新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升&mdash;&mdash;I地层学与岩石学证据

郑洪波; KatherineButcher; ChrisPowell

新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升——I地层学与岩石学证据

1.
同济大学海洋地质实验室上海 200092;
2.
中国科学院地球环境研究所西安 710054;
3.
TectOnic Special research Centre,The University Of western Australia,Australia

基金项目: 中国科学院“百人计划”;国家杰出青年基金(40025107);国家重点基础研究发展规划项目(G2000078501);教育部“长江特聘教授”计划资助

详细信息

作者简介:
郑洪波,男,1965年出生,教授,第四纪地质与过去全球变化

中图分类号: P534.63

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Evolution of Neogene Foreland Basin in Yecheng, Xinjiang, and Uplift of Northern Tibetan Plateau——I Stratigraphy and Petrology

1.
Laboratory of Marine Geology,Tongji University,Shanghai 200092;
2.
Instit ute of Eart h Environment,Chinese Academy of Sciences,Xi'an 710054;
3.
TectOnic Special research Centre,The University Of western Australia,Australia

摘要

摘要: 叶城晚新生代山前盆地的岩性主要由中新世的细粒泥岩和砂岩 (乌恰群 ),上新世的砂岩夹薄层砾岩 (阿图什组 )及上新世—更新世的粗粒砾岩 (西域组 )构成。中新世的沉积以细颗粒泥砂岩为主,表明物源区较远,古流域坡度较小,搬运距离较长。古流向分析显示物源区位于南和偏南方,此时昆仑山的地势起伏尚不大。到上新世的阿图什组沉积时,开始出现砾石沉积,反映西昆仑山已经开始有规模地隆升。西域砾岩的沉积标志着作为物源区的西昆仑山已有相当的高度,随着山系的隆升,基底岩石被暴露和剥蚀。
- 叶城 /
- 晚新生代 /
- 地层学 /
- 青臧高原
Abstract: Late Ceinozoic forland basin deposits in Yecheng are composed of Miocene mudstone and sandstone (Wuqia Group), Early Pliocene sandstone with minor gritstone (Artux Formation) and Late Pliocene-Early Pleistocene conglomerate (Xiyu Formation). The Miocene strata are dominated by fine-grained clastic material, indicating a distal source and low gradient slope. Palaeocurrent measurements suggested northward direction, indicating that the Kunlun area was at low elevation. Deposition of Artux Formation marked the first appearance of gravel and lithic detritus, indicating the uplift of the Kunlun. Xiyu Formation is characterized by coarse debris flow deposits, marking the strong uplift of the northern part of Tibetan Plateau and unroofing of the Kunlun.
- late Ceinozoic /
- stratigraphy /
- Tibetan Plateau /
- Yecheng

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参考文献(1)

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新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升——I地层学与岩石学证据

作者简介:
郑洪波,男,1965年出生,教授,第四纪地质与过去全球变化

计量

Evolution of Neogene Foreland Basin in Yecheng, Xinjiang, and Uplift of Northern Tibetan Plateau——I Stratigraphy and Petrology

计量

目录

新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升——I地层学与岩石学证据

1. 同济大学海洋地质实验室上海 200092;

2. 中国科学院地球环境研究所西安 710054;

3. TectOnic Special research Centre,The University Of western Australia,Australia

作者简介:
郑洪波,男,1965年出生,教授,第四纪地质与过去全球变化

English Abstract

Evolution of Neogene Foreland Basin in Yecheng, Xinjiang, and Uplift of Northern Tibetan Plateau——I Stratigraphy and Petrology

1. Laboratory of Marine Geology,Tongji University,Shanghai 200092;

2. Instit ute of Eart h Environment,Chinese Academy of Sciences,Xi'an 710054;

3. TectOnic Special research Centre,The University Of western Australia,Australia

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留言板

新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升——I地层学与岩石学证据

作者简介: 郑洪波,男,1965年出生,教授,第四纪地质与过去全球变化

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出版历程

Evolution of Neogene Foreland Basin in Yecheng, Xinjiang, and Uplift of Northern Tibetan Plateau——I Stratigraphy and Petrology

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出版历程

目录

新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升——I地层学与岩石学证据

1. 同济大学海洋地质实验室 上海 200092; 2. 中国科学院地球环境研究所 西安 710054; 3. TectOnic Special research Centre,The University Of western Australia,Australia

作者简介: 郑洪波,男,1965年出生,教授,第四纪地质与过去全球变化

English Abstract

Evolution of Neogene Foreland Basin in Yecheng, Xinjiang, and Uplift of Northern Tibetan Plateau——I Stratigraphy and Petrology

1. Laboratory of Marine Geology,Tongji University,Shanghai 200092; 2. Instit ute of Eart h Environment,Chinese Academy of Sciences,Xi'an 710054; 3. TectOnic Special research Centre,The University Of western Australia,Australia

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
郑洪波,男,1965年出生,教授,第四纪地质与过去全球变化

1. 同济大学海洋地质实验室上海 200092;

2. 中国科学院地球环境研究所西安 710054;

3. TectOnic Special research Centre,The University Of western Australia,Australia

作者简介:
郑洪波,男,1965年出生,教授,第四纪地质与过去全球变化

1. Laboratory of Marine Geology,Tongji University,Shanghai 200092;

2. Instit ute of Eart h Environment,Chinese Academy of Sciences,Xi'an 710054;

3. TectOnic Special research Centre,The University Of western Australia,Australia