首页 | 本学科首页   官方微博 | 高级检索  
     检索      

新疆且末奥依亚依拉克几克里阔勒地区河流阶地及其隆升特征
引用本文:戴传固,卢定彪,刘爱民,代雅然.新疆且末奥依亚依拉克几克里阔勒地区河流阶地及其隆升特征[J].贵州地质,2013(4):245-249.
作者姓名:戴传固  卢定彪  刘爱民  代雅然
作者单位:贵州省地质调查院,贵州贵阳550005
基金项目:属1∶25万奥依亚依拉克幅区域地质调查项目成果.
摘    要:通过对新疆且末几克里阔勒地区河流阶地的地貌、沉积特征及年龄测定,分析了该地区河流阶地形成的时代,反演了该地区4.45±0.35× 104a以来的隆升历史.结果表明,44.5 Ka以来的历史进程中地壳的隆升速率极大,大大高于目前青藏高原整体隆升2 mm/a的水平;形成的多级阶地表明该区的隆升存在明显的阶段性、间歇性和差异性,其隆升速率具有从快逐渐变慢的总体趋势.

关 键 词:河流阶地  隆升  几克里阔勒地区

Characteristics of River Terrace and its Uplift in Qimoaoyiyayilake-Jikelikuole Area of Xinjiang
DAI Chuan-gu,LU Ding-biao,LILT Ai-min,DAI Ya-ran.Characteristics of River Terrace and its Uplift in Qimoaoyiyayilake-Jikelikuole Area of Xinjiang[J].Guizhou Geology,2013(4):245-249.
Authors:DAI Chuan-gu  LU Ding-biao  LILT Ai-min  DAI Ya-ran
Institution:( Guizhou Academy of Geologic Survey, Guiyang 550005, Guizhou, China)
Abstract:By study the geomorphology, sedimentary characteristic and determine the age of fiver terrace in Jikelikuole area, the formation age of fiver terraces are analyzed, the uplift process in this area sine 4.45+0.35 × 104 a are reconstructed. The results indicate that a much higher uplift rate ( 〉2 mm/a) existed in the Tibetan Plateau. The multi-stages terraces suggest that the uplift rates of the study area shows a gradually slow trend since about 4.45×104 a.
Keywords:River terrace  Uplift  Jikelikuole area
本文献已被 维普 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号