临汾凹陷地层的划分探索
림분요함지층적화분탐색
The Disscussion of Stratigraphic Classification of Concavity in Linfen
  • 万方数据
    山西师范大学学报：自然科学版 산서사범대학학보：자연과학판
    Journal of Shanxi Teachers University
    2011年 4期 88-90 ,共3页

    刘佩%张杏梅%马志正

    류패%장행매%마지정

    凹陷中心%沉积地层%剥蚀面%临汾 凹陷中心%沉積地層%剝蝕麵%臨汾
    요함중심%침적지층%박식면%림분
    the central of depression%sedimentary strata%erosion surface%Linfen
    临汾凹陷沉积复杂,地层归属学术界争议颇多.最近我们在凹陷中心发现一剖面,沉积层位稳定,且有三个明显的剥蚀面,是地层划分重要的标志,对汾河流域地层划分有重要的参考价值.
    림분요함침적복잡,지층귀속학술계쟁의파다.최근아문재요함중심발현일부면,침적층위은정,차유삼개명현적박식면,시지층화분중요적표지,대분하류역지층화분유중요적삼고개치.
    The stratigraphy deposit is complicated in Linfen depression,and there is much controversies over stratigraphic attribution in academic field.Recently,we found a profile in the central of the depression which sedimentary layer is stable,and there are three distinct erosion surface.There is an important reference value about the stratigraphic division of the Fenhe River Basin which is regarded as the important sign of stratigraph.
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