中国东部早第三纪海侵与全球海平面升降
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RELATIONSHlP BETWEEN EUSTASY AND TRANSGRESSIoN IN EARLY TERTIARY IN EASTERN CHINA
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    摘要:

    中国西北晚上新世一第四纪咸化湖泊沉积中发现了有孔虫、钙质超微化石, 它们作为海侵证据的可靠程度有待商榷。《中国油气区第三系对比表》的发表, 对旧地层年代值作了重要修改,中国大陆东部早第三纪湖盆的湖平面与全球海 平面升降变化不相对应,因此,根据旧的地层年代值所作的湖平面与全球海平 面升降相吻合而得出的海侵结论缺乏可靠的年代地层学的基础。

    Abstract:

    Foraminifera and calcareous nannofossils have been found in late Pliocene to Quaternary salt lake sediments in northwestern China.Evidence of transgression is suspicious。In the newly pub— lished table“The stratigraphic Correlation of the Tertiary in Petroliferous Areas of China” (1991),great revisions have been made of the age values of strata.The authors conclude that the early Tertiary lake level change in the eastern part of the mainland of China does not corre— spond with the eustasy at that time.The conclusion of the transgression drawn ftom the view that the lake level change coincides with eustasy according to the oldage values of strata,lacks the reliable chronostratigraphical foundation.

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孙镇城,彭立才,李东明,王敏.1996.中国东部早第三纪海侵与全球海平面升降[J].地质论评,42(sup):180-187,[DOI].
Sun zhencheng, pen licai, li congming, wang min.1996. RELATIONSHlP BETWEEN EUSTASY AND TRANSGRESSIoN IN EARLY TERTIARY IN EASTERN CHINA[J]. Geological Review,42(sup):180-187.

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