青藏高原南部乌郁盆地渐新世&mdash;上新世地层沉积相分析

朱迎堂 方小敏 高军平 伊海生 王世锋 张伟林

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青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析

朱迎堂方小敏高军平伊海生王世锋张伟林

文章导航 > 沉积学报 > 2006 > 24(06): 775-782

朱迎堂方小敏高军平伊海生王世锋张伟林. 青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析[J]. 沉积学报, 2006, 24(06): 775-782.

引用本文:

朱迎堂方小敏高军平伊海生王世锋张伟林. 青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析[J]. 沉积学报, 2006, 24(06): 775-782.

ZHU Ying-tang. Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2006, 24(06): 775-782.

Citation:

ZHU Ying-tang. Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2006, 24(06): 775-782.

朱迎堂方小敏高军平伊海生王世锋张伟林. 青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析[J]. 沉积学报, 2006, 24(06): 775-782.

引用本文:

朱迎堂方小敏高军平伊海生王世锋张伟林. 青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析[J]. 沉积学报, 2006, 24(06): 775-782.

ZHU Ying-tang. Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2006, 24(06): 775-782.

Citation:

ZHU Ying-tang. Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2006, 24(06): 775-782.

青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析

朱迎堂方小敏高军平伊海生王世锋张伟林

中国科学院青藏高原研究所北京 100085

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中图分类号: P512.2

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Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau

ZHU Ying-tang

Institute of Tibetan Platean Research, Chinese Academy of Sciences, Beijing 100085

摘要

摘要: 青藏高原南部乌郁盆地是欧亚与印度板块碰撞以来冈底斯山隆升最具代表性的盆地之一,也是青藏高原南部较大的新生代残留盆地之一。沉积盆地中保存着完整的渐新世—早更新世连续沉积记录,自下而上由古新世—始新世林子宗群(典中组、年波组和帕那组)、渐新世—中新世日贡拉组、中新世芒乡组、来庆组、上新世—早更新世乌郁群(乌郁组、达孜组),总厚度大于4180m。林子宗群为一套中—酸性钙碱性火山岩系,夹紫红色砂岩、砾岩及粉砂岩。日贡拉组主要为紫红色砂岩、砾岩,夹少量火山熔岩及酸性火山凝灰岩,为一套山间盆地沉积。芒乡组为灰色、深灰色泥岩、砂岩,夹煤和油页岩,为湖泊相—前三角洲相—沼泽相。来庆组为一套褐色安山岩、火山碎屑岩。乌郁组是一套碎屑岩,颜色呈灰色、灰褐色,夹煤及油页岩,为山间盆地辫状河—湖泊—沼泽沉积。达孜组是一套黄褐色砾岩、砂砾岩、砂岩,夹少量泥岩,发育铁质结核,为辫状河沉积。沉积相分析表明具有明显的古新世—始新世林子宗群(典中组、年波组和帕那组)、渐新世—中新世日贡拉组—芒乡组、中新世来庆组—上新世乌郁组、上新世—早更新世达孜组四个阶段式隆升—剥蚀过程。从芒乡组的潮湿炎热的气候转变为乌郁组的干燥凉爽,显然与青藏高原隆升密切相关。乌郁盆地渐新世—早更新世沉积相分析对于研究青藏高原隆升和油气等能源均具有重要意义。
- 沉积相 /
- 芒乡组 /
- 乌郁组 /
- 达孜组 /
- 渐新世&mdash /
- 中新世 /
- 高原隆升 /
- 乌郁盆地 /
- 青藏高原
Abstract: The Wuyu Basin, southern Tibetan Plateau is one of presental basin of India-Eurasia collision, a continuous sedimentary record throughout Oligocene to Miocene was discovered in the Wuyu Basin and considered as the most integrated Oligo-Miocene record within the Tibetan plateau, observed so far. The sedimentary include the Paleo-Eocene Linzizong Group (include the Dianzhong Formation, Nianbo Fm. and Pala Fm.) and the Oligo-Miocene Rigongla Fm., the Miocene Mangxiang Fm., the Miocene Laiqin Fm., the Pliocene Wuyu Fm., the Plio-Pleistocene Dazi Fm., with a total thickness of 4180m.The Linzizong Gr. composed chiefly of intermediate-acid lava, its middle part intercalated with brownish grey clastic sediment. The Oligo-Miocene Rigongla Fm., is the sediment of intermountain basin, consists mainly of reddish brown sandstone and conglomerate, intercalated with lava. The Miocene Mangxiang Fm. is the sediment from fluvial facies to lacustrine facies, swamp, chiefly grey, dark grey sandstone, siltstone, and mudstone, with coal and oil shale. The Miocene Laiqin Fm. is brown lava and pyroclastic flow sediment. The Pliocene Wuyu Fm. is grey, brown grey sandstone, siltstone, and mudstone, with coal and oil shale, which is fluvial-lacustrine-swamp facies. The Plio-Pleistocene Dazi Fm. is conglomerate, intercalated with grey mudstone. The Mangxiang Fm., suggesting the significant shifting of sediment provenance, the stable trending of tectonic movement, and the wet and torridity aridity of paleoclimate condition. The Oligo-Miocene paleoclimate and tectonic evolution of the Wuyu Basin has displayed its significance for understanding the early uplift of the Tibetan Plateau.
- depositional facies /
- Mangxiang Fm. /
- Wuyu Fm. /
- Dazi Fm. /
- Oligo-Miocene /
- Wuyu Basin /
- Tibetan Plateau /

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[1]	李尚昆, 魏志福, 王永莉, 汪亘, 马雪云, 张婷, 何薇, 玉晓丽, 李伦, 马贺, 魏静宜. 青藏高原中东部囊谦盆地始新世气候变化及其驱动机制 . 沉积学报, 2024, 42(2): 545-557. doi: 10.14027/j.issn.1000-0550.2022.063
[2]	戴霜, 胡惠, 马晓军, 樊鑫, 张明震, 姚旭, 王荣华, 郭雪莲, 刘成英, 王子璇, 王艺霖, 李彦杰, 孔雪, 韩思远. 青藏高原东北部武威盆地古近纪—新近纪地层划分及其构造意义 . 沉积学报, 2023, 41(2): 378-391. doi: 10.14027/j.issn.1000-0550.2021.160
[3]	刘昆, 程鹏, 宋鹏, 任科英, 李虎, 刘博通. 南海北部古海流对琼东南盆地中新世储层发育的影响 . 沉积学报, 2023, 41(4): 1181-1191. doi: 10.14027/j.issn.1000-0550.2022.056
[4]	陈留勤, 李鹏程, 郭福生, 刘鑫, 李馨敏. 粤北丹霞盆地晚白垩世丹霞组沉积相及古气候意义 . 沉积学报, 2019, 37(1): 17-29. doi: 10.14027/j.issn.1000-0550.2018.118
[5]	梁敏豪, 杨胜利, 成婷, 李帅, 刘楠楠, 陈慧. 青藏高原东部黄土沉积元素地球化学示踪 . 沉积学报, 2018, 36(5): 927-936. doi: 10.14027/j.issn.1000-0550.2018.065
[6]	. 青藏高原纳木错湖近150年来气候变化的湖泊沉积记录 . 沉积学报, 2014, 32(4): 669-676.
[7]	. 青藏高原北部新生代构造演化在柴达木盆地中的沉积记录 . 沉积学报, 2013, 31(05): 824-833.
[8]	. 南海晚中新世—上新世红河沉积体系研究 . 沉积学报, 2013, 31(1): 32-37.
[9]	王利强. 青藏高原纳木错湖阶沉积的发生特征及环境指示意义 . 沉积学报, 2009, 27(3): 503-510.
[10]	岳信东. 二连盆地白音查干凹陷下白垩统腾格尔组沉积相 . 沉积学报, 2008, 26(4): 593-601.
[11]	. 吉林松江盆地早白垩世大拉子组沉积特征及演化 . 沉积学报, 2008, 26(1): 61-69.
[12]	卓弘春. 松辽盆地北部上白垩统青山口—姚家组沉积相及层序地层界面特征 . 沉积学报, 2007, 25(1): 29-38.
[13]	朱迎堂, 方小敏, 高军平, 伊海生, 王世锋, 张伟林. 青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析 . 沉积学报, 2006, (6): 775-782.
[14]	刘志飞, 王成善, 金玮, 伊海生, 郑洪波, 赵西西, 李亚林. 青藏高原沱沱河盆地渐新—中新世沉积环境分析 . 沉积学报, 2005, 23(2): 210-217.
[15]	林春明, 宋宁, 牟荣, 赵彦彦, 汪亚军, 杨德洲. 江苏盐阜拗陷晚白垩世浦口组沉积相与沉积演化 . 沉积学报, 2003, 21(4): 553-559.
[16]	周江羽, 王江海, 尹安, Spurlin M S, Horton B K. 青藏东北缘早第三纪盆地充填的沉积型式及构造背景——以囊谦和下拉秀盆地为例 . 沉积学报, 2002, 20(1): 85-91.
[17]	宋春晖, 孙淑荣, 方小敏, 孙东. 酒西盆地晚新生代沉积物重矿物分析与高原北部隆升 . 沉积学报, 2002, 20(4): 552-559.
[18]	刘志飞, 王成善. 青藏高原北部可可西里盆地第三纪风火山群沉积环境分析 . 沉积学报, 2001, 19(1): 28-36.
[19]	孙广友, 罗新正, R.E.Turner. 青藏东北部若尔盖高原全新世泥炭沉积年代学研究 . 沉积学报, 2001, 19(2): 177-181,206.
[20]	林清, 王国尚, 耿安松, 张干. 青藏高原多年冻土湖沼沉积中的有机质 . 沉积学报, 1997, 15(S1): 24-29.

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青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析

朱迎堂方小敏高军平伊海生王世锋张伟林

中国科学院青藏高原研究所北京 100085

收稿日期: 2006-01-28
修回日期: 2006-04-01
刊出日期: 2006-12-10

中图分类号: P512.2

关键词:

沉积相 /

芒乡组 /

乌郁组 /

达孜组 /

中新世 /

摘要: 青藏高原南部乌郁盆地是欧亚与印度板块碰撞以来冈底斯山隆升最具代表性的盆地之一,也是青藏高原南部较大的新生代残留盆地之一。沉积盆地中保存着完整的渐新世—早更新世连续沉积记录,自下而上由古新世—始新世林子宗群(典中组、年波组和帕那组)、渐新世—中新世日贡拉组、中新世芒乡组、来庆组、上新世—早更新世乌郁群(乌郁组、达孜组),总厚度大于4180m。林子宗群为一套中—酸性钙碱性火山岩系,夹紫红色砂岩、砾岩及粉砂岩。日贡拉组主要为紫红色砂岩、砾岩,夹少量火山熔岩及酸性火山凝灰岩,为一套山间盆地沉积。芒乡组为灰色、深灰色泥岩、砂岩,夹煤和油页岩,为湖泊相—前三角洲相—沼泽相。来庆组为一套褐色安山岩、火山碎屑岩。乌郁组是一套碎屑岩,颜色呈灰色、灰褐色,夹煤及油页岩,为山间盆地辫状河—湖泊—沼泽沉积。达孜组是一套黄褐色砾岩、砂砾岩、砂岩,夹少量泥岩,发育铁质结核,为辫状河沉积。沉积相分析表明具有明显的古新世—始新世林子宗群(典中组、年波组和帕那组)、渐新世—中新世日贡拉组—芒乡组、中新世来庆组—上新世乌郁组、上新世—早更新世达孜组四个阶段式隆升—剥蚀过程。从芒乡组的潮湿炎热的气候转变为乌郁组的干燥凉爽,显然与青藏高原隆升密切相关。乌郁盆地渐新世—早更新世沉积相分析对于研究青藏高原隆升和油气等能源均具有重要意义。

English Abstract

Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau

ZHU Ying-tang

Institute of Tibetan Platean Research, Chinese Academy of Sciences, Beijing 100085

Received Date: 2006-01-28
Rev Recd Date: 2006-04-01
Publish Date: 2006-12-10

Keywords:

Abstract: The Wuyu Basin, southern Tibetan Plateau is one of presental basin of India-Eurasia collision, a continuous sedimentary record throughout Oligocene to Miocene was discovered in the Wuyu Basin and considered as the most integrated Oligo-Miocene record within the Tibetan plateau, observed so far. The sedimentary include the Paleo-Eocene Linzizong Group (include the Dianzhong Formation, Nianbo Fm. and Pala Fm.) and the Oligo-Miocene Rigongla Fm., the Miocene Mangxiang Fm., the Miocene Laiqin Fm., the Pliocene Wuyu Fm., the Plio-Pleistocene Dazi Fm., with a total thickness of 4180m.The Linzizong Gr. composed chiefly of intermediate-acid lava, its middle part intercalated with brownish grey clastic sediment. The Oligo-Miocene Rigongla Fm., is the sediment of intermountain basin, consists mainly of reddish brown sandstone and conglomerate, intercalated with lava. The Miocene Mangxiang Fm. is the sediment from fluvial facies to lacustrine facies, swamp, chiefly grey, dark grey sandstone, siltstone, and mudstone, with coal and oil shale. The Miocene Laiqin Fm. is brown lava and pyroclastic flow sediment. The Pliocene Wuyu Fm. is grey, brown grey sandstone, siltstone, and mudstone, with coal and oil shale, which is fluvial-lacustrine-swamp facies. The Plio-Pleistocene Dazi Fm. is conglomerate, intercalated with grey mudstone. The Mangxiang Fm., suggesting the significant shifting of sediment provenance, the stable trending of tectonic movement, and the wet and torridity aridity of paleoclimate condition. The Oligo-Miocene paleoclimate and tectonic evolution of the Wuyu Basin has displayed its significance for understanding the early uplift of the Tibetan Plateau.

朱迎堂方小敏高军平伊海生王世锋张伟林. 青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析[J]. 沉积学报, 2006, 24(06): 775-782.

引用本文:

朱迎堂方小敏高军平伊海生王世锋张伟林. 青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析[J]. 沉积学报, 2006, 24(06): 775-782.

ZHU Ying-tang. Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2006, 24(06): 775-782.

Citation:

ZHU Ying-tang. Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2006, 24(06): 775-782.

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青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析

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Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau

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青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析

中国科学院青藏高原研究所北京 100085

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Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau

Institute of Tibetan Platean Research, Chinese Academy of Sciences, Beijing 100085

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Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau

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青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析

中国科学院青藏高原研究所 北京 100085

English Abstract

Oligo-Mioence Depositional Facies of the Wuyu Basin, Southern Tibetan Plateau

Institute of Tibetan Platean Research, Chinese Academy of Sciences, Beijing 100085

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