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WANG QIANG,LI FENGLIN,LI YUDE,GAO XIULIN. 1987. DISCUSSION ON THE NAMING OF QUATERNARY TRANSGRESSIONS IN WEST-SOUTHERN COAST PLAIN OF BOHAI SEA. Acta Oceanologica Sinica, (1):104-115
DISCUSSION ON THE NAMING OF QUATERNARY TRANSGRESSIONS IN WEST-SOUTHERN COAST PLAIN OF BOHAI SEA
DISCUSSION ON THE NAMING OF QUATERNARY TRANSGRESSIONS IN WEST-SOUTHERN COAST PLAIN OF BOHAI SEA
Received:July 28, 1985  Revised:May 30, 1986
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Author NameAffiliation
WANG QIANG Tianjin Institute of Geology and Mineral Resources, Tianjin 
LI FENGLIN Tianjin Institute of Geology and Mineral Resources, Tianjin 
LI YUDE Geology and Mineral Resources Bureau, Shandong Province, Dezhou 
GAO XIULIN Department of Geography, Tianjin Teachers University, Tianjin 
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Abstract:
      Based on micropalaeontological information of over 150 drill holes, this paper discusses the problem on the naming of Quaternary transgressions in the west-southern coast plain of Bohai Sea.We consider that palaeotide and sedimentation have a great influence on the distribution of micropalaeontological fossils.In view of the present technical level, it is necessary for transgression sequence to be established under the following conditions:full evidence of fossils; clear climate; and stable sedimentary beds.In establishing a transgression, its contents of time and phase concept must be proposed, and its biofacies, sedimentary facies and palaeoclimatology must be analysed synthetically.
中文摘要:
      Based on micropalaeontological information of over 150 drill holes, this paper discusses the problem on the naming of Quaternary transgressions in the west-southern coast plain of Bohai Sea.We consider that palaeotide and sedimentation have a great influence on the distribution of micropalaeontological fossils.In view of the present technical level, it is necessary for transgression sequence to be established under the following conditions:full evidence of fossils; clear climate; and stable sedimentary beds.In establishing a transgression, its contents of time and phase concept must be proposed, and its biofacies, sedimentary facies and palaeoclimatology must be analysed synthetically.
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