHANGBAISHAN AREA BETWEEN CHINA AND KOREA[J]; JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY;2000-02CHEN Yue jun 1,2 , PENG Yu jing 2, LU Xiao ping 1,2 , LIU Yue wen 2 (1.