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青海囊谦古近纪盆地沉积特征及沉积环境分析
引用本文:杜后发,姜勇彪,严兆斌,侯增谦,杨天南,郭福生,杨庆坤.青海囊谦古近纪盆地沉积特征及沉积环境分析[J].地质学报,2011,85(3):383-395.
作者姓名:杜后发  姜勇彪  严兆斌  侯增谦  杨天南  郭福生  杨庆坤
作者单位:1. 东华理工大学地球科学学院,江西抚州,344000;放射性地质与勘探技术国防重点学科实验室,江西抚州,344000
2. 东华理工大学地球科学学院,江西抚州,344000
3. 东华理工大学核资源与环境教育部重点实验室,南昌,330013
4. 东华理工大学地球科学学院,江西抚州,344000;中国地质科学院地质研究所,北京,100037
5. 中国地质科学院地质研究所,北京,100037
基金项目:国家自然科学基金项目(批准号:U0933605),中国地质调查局地质调查工作项目(编号:1212010818096)
摘    要:囊谦盆地是在藏东北段沿金沙江-红河构造带分布着一系列呈NNW向展布的中小型古近纪盆地的典型代表.通过野外地质调查、分析测试和室内综合研究,在盆地演化的格架内,系统分析了囊谦盆地贡觉组古气候、沉积相标志、物源以及沉积环境等方面的特征,认为贡觉组可划分为三段式结构,沉积环境为冲积扇-河流-湖泊-三角洲环境;砾石成分较复杂,...

关 键 词:沉积环境  沉积特征  古近纪  物源  囊谦盆地
收稿时间:2010/7/10 0:00:00
修稿时间:2010/10/24 0:00:00

Sedimentary characteristics and environment of Nangqian Paleogene basin in Qinghai Province
Du houf,Jiang Yongbiao,Yan Zhaobin,Hou Zengqian,Yang Tiannan,Guo Fusheng and Yang Qingkun.Sedimentary characteristics and environment of Nangqian Paleogene basin in Qinghai Province[J].Acta Geologica Sinica,2011,85(3):383-395.
Authors:Du houf  Jiang Yongbiao  Yan Zhaobin  Hou Zengqian  Yang Tiannan  Guo Fusheng and Yang Qingkun
Institution:East China Institute of Technology,College of Earth Sciences, East China Institute of Technology,Key Laboratory of Radioactive Geology and Exploration Technology Fundamental Science for National Defense,Institute of Geology, CAGS,Institute of Geology, CAGS,,East China Institute of Technology,College of Earth Sciences, East China Institute of Technology
Abstract:Nangqian basin is the typical representative of the medium-mini-type paleogene basins controlled by the local north-northwest-treading faults and distributing along Jinsha-Red River belt in the northeastern margin of Qinghai-Tibet. Combined with results of field geological investigation, and analysis and determination of samples, as well as the indoor comprehensive study, the paleoclimate characteristics, indications of sedimentary facies, the provenance as well as depositional environment of Gonjo group in Nangqian basin are systematically analyzed in the framework of the basin evolution. Authors conclude that the Gonjo group can be divided into the three-stage structure, and the depositional environment is the alluvial fan - river - lake - delta environment; the complex conglomerate gravel composition, the poorly sorted and rounded sandstone, and the fillings being the sub-angular shaped inequigranular grit , the calcite cement or the ferruginous cement indicate that the sedimentary environment is proximal and quickly accumulated, and the paleocurrent direction is versatile; the depositional environments belong to warm and moist-dry climate with strong evaporation.
Keywords:Depositional Environment  Sedimentary characteristics  Paleogene  Provenance  Nangqin baisn
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