SEQUENCE-STRATIGRAPHIC SUCCESSION AND SEDIMENTARY-BASIN EVOLUTION FROM LATE PALEOZOIC TO TRIASSIC IN THE YUNNAN-GUIZHOU-GUANGXI REGION

• Engineering Geology and Environmental Geology • Previous Articles Next Articles

MEI Ming-xiang, LI Zhong-yuan

Research Institute of Exploration and Production, SINOPEC, Beijing 100083, China

Received:2004-07-05 Revised:2004-09-23 Online:2004-04-20 Published:2004-04-20

[1]	SHI Guo, TIAN Jing-Chun, ZHANG Xiang, LI Rong, YU Mei-Yi. The Sedimentary Characteristics, Evolution and Controlling Factors of Southern Margin, Yangtze Carbonate Platform During the Hercynian-Indosinian Stage [J]. Geoscience, 2009, 23(6): 1113-1120.
[2]	MEI Mian-Xiang. Implication for the Unusual Giant Oolites of the Phanerozoic and Their Morphological Diversity: A Case Study from the Triassic Daye Formation at the Lichuan Section in Hubei Province, South China [J]. Geoscience, 2008, 22(5): 683-698.
[3]	MEI Ming-xiang. New Interpretation of Spheroidal Molar-Tooth Structures from Mesoproterozoic Gaoyuzhuang Formation at the Jixian Section in Tianjin: Possibly Cellular Microstructure of the Spheroidal or the Sub-spheroidal Three-Dimensional Fossils of Megascopic Algae before 1400 Ma [J]. Geoscience, 2007, 21(4): 738-748.
[4]	YU Tao，ZHOU Zhi-guang，LIU Chang-feng，LIANG Ding-yi. Metamorphic Structural Sequence of Carboniferous and Its Underlying Strata in Kangmar Region of Southern Tibet [J]. Geoscience, 2007, 21(3): 491-497.

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