| 辽南晚前寒武纪地层层序问题的研讨 |
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| 引用本文： | 张丕孚.辽南晚前寒武纪地层层序问题的研讨[J].地层学杂志,1994,18(3):228-231. |
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| 作者姓名： | 张丕孚 |
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| 作者单位： | 地科院沈阳地矿所 |
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| 摘 要： | 辽南晚前寒武纪地层层序问题的研讨张丕孚（地科院沈阳地矿所,辽宁沈阳,１１００３２）关键词地层层序,叠接,标志层,晚前寒武纪,辽南地区长期沿用的辽南晚前寒武纪地层层序为永宁群（松树组、朵子山组、庙山组）、细河群（钓鱼台组、南芬组、桥头组）、五行山群（长...
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| 关 键 词： | 地层层序 叠接 标志层 晚前寒武纪 辽南地区 |
A discussion on the Late Precambrian stratigraphic sequences of Southern Liaoning |
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| Zhang Pifu.A discussion on the Late Precambrian stratigraphic sequences of Southern Liaoning[J].Journal of Stratigraphy,1994,18(3):228-231. |
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| Authors: | Zhang Pifu |
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| Abstract: | Many practical materials revealed that the so-called Yongning, Xihe and Wuxingshan Groups of the Dalian-Jinzhou area are completely different from those of the Fuzhou area in their fossil centent, metamorphism, tectonic pattern and isotopic ages. Stratigraphically they are not equivalent and the Changlingzi Formation is not an index horizon.The "Ganjingzi Formation" (i.e. Jinjia Formation) at the Wuxingshan of the Jinzhou district is a series of dolomites(not dolomitic limestones) of lagoon factes,containing stromatolites Baicalia and Juyushania. And the Yingchengzi and Shisanlitai Formations, lithologically, are a series of limestones of shallow sea facies,bearing stromatolites Baicalia cf. baicalica, Conophyton ocularoides, Anabaria, Chihsienella and Kussiella. This proved that the "Ganjingzi Formation". (i.e. Jinjia Formation) of Wuxingshan does not include the Yingchengzi Formation of the Jinxian Group and Shisanlitai Formation. There is no evidence to prove that the Majiatun Formation is disconformably covered by the Dalinzi Formation in the Zhaojiakanzi section of Fuzhouwan. The contact relation between them is conformble without any hiatus of upper Jinxian Group in the section. In the east of Henan Village of Fuzhouwan, we saw that the Jinjia Formation (i.e. so-called "Ganjingzi Formation")conformably overlies the Dalinzi Formation-Yingchengzi Formation, and the lower part of the Dingjiagou Formation, i.e. so-called "Nanguanling Formation", to be the middle-upper parts of the Dingjiagou Formation. Hence there are no Yingchengzi, Shisanlitai and Majiatun Formation of the Jinxian Group in the Zhaojiakanzi section.If we put the present fossils and isotopic ages in the long-term used Late Precambrian stratigraphic sequence of Southern Liaoning, the basic contradictions of them with the sequence appeared in the overlapped part of the stratigraphic column.The overlapping of the column made some mistakes in the sequence. |
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| Keywords: | stratigraphic sequence overlapping index horizon Late Precambrian Southern Liaoning |
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