地质调查与研究
地質調查與研究
지질조사여연구
Geological Survey and Research
2015年
3期
161-170
,共10页
雾迷山组%疑源类%燕山地区
霧迷山組%疑源類%燕山地區
무미산조%의원류%연산지구
Wumishan Formation%Acritarches%Yanshan range
本文通过系统采样,利用化学浸泡法,对冀北坳陷凌源地区和宣龙坳陷北京延庆地区的雾迷山组疑源类进行了研究,并划分出四个化石组合,自下而上分别为:罗庄组合(Asperatopsophosphaera umishanensis-Oscillatori-opsis luozhuangensis)、磨盘峪组合(Stictosphaeridium pectinale-Micrhystridium pallidum)、二十里堡组合(Pale-amorpha punctulata-Orygmatosphaeridium rubignosum)和闪坡岭组合(Microconcentrica cymata-Baltisphaeridium cerinum).通过两个地区疑源类组合特征的对比,认为凌源地区和延庆地区雾迷山组微疑源类化石组合及特征具有可对比性.
本文通過繫統採樣,利用化學浸泡法,對冀北坳陷凌源地區和宣龍坳陷北京延慶地區的霧迷山組疑源類進行瞭研究,併劃分齣四箇化石組閤,自下而上分彆為:囉莊組閤(Asperatopsophosphaera umishanensis-Oscillatori-opsis luozhuangensis)、磨盤峪組閤(Stictosphaeridium pectinale-Micrhystridium pallidum)、二十裏堡組閤(Pale-amorpha punctulata-Orygmatosphaeridium rubignosum)和閃坡嶺組閤(Microconcentrica cymata-Baltisphaeridium cerinum).通過兩箇地區疑源類組閤特徵的對比,認為凌源地區和延慶地區霧迷山組微疑源類化石組閤及特徵具有可對比性.
본문통과계통채양,이용화학침포법,대기북요함릉원지구화선룡요함북경연경지구적무미산조의원류진행료연구,병화분출사개화석조합,자하이상분별위:라장조합(Asperatopsophosphaera umishanensis-Oscillatori-opsis luozhuangensis)、마반욕조합(Stictosphaeridium pectinale-Micrhystridium pallidum)、이십리보조합(Pale-amorpha punctulata-Orygmatosphaeridium rubignosum)화섬파령조합(Microconcentrica cymata-Baltisphaeridium cerinum).통과량개지구의원류조합특정적대비,인위릉원지구화연경지구무미산조미의원류화석조합급특정구유가대비성.
On the basis of systematic sampling and chemical soaking treatment,a large amount of acritarches were found from the Wumishan Formaton of the middle Jixian system of the early Mesoproterozoic in Lingyuan area of eastern Yanshan range and Yanqing area of western Yanshan rang.They could be distinctly subdivided in-to following four assemblages preliminarily,namely the Luozhuang assemblage(Asperatopsophosphaera umisha-nensis—Oscillatoriopsis luozhuangensis),the Mopanyu assemblage(Stictosphaeridium pectinale—Micrhystridi-um pallidum),the Ershilipu assemblage(Paleamorpha punctulata—Orygmatosphaeridium rubignosum)and the Shanpoling assemblage(Microconcentrica cymata—Baltisphaeridium cerinum)in ascending order.Comparative study indicates acritarch assemblages possess considerable comparability and the potential of stratgraphic corre-lation.