甘肃龙首山新元古代烧火筒群沉积特征及其构造意义

李文渊; 杨鹏飞

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甘肃龙首山新元古代烧火筒群沉积特征及其构造意义

李文渊, 杨鹏飞

文章导航 > 沉积学报 > 2004 > 22(1): 142-147

李文渊, 杨鹏飞. 甘肃龙首山新元古代烧火筒群沉积特征及其构造意义[J]. 沉积学报, 2004, 22(1): 142-147.

引用本文:

李文渊, 杨鹏飞. 甘肃龙首山新元古代烧火筒群沉积特征及其构造意义[J]. 沉积学报, 2004, 22(1): 142-147.

LI Wen yuan, YANG Peng fei. Late Neoproterozoic Sedimentations of the Carbonate -Detrital Flows in Longshou Mountains, Northwest China: Implications for Its Tectonic Environments[J]. Acta Sedimentologica Sinica, 2004, 22(1): 142-147.

Citation:

李文渊, 杨鹏飞. 甘肃龙首山新元古代烧火筒群沉积特征及其构造意义[J]. 沉积学报, 2004, 22(1): 142-147.

引用本文:

李文渊, 杨鹏飞. 甘肃龙首山新元古代烧火筒群沉积特征及其构造意义[J]. 沉积学报, 2004, 22(1): 142-147.

Citation:

甘肃龙首山新元古代烧火筒群沉积特征及其构造意义

李文渊^1,2,
杨鹏飞²

1.
西安地质矿产研究所西安 710054;
2.
西北大学地质学系西安 710054

基金项目: 中国地质调查局地质调查项目资助

详细信息

作者简介:
李文渊,男,1962年出生,研究员,区域地质学

中图分类号: P512.2

计量

文章访问数: 564
HTML全文浏览量: 13
PDF下载量: 436
被引次数: 0

Late Neoproterozoic Sedimentations of the Carbonate -Detrital Flows in Longshou Mountains, Northwest China: Implications for Its Tectonic Environments

LI Wen yuan^1,2,
YANG Peng fei²

1.
Xi'an Institute of Geology and Mineral Resources, Xi'an 710054;
2.
Northwest University,Xi'an 710069

摘要

摘要: 华北地块西南缘龙首山隆起广布一套前寒武纪碳酸盐质为主要成分组成的碎屑流沉积,近年来发现在邻区北山、祁连山地区亦有分布。岩石状貌特殊,砾石大小混杂,呈无磨圆的棱角、半棱角状,为杂基支撑结构。区域上岩层连续性好,但厚薄不一,厚几米至几十米,局部与火山岩相变。根据其上覆、下伏岩层同位素年龄和微古植物化石定年资料,分析判断为新元古代中晚期的产物,讨论其成因为大陆裂谷沉积构造环境下,地壳急剧动荡,崩塌原稳定台地相的沉积,大量崩塌堆积物在大陆裂谷斜坡形成碎屑流移动而成。其为大陆裂谷的典型沉积,具有重要的指相意义。龙首山及邻区新元古代中晚期大面积碎屑流沉积分布,表证当时大规模大陆裂谷作用的发生,与全球性Rodinia大陆裂解的认识一致.
- 碳酸盐质碎屑流沉积 /
- 大陆裂谷 /
- 构造指相
Abstract: In Longshou Mountains of the southwestern margins of North China. s Plate, there is extensively a se -ries of Pre -Cambrian sedimentary of the detrital flows consisting of dominant carbonate, and the sedimentary rockshave also been found in recent years. The rocks are characterized by chaotic gravels on grain sizes, dominantdolomite gravels, bed -rounded gravelsshowing angulate -subangulate, and textures of matrix support. In the regionthe sediments distributed continuously, but its thickness is various from several meters to tens of meters, locallytransforming to volcanic rocks. On the basis of the isotopic ages and micro -paleobotanic fossils of the over and un -derlain strata, the sedimentary rocks were suggested forming in late Neoproterozoic era. Its origin is thought to bethe sediments of the carbonate - fragmental flows, on a sedimentary- tectonic environment of paleo- continentalrift, coming from large quantities of collapse files on slope of continental rift due to crustal movement rapidly tolead to breakdown of sedimentary rocks on steady platform. So these rocks are the typical sediments of the cont- inental rift, and important significance on implication for the tectonic environments. In Longshou Mountains andneighboring area the distribution of large quantities of the late Neoprozoic sediments of palaeo- fargmental flowsindicate that in that time a large scale of continental rift had occurred and consistent with splitting recognition ofthe Rodinia continent globally.
- carbonate -debris flows /
- continental rift /
- tectonic facies

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参考文献(13)

[1]	李文渊.龙首山震旦纪砾状白云岩成因探讨.甘肃地质, 1991,12:81～88[Li Wenyuan.Discussion on the origin of the Sinian rudaceous dolomitites in the Longshou Mountains. Gansu Geology, 1991,12: 81～88]
[2]	李文渊.龙首山地区的震旦系.西北地质, 1992,2:81～88[Li Wenyuan.On the Sinian systemte in the Longshou Mountains. Northwestern Geology, 1991, 2: 81～88]
[3]	修群业,陆松年,于海峰,等.龙首山岩群主体划归古元古代的同位素年龄证据.前寒武纪研究进展, 2002.25(2):93～96[Xiu Qunyi, Lu Songnian, Yu Haifeng, et al. The isotopic age evidence for main Longshoushan Group contributing to Palaeoproterozoic. Progess in Precambrian Research, 2002, 25(2): 93～96]
[4]	汤中立,李文渊.金川硫化铜镍(含铂)矿床成矿模式及地质对比.北京:地质出版社, 1995.1～209[Tang Zhongli, Li Wenyuan. Nickel-copper sulfide ( platinum-bearing) mineral deposit and geologic contrast. Beijing: Geological Publishing House, 1995. 1～209]
[5]	John Shaw. Coarse-grained sediment gravity flow facies in a large supraglacial lake. Sedimentology, 1988, 35: 527～529
[6]	赵祥生,邹湘华,牛道韫, 等. 北山地区震旦系及其冰川沉积. 西安地质矿产研究所所刊, 1984, 7: 29～37[Zhao Xiangsheng, Zou Xianghua, Niu Daoyun, et al. The Sinian system and its glacial deposits in Beishan district. Bulletin of the Xian Institute of Geology and Mieram Resources, Chinese Academy of Geological Sciences, 1984,7: 29～37]
[7]	Zhang Zhimeng, Liou J G, Coleman R G. An outline of the plate tectonic of China. Geologist Society of America Bulletin, 1984, 5:.295～312
[8]	夏林圻,夏祖春,徐学义.北祁连山海相火山岩岩石成因.北京:地质出版社, 1996.1～153[Xia Linqi, Xia Zuchun, Xu Xueyi. The petrogenesis of marine volcanic rocks from the Northern Qilian Mountains. Beijing: Geological Publish House, 1996. 1～153]
[9]	孙枢.中国地台区张裂盆地沉积.沉积学报, 1987,5(3): 6～16[Song Shu. Sedimentations of tension basins in China. Acta Sedimentologica Sinica, 1987, 5(3): 6～16]
[10]	张文治.新元古时期中国华南和华北陆块的相对位置及构造意义.前寒武纪研究进展, 2002,25(2):120～128[Zhang Wenzhi. Relative positions of South and North China blocks in Neoproterozoic and its tectonic significance. Progess in Precambrian Research, 2002, 25(2): 120-128]
[11]	董云鹏, 张国伟, 朱炳泉. 北秦岭构造属性与元古代构造演化. 地球学报, 2003, 24(1): 3～10[Dong Yunpeng, Zhang Guowei, Zhu Bingquan. Proterozoic tectonics and evolutionary history of the North Qinling Terrane. Acta Geoscientia Sinica, 2003, 24(1): 3～10]
[12]	崔广振. 贺兰山裂堑的垮塌堆积. 见: 中国北方板块构造论文集( 第1集).北京:地质出版社, 1987.1～209[Cui Guangzheng. Collapse piles of the pear in Helanshun. in: Contributions for the project of plate tectonics in Northern China,Vol.1. Beijing: Geological Publishing House, 1987.1～209]
[13]	Yin An. Geologic evolution of the Himalayan-Tibetan orogen in the context of Phanerozoic contiental growth of Asia. Acta Geoscientia Sinica, 2001, 22(3): 193～230

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甘肃龙首山新元古代烧火筒群沉积特征及其构造意义

李文渊^1,2,
杨鹏飞²

1. 西安地质矿产研究所西安 710054;

2. 西北大学地质学系西安 710054

基金项目: 中国地质调查局地质调查项目资助

作者简介:
李文渊,男,1962年出生,研究员,区域地质学

收稿日期: 2003-06-10
修回日期: 2003-08-26
刊出日期: 2004-03-10

中图分类号: P512.2

关键词:

碳酸盐质碎屑流沉积 /

大陆裂谷 /

构造指相

摘要: 华北地块西南缘龙首山隆起广布一套前寒武纪碳酸盐质为主要成分组成的碎屑流沉积,近年来发现在邻区北山、祁连山地区亦有分布。岩石状貌特殊,砾石大小混杂,呈无磨圆的棱角、半棱角状,为杂基支撑结构。区域上岩层连续性好,但厚薄不一,厚几米至几十米,局部与火山岩相变。根据其上覆、下伏岩层同位素年龄和微古植物化石定年资料,分析判断为新元古代中晚期的产物,讨论其成因为大陆裂谷沉积构造环境下,地壳急剧动荡,崩塌原稳定台地相的沉积,大量崩塌堆积物在大陆裂谷斜坡形成碎屑流移动而成。其为大陆裂谷的典型沉积,具有重要的指相意义。龙首山及邻区新元古代中晚期大面积碎屑流沉积分布,表证当时大规模大陆裂谷作用的发生,与全球性Rodinia大陆裂解的认识一致.

English Abstract

Late Neoproterozoic Sedimentations of the Carbonate -Detrital Flows in Longshou Mountains, Northwest China: Implications for Its Tectonic Environments

LI Wen yuan^1,2,
YANG Peng fei²

1. Xi'an Institute of Geology and Mineral Resources, Xi'an 710054;

2. Northwest University,Xi'an 710069

Received Date: 2003-06-10
Rev Recd Date: 2003-08-26
Publish Date: 2004-03-10

Keywords:

Abstract: In Longshou Mountains of the southwestern margins of North China. s Plate, there is extensively a se -ries of Pre -Cambrian sedimentary of the detrital flows consisting of dominant carbonate, and the sedimentary rockshave also been found in recent years. The rocks are characterized by chaotic gravels on grain sizes, dominantdolomite gravels, bed -rounded gravelsshowing angulate -subangulate, and textures of matrix support. In the regionthe sediments distributed continuously, but its thickness is various from several meters to tens of meters, locallytransforming to volcanic rocks. On the basis of the isotopic ages and micro -paleobotanic fossils of the over and un -derlain strata, the sedimentary rocks were suggested forming in late Neoproterozoic era. Its origin is thought to bethe sediments of the carbonate - fragmental flows, on a sedimentary- tectonic environment of paleo- continentalrift, coming from large quantities of collapse files on slope of continental rift due to crustal movement rapidly tolead to breakdown of sedimentary rocks on steady platform. So these rocks are the typical sediments of the cont- inental rift, and important significance on implication for the tectonic environments. In Longshou Mountains andneighboring area the distribution of large quantities of the late Neoprozoic sediments of palaeo- fargmental flowsindicate that in that time a large scale of continental rift had occurred and consistent with splitting recognition ofthe Rodinia continent globally.

李文渊, 杨鹏飞. 甘肃龙首山新元古代烧火筒群沉积特征及其构造意义[J]. 沉积学报, 2004, 22(1): 142-147.

引用本文:

李文渊, 杨鹏飞. 甘肃龙首山新元古代烧火筒群沉积特征及其构造意义[J]. 沉积学报, 2004, 22(1): 142-147.

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甘肃龙首山新元古代烧火筒群沉积特征及其构造意义

作者简介:
李文渊,男,1962年出生,研究员,区域地质学

计量

Late Neoproterozoic Sedimentations of the Carbonate -Detrital Flows in Longshou Mountains, Northwest China: Implications for Its Tectonic Environments

计量

目录

甘肃龙首山新元古代烧火筒群沉积特征及其构造意义

1. 西安地质矿产研究所西安 710054;

2. 西北大学地质学系西安 710054

作者简介:
李文渊,男,1962年出生,研究员,区域地质学

English Abstract

Late Neoproterozoic Sedimentations of the Carbonate -Detrital Flows in Longshou Mountains, Northwest China: Implications for Its Tectonic Environments

1. Xi'an Institute of Geology and Mineral Resources, Xi'an 710054;

2. Northwest University,Xi'an 710069

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[1]	李忠. “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, (6): 928-933.
[2]	李忠. “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, 24(06): 928-933.

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甘肃龙首山新元古代烧火筒群沉积特征及其构造意义

作者简介: 李文渊,男,1962年出生,研究员,区域地质学

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Late Neoproterozoic Sedimentations of the Carbonate -Detrital Flows in Longshou Mountains, Northwest China: Implications for Its Tectonic Environments

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出版历程

目录

甘肃龙首山新元古代烧火筒群沉积特征及其构造意义

1. 西安地质矿产研究所 西安 710054; 2. 西北大学地质学系 西安 710054

作者简介: 李文渊,男,1962年出生,研究员,区域地质学

English Abstract

Late Neoproterozoic Sedimentations of the Carbonate -Detrital Flows in Longshou Mountains, Northwest China: Implications for Its Tectonic Environments

1. Xi'an Institute of Geology and Mineral Resources, Xi'an 710054; 2. Northwest University,Xi'an 710069

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
李文渊,男,1962年出生,研究员,区域地质学

1. 西安地质矿产研究所西安 710054;

2. 西北大学地质学系西安 710054

作者简介:
李文渊,男,1962年出生,研究员,区域地质学

1. Xi'an Institute of Geology and Mineral Resources, Xi'an 710054;

2. Northwest University,Xi'an 710069