| 可可西里盆地中新统五道梁群湖相碳酸盐岩岩石学特征与沉积环境分析 |
| |
| 引用本文： | 周恳恳,伊海生,林金辉. 可可西里盆地中新统五道梁群湖相碳酸盐岩岩石学特征与沉积环境分析[J]. 沉积与特提斯地质, 2007, 27(1): 25-31 |
| |
| 作者姓名： | 周恳恳 伊海生 林金辉 |
| |
| 作者单位： | 成都理工大学 沉积地质研究院,四川 成都 610059 |
| |
| 摘 要： | 湖相碳酸盐岩在可可西里盆地的古、新近纪地层中分布广泛,更是中新统五道梁群沉积的主要组成部分。五道梁群湖相碳酸盐岩分为生物粘结灰岩(叠层石)、泥晶灰岩、颗粒灰岩与泥晶白云岩四大类,反映出沉积环境为一个具有浅水—半深水、高盐度、半封闭—封闭特点的综合湖泊系统。
|
| 关 键 词： | 可可西里盆地 中新统 五道梁群 湖相碳酸盐岩 岩石学 沉积环境 青海 |
| 文章编号： | 1009-3850（2007）01-0025-07 |
| 收稿时间： | 2006-07-03 |
| 修稿时间： | 2006-07-032006-09-25 |
Petrology and sedimentary environments of the lacustrine carbonate rocks from the Miocene Wudaoliang Group in the Hoh Xil Basin, Qinghai |
| |
| ZHOU Ken-ken,YIN Hai-sheng,LIN Jin-hui. Petrology and sedimentary environments of the lacustrine carbonate rocks from the Miocene Wudaoliang Group in the Hoh Xil Basin, Qinghai[J]. Sedimentary Geology and Tethyan Geology, 2007, 27(1): 25-31 |
| |
| Authors: | ZHOU Ken-ken YIN Hai-sheng LIN Jin-hui |
| |
| Affiliation: | Research Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059,Sichuan,China |
| |
| Abstract: | The lacustrine carbonate rocks occur on a wide range of scales in the Palaogene and Neogene strata in the Hoh Xil Basin,Qinghai,and constitute an important part of the Miocene Wudaoliang Group sediments.The lacustrine carbonate rocks in the Wudaoliang Group consist of boundstone(stromatolite),micritic limestone,grainstone and micritic dolostone which were laid down in the shallow-water to bathyal,high-salinity and enclosed to semienclosed lake systems. |
| |
| Keywords: | Hoh Xil Basin Miocene Wudaoliang Group lacustrine carbonate rock petrology sedimentary environment Qinghai |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《沉积与特提斯地质》浏览原始摘要信息 |
|
点击此处可从《沉积与特提斯地质》下载全文 |
