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松潘黄龙自然保护区第四纪冰期划分与古气候环境分析研究
引用本文:曹俊,郭建强.松潘黄龙自然保护区第四纪冰期划分与古气候环境分析研究[J].四川地质学报,2001,21(3):141-146.
作者姓名:曹俊  郭建强
作者单位:四川省地勘局区调队环境旅游所,四川双流,610213
摘    要:松潘黄龙自然保护区第四纪冰川遗迹十分发育,在三岔子一带冰碛物出露齐全、保存完好。通过剖面的测制,再结合孢粉、ESR测年样等成果综合研究,将该地区划分为四次冰期,三次间冰期,Ⅳ个孢粉组合带。阐明了冰川活动与成景作用关系密切,黄龙钙华景观的雏形是在中更新世末形成,大量钙华堆积形成了晚更新世。

关 键 词:冰期划分  古气候环境分析  冰川活动  成景作用关系  松潘黄龙自然保护区  冰川遗迹
文章编号:1006-0995(2001)03-0141-06

QUATERNARY ICE AGE DIVISION AND PALEOCLIMATE AND PALEOENVIRONMENT IN THE HUANGLONG NATURE RESERVE, SONGPAN
Cao Jun and Guo Jianqiang.QUATERNARY ICE AGE DIVISION AND PALEOCLIMATE AND PALEOENVIRONMENT IN THE HUANGLONG NATURE RESERVE, SONGPAN[J].Acta Geologica Sichuan,2001,21(3):141-146.
Authors:Cao Jun and Guo Jianqiang
Abstract:Quaternary glacial vestige is well developed in the Huanglong Nature Reserve, especially, in the Sanchazi Valley. On the basis of profiling in combination with sporopollen analysis and ESR dating, the Quaternary ice age in this region may be divided into 4 glacial stages, 3 interglacial stages and 4 sporopollen association zones. Glaciation was in close relationship with landscape formation. The undeveloped forms of the Huanglong Travertine Landscape were formed at the end of the Middle Pleistocene, while a great amount of travertine accumulation were formed in the Late Pleistocene.
Keywords:Huanglong  Songpan  glacial age division  analysis of paleoclimate and paleoenvironment  relationship between glaciation and landscape formation
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