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THE ANALYSIS METHODOLOGY OF POLLEN FROM THE MESOZOIC—CENOZOIC RED BEDS IN NORTHERN TIBET
引用本文:WT,”BZ]Wei Mingjian ,Wan Xiaoqiao ,Wang Chengshan ,Yin Haisheng .THE ANALYSIS METHODOLOGY OF POLLEN FROM THE MESOZOIC—CENOZOIC RED BEDS IN NORTHERN TIBET[J].地学前缘,2000(Z1).
作者姓名:WT  ”BZ]Wei Mingjian  Wan Xiaoqiao  Wang Chengshan  Yin Haisheng
作者单位:1.Capital Normal University,Beijing 100037,China;2.China University of Geosciences,Beijing 100083,China;3.Chengdu Institute of Technology,Chengdu 610059,China
基金项目:theNational (G19980 40 80 0 5 .3)andtheProject (49872 0 0 3)supportedbyNNSFC
摘    要:THE ANALYSIS METHODOLOGY OF POLLEN FROM THE MESOZOIC—CENOZOIC RED BEDS IN NORTHERN TIBETtheNational (G19980 40 80 0 5 .3)andtheProject (49872 0 0 3)supportedbyNNSFC


The Analysis Methodology of Pollen From the Mesozoic-Cenozoic Red Beds in Northern Tibet
Wei Mingjian,et al.The Analysis Methodology of Pollen From the Mesozoic-Cenozoic Red Beds in Northern Tibet[J].Earth Science Frontiers,2000(Z1).
Authors:Wei Mingjian  
Abstract:A group of red interbedded sandstone, siltstone and clay\|stone occur in the inland of northern Tibet. During the last 50 years, a lot of researches have been done at this group of beds along the Qinghai\|Xizang highway in the Kekexili area.. According to the lithological characters, the strata have been divided into tow parts, the lower part named as the Feng huoshan group, and the upper part the Yaxicuo group. It is obscure to the age of the strata. For example, Yi jixiang et al. (1990) put them in early Pliocene in the light of the microfossils which they found at the foot of Feng huoshan mountain. The fossils include (1) Charophyta: Rhabdochara? sp ., Peckichara subsphecrica?, Cyrogoniae; (2) Ostracoda: Cypris sp .; (3) Gastropod: Sinoplanorbis sp ., Amnicola sp ., Bithynia sp .; and (4) Sporopollen: Tricoporopollenites nactonodus ?, Polypodiceoisporites, Cyathidites, Schizosporis, Pediastrum. Based on different species of Charophyta, Ostracoda, Gastropod, Bivalve, Sporopollen, Zhang Yifu et al. (1994) refer the strata to Cretaceous. The lower abundance of the fossils from previous research gave lower precision of fossil identification. Thus, the age of the strata was confusion.
Keywords:inland of Tibet  Cenozoic  red beds  Pollen analysis  method ology
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