About 12 item dissertation in line with dating by isotope query results,the following is 1 to 50(Search took 0.041 seconds)

  1. Geological-geochemical Characteristics of Caledonian Granitoids and Its Geological Significance Hunan Province,WangGao/Central South University,0/29
  2. Geochoronology, Geochemistry and Origin of Carboniferous-permian Alkali Granites Ineastern Tianshan, Hami, NW China,HuangWei/Chinese Geology University (Beijing),0/3
  3. The Geological-geochemical Characteristics and Genesis of Xinsheng Copper Polymetallic Deposit in Hunan Province,FeiLiDong/Central South University,0/60
  4. Atom Trap Trace Analysis for Rare Gas Atomic Isotopes,ChengCunFeng/University of Science and Technology of China,0/88
  5. The Preliminary Discussion on the Era of Neoproterozoic Glaciations in Quruqtagh and the Precambrian Crustal Evolution of the Tarim Craton,HeJingWen/Nanjing University,0/103
  6. The Tectono-magma Events in the Western Margin of the Eastern Himalayan Syntaxis and Their Geodynamic Implications,GuoLiang/China University of Geosciences,0/259
  7. Compositions, Characteristics, Chronological Framework and Origin of Early-Precambrian Metamorphic Basement in Western Alxa Block,GongJiangHua/Chinese Academy of Geological Sciences,0/91
  8. Study on LUCC and Soil Erosion of Small Catchment in Karst Area,WangWenBo/Beijing University,0/878
  9. Petrogrnesis of Granites and Their Relation to Tectonic Evolution of Orogen in the East Part of Qinling Orogenic Belt,LeiMin/Chinese Academy of Geological Sciences,5/346
  10. Chronology, Petrogenesis and Tectonic Implications of the Cumulate Gabbro in Tahe Area, Northern Great Xing’an Range,ZhouChangYong/Jilin University,0/261
  11. The Geochronology, Geochemical Characteristics and Tectonic Implication of the Xiaomaoling Composite Intrusives in Zhashui, Shaanxi,LiuRenYan/Chinese Academy of Geological Sciences,0/72
  12. Petrographic and Zircon Geochronological Studies of the Taihua Group on the Southern Margin of the North China Craton,MaZuo/Nanjing University,0/106

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