易成兴,曾昌兴,陈仁.藏北丁固—加措地区中-上更新统高台阶砾石层的厘定及其意义[J].贵州地质,2014,31(2):96-98,88 |
藏北丁固—加措地区中-上更新统高台阶砾石层的厘定及其意义 |
Determination and Its Significance of Gravel Layer of High Stage of Middle-upper Pleistocene Series in Dinggu-Jiacuo Area of North Tibet |
投稿时间:2014-02-11 |
DOI: |
中文关键词: 中更新世 岩石地层 高台阶砾石层 丁固—加措地区 |
英文关键词:Middle Pleistocene Layer Gravel layer of high stage Dinggu-Jiacuo area |
基金项目:属1∶25万加措幅、丁固幅区域地质调查项目成果。 |
|
摘要点击次数: 2557 |
全文下载次数: 901 |
中文摘要: |
西藏北部丁固-加措地区,分布一套零星出露的、固结—半固结状态的砂砾岩层,在综合研究其岩石组合、沉积特征、地质时代、区域地质特征的基础上,将其厘定为一个非正式岩石地层单位——高台阶砾石层,该砾石层对研究区内第四系地质演化具有重要意义。 |
英文摘要: |
In the Dinggu-Jiacuo area of north Tibet, there is some exposed, solidified and semi-solidified gravel distributed, on the basis of studying the rock composition, sedimentary feature, geologic era and regional geologic characters, it is determined to be a informal stratigraphic unit:gravel layer of high stage, it will be important for Quaternary study in the target area. |
查看全文 查看/发表评论 下载PDF阅读器 |
|
|
|