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大同煤田含煤地层中植物化石的垂向分布特征
引用本文:常江林,张春燕.大同煤田含煤地层中植物化石的垂向分布特征[J].中国煤田地质,1999,11(4):6-9.
作者姓名:常江林  张春燕
作者单位:山西煤田地质研究所!太原,030001,山西煤炭地质公司,霍州矿务局地质处
摘    要:以吴家窑剖面为基础,讨论了大同煤田南部晚古生代含煤地层内植物化石的垂向分布特征。认为植物群面貌在小煤与5煤之间发生了重大改变。小峪砂岩之下发育了以Neuropterisouata为代表的早期华夏植物群;其上则出现了许多具二叠纪色彩的植物分子,如Emplectopteristriangulariscladophlebismanchuricus,TaeniopterismultinervisPrecopterisWongiiPtaiyuanensis因此,本区石炭、二叠系界线应置于小峪砂岩之底。

关 键 词:植物化石  垂向分布  晚古生代  大同煤田

Characteristics of Vertical Distribution of Fossil Plants in Coal - bearing Strada of Datong Coalfield
CHANG Jiang-lin.Characteristics of Vertical Distribution of Fossil Plants in Coal - bearing Strada of Datong Coalfield[J].Coal Geology of China,1999,11(4):6-9.
Authors:CHANG Jiang-lin
Abstract:Based on the Wuiayao Section, uertical distribution of fossil plants in late Paleozoic coal - bearing strata of Southem Datong coalfield is discussed. A obviously changes of the flora features have taken place between No. 4 and No. 5 coal seams. Under the Xiaoyu Sandstone the flora is characterized by the presence of the elements of Early Cathaysian Flora, i. e. Neuropteris ovata , etc Above it, the flora is characterized by the barge amount of the elements of Middle Cathasian Flora, i. e. Emplectopteris triangularis , Cladophlebis , Taeniopteris etc. Thus the boundare between Carboniferous and Permian should be placed in the bottom of Xiaoyu sandstone.
Keywords:vertical distribution  fossil plans  Late Paleozoic Era Datong coalfield
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