| 山东新泰盘车沟地区崮山组和长山组风暴沉积特征 |
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| 引用本文： | 田海芹,马玉新,狄明信. 山东新泰盘车沟地区崮山组和长山组风暴沉积特征[J]. 中国石油大学学报(自然科学版), 1994, 0(6) |
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| 作者姓名： | 田海芹 马玉新 狄明信 |
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| 作者单位： | 石油大学勘探系 |
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| 摘 要： | 通过对山东新泰盆车沟地区崮山组和长山组的宏观、微观岩石学特征及沉积层序的研究。识别出崮山组至少有１３套由竹叶石灰岩、颗粒石灰岩、含颗粒石灰岩及泥晶石灰岩所组成的沉积层序及大型丘状交错层理，同样也发现了长山组中的数套不同类型的竹叶石灰岩层序，崮山组的竹叶石灰岩为远源深水风暴流的产物；而长山组的竹叶石灰岩及有关台石则为近源风暴流沉积，在上述研究的基础上．分别建立了本区晚寒武世远源和近源风暴沉积层序，进而总结归纳出风暴沉积综合模式。
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| 关 键 词： | 砾屑；石灰岩；风暴；沉积；模式；层序 |
STORR DEPOSIIS OF GUSHAN AND CHANGSHAN FORMATIONSAT PANCHEGOU REGION OF XINTAIIN SHANDONG PROVINCE |
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| Tian Haiqin, Ma Yuxin, Di Mingxin. STORR DEPOSIIS OF GUSHAN AND CHANGSHAN FORMATIONSAT PANCHEGOU REGION OF XINTAIIN SHANDONG PROVINCE[J]. Journal of China University of Petroleum (Edition of Natural Sciences), 1994, 0(6) |
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| Authors: | Tian Haiqin Ma Yuxin Di Mingxin |
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| Abstract: | This paper studies the macrolithology, micropetrological character istics andthe sedimentary sequences of the Gushan and Changshan formations at Panchegou area ofXintai in Shandong Province. In Gushan formation,at least thirteen sedimentary sequencescomposed of wormkalks or rudstones,grainstones,packstones,wackestones and mudston es orshales are recognized.In these sequences,the large scale hammock cross bedding are found.While,several similar sequences mainly composed of the rudstones are also identified.Theresearch comparison showed that wormkalk sequences of Gushan formation are caused ofdeeper water storm deposits of far resources. The rudstone sequences of the Changshanformation are formed by the storm production of near resources.A far and a near resourcestorm sedimentary sequences of the upper cambain (carbonate)rocks in this region arerespectively established according to the studies above.and a complex storm sedimentarymodel is also presented. |
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| Keywords: | Rudaceousintraclast:Limestone:Storm:Sedimention Models:Sequence |
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