闽西南地区早三叠世溪口组浊流沉积

李培军; 侯泉林; 李继亮; 孙枢

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闽西南地区早三叠世溪口组浊流沉积

李培军, 侯泉林, 李继亮, 孙枢

文章导航 > 沉积学报 > 1997 > 15(4): 50-57

李培军, 侯泉林, 李继亮, 孙枢. 闽西南地区早三叠世溪口组浊流沉积[J]. 沉积学报, 1997, 15(4): 50-57.

引用本文:

李培军, 侯泉林, 李继亮, 孙枢. 闽西南地区早三叠世溪口组浊流沉积[J]. 沉积学报, 1997, 15(4): 50-57.

Li Peijun, Hou Quanlin, Li Jiliang, Sun Shu. urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China[J]. Acta Sedimentologica Sinica, 1997, 15(4): 50-57.

Citation:

Li Peijun, Hou Quanlin, Li Jiliang, Sun Shu. urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China[J]. Acta Sedimentologica Sinica, 1997, 15(4): 50-57.

李培军, 侯泉林, 李继亮, 孙枢. 闽西南地区早三叠世溪口组浊流沉积[J]. 沉积学报, 1997, 15(4): 50-57.

引用本文:

李培军, 侯泉林, 李继亮, 孙枢. 闽西南地区早三叠世溪口组浊流沉积[J]. 沉积学报, 1997, 15(4): 50-57.

Li Peijun, Hou Quanlin, Li Jiliang, Sun Shu. urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China[J]. Acta Sedimentologica Sinica, 1997, 15(4): 50-57.

Citation:

Li Peijun, Hou Quanlin, Li Jiliang, Sun Shu. urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China[J]. Acta Sedimentologica Sinica, 1997, 15(4): 50-57.

闽西南地区早三叠世溪口组浊流沉积

1 北京大学遥感与地理信息系统研究所,北京 100871;
2 中国科学院地质研究所,北京 100029

基金项目: 国家自然科学基金，中国科学院资助重大项目

详细信息

作者简介:
李培军男 30岁博士后沉积大地构造

中图分类号: P512.2

计量

文章访问数: 541
HTML全文浏览量: 8
PDF下载量: 521
被引次数: 0

urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China

1Institute of Remote Sensing and Geographic Information System,Peking University,Beijing,100871,China;
2 Institute of Geology,Chinese Academy of Sciences,Beijing,Beijing,100029,China

摘要

摘要: 闽西南地区的早三叠世溪口组主要由深水浊流沉积组成，可以识别出５个相类型：砾岩相、砂岩相、砂岩－泥岩相、粉砂岩－泥岩相、具粒序的粉砂质泥岩相。它们可组成５个相组合，分别形成于浊积扇的上扇、中扇和下扇环境。相组合的空间展布、古水流以及遗迹化石的分布均一致表明，当时的大陆坡倾向南东。砂岩的地球化学成分反映其构造背景为被动大陆边缘.
- 浊积岩 /
- 早三叠世 /
- 溪口组 /
- 被动陆缘
Abstract: The sedimentological research on the Lower Triassic Xikou Formation in southwestern Fujiandemonstrated that the rocks are mainly composed of deep-water turbidites, in which 5 facies and 7 sub-facies are recognized on the basis of lithology, textures and structures of the rocks,i.e.(1) conglomeratefacies;(2) sandstone facies;(3) sandstone-mudstone facies;(4) siltstone-mudstone facies;(5) graded siltymudstone facies.These facies consist of 5 facies associations that are formed in upper-fan, mid-fan andlower-fan environments, respectively.According to the characteristics of the turbidites, the turbiditefan in the study area is inferred to an elongate fan which is mainly formed in a stable tectonic setting,such as passive continental margin.Trace fossils contained in the rocks, such as Pasichnia, Grazing traces and some horizontal traces,indicated that they once lived in a bathyal-abyssal environment.The paleocurrent directions derivedfrom the sole marks and cross-beddings are toward to southeast after rotation correction.The spatialdistribution of the facies associations, paleocurrent data and distribution of the trace fossils all suggestedthat the continental slope was once dipped toward to the southeast at that time.The tectonic setting of the sedimentary basin was interpreted as passive continental margin based onthe geochemical composition analysis of the sandstone
- turbidite /
- Xikou Formation /
- Early Triassic /
- passive continental margin

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参考文献(1)

[1]

(1) 福建省地矿局.福建省区域地质志.北京: 地质出版社, 1985.

(2) 吴歧,郑云钦.福建下三叠统溪口组浊积岩的发现及其意义.岩相古地理, 1990, (6): 1～7.

(3)Li Peijun, Hou Quanlin, Li Jiliang and Sun Shu.Contouritesin the Lower Triassic Xikou Formation in southwestern Fu-jian, China.In: China' s Postdoctors'Contributions to the30th International Geological Cong ress.Beijing, 1996, 1～10.

(4) 李培军,侯泉林,李继亮,孙枢.闽西南地区早三叠世溪口组中的孤立滑塌岩块及其地质意义.科学通报, 1996, 41(21).

(5) Mutti E and Ricci Lucchi F.Turbidite of the northern Apen-nines: introduction to facies analysis (English translation by TH Nilsen, 1978).International Geology Review, 1972, 20 2): 125～166.

(6)Pikering K T, Stow D, Watson M and Hiscott R.Deep - waterfacies, process and models: a review and classification schemefo r modern and ancient sediments.Earth - Science Review,1986, 23: 75～174.

(7)Bouma A H.Sedimentology of some flysch deposits: a raphicapproach to Facies interpretation, Elsevies.Amsetrdam,1962.

(8) Lowe D R.Sediment gravity flow Ⅱ: Depositional modelswith special reference to the deposits of high-density turbiditycurrents.J.sedim.Petrol., 1982, 52: 279～297.

(9) Ineson J R.Coarse-grained submarine fan and slope aporn de-posits in a Cretaceous back-arc baisn, Antarctica.Sedimentol-og y, 1989, 36: 793～819.

(10) Stow D A V, D G Howell and C H Nelson.Sedimentary,tectonic and sea-level controls.In: A H Bouma, W R Normakand N R Barnes(eds.), Submarine fans and related deposition-al systems.Springer-Verlag, 1985, 15～23.

(11)Mutti E, Distinctive thin - bedded turbidite facies and relateddepositional environments in the Eocene Hecho Group (South- central Pyrenees, Spain).Sedimentology, 1977, 24: 107～131.

(12) Ekdale A A, Bromly C G, Pemberton S G.Ichnology.Soci-ety of Economic Paleontologists and Mineralogists, Tulsa,Oklahoma, 1984, 232～255.

(13) Frey R W and A Seilacher.Uniformity in marine inv erbrateichnology.Lethhaia, 1980, 13: 183～207.

(14) Dobson J.Paleomagnetism of the Huanan and Yangtzeblocks, SE China, Ph D Thesis, 1990, 150.

(15)Floyd P A, Shail R, Leveridge B Eand Franke W.Geochem-istry and provenance of Rhenohercynian synorg enic sand-stones: implications fo r tectonic environment dicrmination.In: Development in sedimentary provenance studies (Ed.byMorton A C, Todd S P and Haughton P D W).Geological So-cietty Special Publication, 1991, (57): 173～188.

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闽西南地区早三叠世溪口组浊流沉积

1 北京大学遥感与地理信息系统研究所,北京 100871;

2 中国科学院地质研究所,北京 100029

基金项目: 国家自然科学基金，中国科学院资助重大项目

作者简介:
李培军男 30岁博士后沉积大地构造

收稿日期: 1996-09-24
刊出日期: 1997-12-10

中图分类号: P512.2

关键词:

浊积岩 /

早三叠世 /

溪口组 /

被动陆缘

摘要: 闽西南地区的早三叠世溪口组主要由深水浊流沉积组成，可以识别出５个相类型：砾岩相、砂岩相、砂岩－泥岩相、粉砂岩－泥岩相、具粒序的粉砂质泥岩相。它们可组成５个相组合，分别形成于浊积扇的上扇、中扇和下扇环境。相组合的空间展布、古水流以及遗迹化石的分布均一致表明，当时的大陆坡倾向南东。砂岩的地球化学成分反映其构造背景为被动大陆边缘.

English Abstract

urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China

1Institute of Remote Sensing and Geographic Information System,Peking University,Beijing,100871,China;

2 Institute of Geology,Chinese Academy of Sciences,Beijing,Beijing,100029,China

Received Date: 1996-09-24
Publish Date: 1997-12-10

Keywords:

Abstract: The sedimentological research on the Lower Triassic Xikou Formation in southwestern Fujiandemonstrated that the rocks are mainly composed of deep-water turbidites, in which 5 facies and 7 sub-facies are recognized on the basis of lithology, textures and structures of the rocks,i.e.(1) conglomeratefacies;(2) sandstone facies;(3) sandstone-mudstone facies;(4) siltstone-mudstone facies;(5) graded siltymudstone facies.These facies consist of 5 facies associations that are formed in upper-fan, mid-fan andlower-fan environments, respectively.According to the characteristics of the turbidites, the turbiditefan in the study area is inferred to an elongate fan which is mainly formed in a stable tectonic setting,such as passive continental margin.Trace fossils contained in the rocks, such as Pasichnia, Grazing traces and some horizontal traces,indicated that they once lived in a bathyal-abyssal environment.The paleocurrent directions derivedfrom the sole marks and cross-beddings are toward to southeast after rotation correction.The spatialdistribution of the facies associations, paleocurrent data and distribution of the trace fossils all suggestedthat the continental slope was once dipped toward to the southeast at that time.The tectonic setting of the sedimentary basin was interpreted as passive continental margin based onthe geochemical composition analysis of the sandstone

李培军, 侯泉林, 李继亮, 孙枢. 闽西南地区早三叠世溪口组浊流沉积[J]. 沉积学报, 1997, 15(4): 50-57.

引用本文:

李培军, 侯泉林, 李继亮, 孙枢. 闽西南地区早三叠世溪口组浊流沉积[J]. 沉积学报, 1997, 15(4): 50-57.

Li Peijun, Hou Quanlin, Li Jiliang, Sun Shu. urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China[J]. Acta Sedimentologica Sinica, 1997, 15(4): 50-57.

Citation:

Li Peijun, Hou Quanlin, Li Jiliang, Sun Shu. urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China[J]. Acta Sedimentologica Sinica, 1997, 15(4): 50-57.

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闽西南地区早三叠世溪口组浊流沉积

作者简介:
李培军男 30岁博士后沉积大地构造

计量

urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China

计量

目录

闽西南地区早三叠世溪口组浊流沉积

1 北京大学遥感与地理信息系统研究所,北京 100871;

2 中国科学院地质研究所,北京 100029

作者简介:
李培军男 30岁博士后沉积大地构造

English Abstract

urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China

1Institute of Remote Sensing and Geographic Information System,Peking University,Beijing,100871,China;

2 Institute of Geology,Chinese Academy of Sciences,Beijing,Beijing,100029,China

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闽西南地区早三叠世溪口组浊流沉积

作者简介: 李培军 男 30岁 博士后 沉积大地构造

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urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China

计量

出版历程

目录

闽西南地区早三叠世溪口组浊流沉积

1 北京大学遥感与地理信息系统研究所,北京 100871; 2 中国科学院地质研究所,北京 100029

作者简介: 李培军 男 30岁 博士后 沉积大地构造

English Abstract

urbidites in the Lower Triassic Xikou Formation in Southwestern Fujian, South China

1Institute of Remote Sensing and Geographic Information System,Peking University,Beijing,100871,China; 2 Institute of Geology,Chinese Academy of Sciences,Beijing,Beijing,100029,China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
李培军男 30岁博士后沉积大地构造

1 北京大学遥感与地理信息系统研究所,北京 100871;

2 中国科学院地质研究所,北京 100029

作者简介:
李培军男 30岁博士后沉积大地构造

1Institute of Remote Sensing and Geographic Information System,Peking University,Beijing,100871,China;

2 Institute of Geology,Chinese Academy of Sciences,Beijing,Beijing,100029,China