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    WANG Hai-feng, ZHANG Ting-shan, DAI Chuan-rui, LUO Mei, HU Wen-wen, XIE Xiao'an. Stratigraphic division and correlation of the UpperJurassic-Pliocene in the Dunhua basin[J]. GEOLOGY IN CHINA, 2008, 35(1): 40-53.
    Citation: WANG Hai-feng, ZHANG Ting-shan, DAI Chuan-rui, LUO Mei, HU Wen-wen, XIE Xiao'an. Stratigraphic division and correlation of the UpperJurassic-Pliocene in the Dunhua basin[J]. GEOLOGY IN CHINA, 2008, 35(1): 40-53.

    Stratigraphic division and correlation of the UpperJurassic-Pliocene in the Dunhua basin

    • Abstract:The authors used the field data, seismic data, coal field drilling data and paleontological data to compile and analyze the representative stratigraphic division schemes for the Dunhua basin-coal prospect area at peripheries of the Songliao basin, and got the following understandings: (1) the age of the Huichun Formation is Eocene-Oligocene;(2) the Upper Cretaceous Longjing Formation may not exist in the basin; (3) the upper member and lower member of the so-called Mao'ershan Formation should be assigned to the Quanshuicun Formation and Changcai Formation;(4) the Dalazi, Quanshuicun, Changcai and Tuntianying formations do exist in the basin, of which the Dalazi Formation and Changcai Formation might be Early Cretaceous Aptian-Albian and Berriasian-Aptian in age respectively according to the lithostratigraphic and biostratigraphic correlation between the Dunhua basin and its neighboring basins;(5) the wrong uses of some local formation names at several sites of the basin are revised; and (6) a stratigraphic sequence is established in the Dunhua basin, which may be used for reference at present.
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