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    How geological work is oriented to economic construction during the period of economic restructuring
    2004, 23(9): 827-828.
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    Mr. Li Chunyu and China''''s geological cause
    2004, 23(9): 829-838.
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    Thoughts on several problems about the information technology(IT) application to geological work
    2004, 23(9): 839-845.
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    Mianlue paleo-suture on the southern margin of the Central Orogenic System in Qinling-Dabie with a discussion of the assembly of the main part of the continent of China
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    2004, 23(9): 846-853.
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    Major tectonic event in the Yanshanian intraplate deformation belt in the jurassic
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    2004, 23(9): 854-863.
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    Mesozoic tectonic framework and evolution in the central segment of the intraplate Yanshan orogenic belt
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    2004, 23(9): 864-875.
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    Geological features and tectonic evolution of Meso-Cenozoic basins in southeastern China
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    2004, 23(9): 876-884.
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    Nature of the Yanbian suture zone and structure of Northeast Asia
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    2004, 23(9): 885-891.
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    Recognition of Neoproterozoic ophiolite on the northern margin of the Qaidam basin: evidence of the breakup of Rodinia?
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    2004, 23(9): 892-898.
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    Advances in the study of the Paleogene magnetostratigraphy on the northwestern margin of the Qaidam basin
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    2004, 23(9): 899-902.
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    Carboniferous Tianshan igneous megaprovince and mantle plume
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    2004, 23(9): 903-910.
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    From the back-arc basin to foreland basin-Ordovician Devonian sedimentary basin and tectonic evolution in the North Qilian orogenic belt
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    2004, 23(9): 911-917.
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    Early Paleozoic plate-tectonic evolution and deep continental subduction on the northern margin of the Qinghai-Tibet Plateau
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    2004, 23(9): 918-925.
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    Multi-stage strike-slip motion and uplift along the Altyn Tagh fault since the Late Cretaceous
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    2004, 23(9): 926-932.
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    Charm of landing of plate tectonics on the continent as viewed from the study of the archipelagic arc-basin system
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    2004, 23(9): 933-939.
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    Paying attention to the 3 Dimensional crossing structure of the lithosphere-Exposed continental lithospheric decoupling surface
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    2004, 23(9): 940-946.
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    Basic characteristics of accretion-type orogens
    2004, 23(9): 947-951.
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    Comparison of the Pan-Cathaysian orogeny with the Caledonian and Pan-African orogenies
    2004, 23(9): 952-958.
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    Diversity of adakite
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    2004, 23(9): 959-965.
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    Rotation of the Jurassic crust and transformation of the lithosphere of eastern China
    2004, 23(9): 966-972.
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    Transformation of the tectonic regime is a lithospheric-scale activity
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    2004, 23(9): 973-979.
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    Microstructures of deformed rocks and rheology of the lithosphere
    2004, 23(9): 980-985.
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    Structure Characteristics of crustal "mosaicking and superimposition" of the continental crust of China and its evolution
    2004, 23(9): 986-1004.
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    Discovery of Late Jurassic Mamenchisaurus in Yunnan, southwestern China
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    2004, 23(9): 1005-1011.
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    Environmental evolution in the Yellow River source area in the past 1000 years
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    2004, 23(9): 1012-1017.
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    New progress in the study of Paleozoic strata in the Xainza area, Tibet
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    2004, 23(9): 1018-1022.
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    Zonality of the Gangdise magmatic arc on the Qinghai-Tibet Plateau and its geological significance
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    2004, 23(9): 1023-1032.
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    Discovery of the Jaggang Snow Mountain tungsten-molybdenum-copper-gold polymetallic occurrence in the northern part of the Gangdise block, Tibet
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    2004, 23(9): 1033-1039.
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    Characteristics of the Laorite Co granite porphyry in central Qiangtang, northern Tibet and its tectonic significance
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    2004, 23(9): 1040-1045.
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    Characteristics of structural-stratabound gold deposits and genetic model in the Ningzhen Area, Jiangsu
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    2004, 23(9): 1046-1049.
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    Stratigraphic division and correlation 0f Qingbaikouan strata in south-central Jiangxi
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    2004, 23(9): 1050-1054.
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