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新疆伊犁塔克尔莫乎尔沙漠全新世晚期沉积微量元素反映的古气候变化
引用本文:靳建辉,李志忠,陈秀玲,凌智永,曹相东,王少朴. 新疆伊犁塔克尔莫乎尔沙漠全新世晚期沉积微量元素反映的古气候变化[J]. 沉积学报, 2011, 29(2): 336-345
作者姓名:靳建辉  李志忠  陈秀玲  凌智永  曹相东  王少朴
作者单位:福建师范大学 地理科学学院 福州 350007
基金项目:国家“十一五”科技支撑计划项目(编号:2007BAC15B07); 新疆维吾尔自治区自然科学基金项目(编号:200821103)资助
摘    要:在新疆伊犁塔克尔莫乎尔沙漠腹地,选择可克达拉剖面(TKP)进行光释光(OSL)测年、微量元素含量测定,通过不同化学性质微量元素含量变化以及元素比值的相关分析与因子分析,探讨微量元素迁移的气候环境意义,结合粒度参数和碳酸盐含量变化特点,重建了研究区3.71 ka BP以来的气候变化序列.结果表明:晚全新世以来研究区古气候...

关 键 词:新疆  塔克尔莫乎尔沙漠  晚全新世  微量元素  地球化学  古气候
收稿时间:1900-01-01

Paleoclimatic Significance of Geochemical Elements from Takermohur Desert, Xinjiang since Late Holocene
JIN Jian-hui,LI Zhi-zhong,CHEN Xiu-ling,LING Zhi-yong,CAO Xiang-dong,WANG Shao-pu. Paleoclimatic Significance of Geochemical Elements from Takermohur Desert, Xinjiang since Late Holocene[J]. Acta Sedimentologica Sinica, 2011, 29(2): 336-345
Authors:JIN Jian-hui  LI Zhi-zhong  CHEN Xiu-ling  LING Zhi-yong  CAO Xiang-dong  WANG Shao-pu
Affiliation:School of Geography Science, Fujian Normal University, Fuzhou 350007
Abstract:Takermohur desert is located in Yili valley of west Xinjiang,which is also situated at semiarid desert geochemical environment in mid-latitude westerlies of northern hemisphere.In the center of the desert,we observed a continuously sedimentary profile(with 3.6m outcropped thickness) which is formed with alternative aeolian layers and paleosol layers.On this profile,we collected 72 samples with 5cm equal interval and 3 samples for OSL dating.In the laboratory,we tested 18 trace elements content with X-ray fl...
Keywords:Xinjiang  Takermohur Desert  late Holocene  trace element  geochemistry  paleoclimate  
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