IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
长江河源泥炭地形形成与全新世以来的环境变化
Alternative TitlePEATLAND AND ENVIRONMENT CHANGE SINCE LATE HOLOCENE IN THE SOURCE REGION OF CHANGJIANG RIVER
Language中文
孙广友; 汪佩芳; 王曼华; 邵庆春; 邓伟
Source Publication长江河源区自然环境研究
Editor孙广友 ; 唐邦兴 主编
Pages112-121
1995
Publisher科学出版社
Publication Place北京市
Keyword长江河源 泥炭地形 环境变化
Abstract

本文阐述了该区是世界最大的高原泥炭地,总面积达8000km2,最高海拔为5300m,最大泥炭厚度为1.8m。14C年龄为2670±70a,B.P.属于晚全新世堆积。近期环境趋向干旱。

Other Abstract

The peatland in Source the region of the Changjiang river is great area of plateau peatland in the world.Total area is 8000 km2, the highest elevation is 5300m.
    The peatland in the region Can be dividied into eight types as flood plain peatland. etc. all of them are deposit late Holocene,the large age is 2670±70a.B.P., rate of deposit is 1.1-0.27mm/a.
    In the the processes of peatland developilag,the ancient climate which has six times changes was cold wet and littie dry warm.

Document Type专著章节文集论文
Identifierhttp://ir.imde.ac.cn/handle/131551/7297
Collection成都山地所知识仓储(2009年以前)
山区发展研究中心
Recommended Citation
GB/T 7714
孙广友,汪佩芳,王曼华,等. 长江河源泥炭地形形成与全新世以来的环境变化. 长江河源区自然环境研究. 北京市:科学出版社,1995:112-121.
Files in This Item:
File Name/Size DocType Version Access License
12-长江河源泥炭地形形成与全新世以来的(2567KB) 开放获取CC BY-NC-SAView Application Full Text
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[孙广友]'s Articles
[汪佩芳]'s Articles
[王曼华]'s Articles
Baidu academic
Similar articles in Baidu academic
[孙广友]'s Articles
[汪佩芳]'s Articles
[王曼华]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[孙广友]'s Articles
[汪佩芳]'s Articles
[王曼华]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: 12-长江河源泥炭地形形成与全新世以来的环境变化.pdf
Format: Adobe PDF
This file does not support browsing at this time
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.