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

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

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: 576
HTML全文浏览量: 15
PDF下载量: 523
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

HTML全文

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.

[1]	付志方, 宫越, 苏玉山, 郭荣涛, 林东升, 汲生珍. 被动陆缘深水海底限制性水道三维地震表征及沉积演化 . 沉积学报, 2024, 42(1): 228-237. doi: 10.14027/j.issn.1000-0550.2022.031
[2]	梁钊, 云玉攀, 魏浩. 快速沉积引发的软沉积物变形构造特征 . 沉积学报, 2023, 41(2): 450-458. doi: 10.14027/j.issn.1000-0550.2021.094
[3]	张风顺, 谭谦, 施泽进, 彭秋, 易驰. 早三叠世鲕粒和巨鲕差异成因及其古环境意义——以川北元坝地区为例 . 沉积学报, 2023, (): -. doi: 10.14027/j.issn.1000-0550.2023.083
[4]	高抒. 南京地区早三叠世碳酸盐沉积动力过程初探 . 沉积学报, 2023, 41(6): 1673-1680. doi: 10.14027/j.issn.1000-0550.2023.124
[5]	. 远源缓坡型薄层细粒浊积岩沉积规律——以松南西斜坡大布苏地区青一段地层为例 . 沉积学报, 2013, 31(2): 291-301.
[6]	. 湖南慈利溪口震旦系陡山沱组震积岩的发现及其地质意义 . 沉积学报, 2012, 30(6): 1032-1041.
[7]	. 四川盆地东南部早三叠世地震事件沉积及其地质意义 . 沉积学报, 2012, 30(3): 477-489.
[8]	曾德勇. 广元上寺剖面下三叠统飞仙关组风暴岩：巨型季风体制下的极端气候事件? . 沉积学报, 2011, 29(3): 440-448.
[9]	傅强. 鄂尔多斯盆地晚三叠世湖盆浊积岩发育特征及地质意义 . 沉积学报, 2008, 26(2): 186-192.
[10]	罗根明. 西秦岭地区晚二叠世—早三叠世沉积相分析和沉积古环境再造 . 沉积学报, 2007, 25(3): 332-342.
[11]	张小莉. 惠民凹陷临邑洼陷岩性油藏控制因素分析 . 沉积学报, 2006, 24(2): 289-293.
[12]	肖传桃, 李维峰, 胡明毅. 江汉盆地早三叠世生态地层学及古地理特征 . 沉积学报, 1997, 15(1): 85-91.
[13]	何海清. 西秦岭早三叠世沉积特征及其构造控制作用 . 沉积学报, 1996, 14(1): 86-92.
[14]	张晓宝, 方国庆, 何海清. 西秦岭上三叠统浊积岩系中波痕的主要特征及其成因探讨 . 沉积学报, 1994, 12(4): 124-131.
[15]	孟庆任, 薛峰, 张国伟. 秦岭商丹带内黑河地区砾岩沉积及其构造意义 . 沉积学报, 1994, 12(3): 37-46.
[16]	赵永胜, 王多义, 胡志水. 四川盆地西缘早三叠世早期碳酸盐重力流沉积与环境 . 沉积学报, 1994, 12(2): 1-9.
[17]	龚一鸣. 新疆北部泥盆系火山碎屑浊积岩层序结构特征及其地质意义 . 沉积学报, 1993, 11(2): 75-83.
[18]	刘金钟, 范德廉. 沉积成岩作用对桂西北中三叠统板纳组中金丰度的影响 . 沉积学报, 1993, 11(2): 51-57.
[19]	左国朝, 张淑玲, 王谐, 金松桥. 北山洗肠井地区寒武系—中奥陶统浊积岩及其火山—沉积组合特征 . 沉积学报, 1987, 5(2): 63-72.
[20]	王一刚. 黔南桂西早三叠世大陆斜坡碳酸盐重力流沉积 . 沉积学报, 1986, 4(2): 91-100.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 576
HTML全文浏览量: 15
PDF下载量: 523
被引次数: 0

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.

全文HTML

参考文献 (1)

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

留言板

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

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

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

出版历程

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