TL age of lacustrine sediments from Aibi Lake of Xinjiang and its enviromental implication

Lu Liangcai Huang Baolin

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TL age of lacustrine sediments from Aibi Lake of Xinjiang and its enviromental implication

更新时间：2021-04-09

- TL age of lacustrine sediments from Aibi Lake of Xinjiang and its enviromental implication
- NUCLEAR TECHNIQUES Issue 4, (1993)
- 作者机构：
  
  1. 中国科学院地球化学研究所广州分部
  2. 中国科学院地球化学研究所广州分部,广州,510640
- 作者简介：
- 基金信息：
- DOI：
  CLC：
- Published：01 April 1993
- 稿件说明：
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[1]卢良才,黄宝林.新疆艾比湖沉积物的热释光年龄及其环境意义[J].核技术,1993(04):251-253.

Lu Liangcai Huang Baolin. TL age of lacustrine sediments from Aibi Lake of Xinjiang and its enviromental implication[J]. Nuclear techniques, 1993, (4): 251-253.
[1]卢良才,黄宝林.新疆艾比湖沉积物的热释光年龄及其环境意义[J].核技术,1993(04):251-253. DOI：

Lu Liangcai Huang Baolin. TL age of lacustrine sediments from Aibi Lake of Xinjiang and its enviromental implication[J]. Nuclear techniques, 1993, (4): 251-253. DOI：

摘要

应用热释光（TL）技术对新疆艾比湖进行了TL年龄测定。其结果表明新疆艾比湖区存在着大约以5000年为周期的湖退过程。全新世以来湖区存在着三次较大的气候环境演变:10—7kaB.P.气候干凉;7.5—2.5kaB.P.气候温暖湿润;2.5kaB.P.至今气候干凉偏旱。

Abstract

Lacustrine deposits from Aibi Lake

Xinjiang have been dated by TL technique. The results suggest that the regression process of the lake has a period of about 5000 years and 3 climate stages occur sequently in the evolution process in Holocene

including the dry and cool stage of 10- 7 ka B.P.

the moist and warm stage of 7.5- 2.5ka B.P. and the dry and cool stage since 2.5ka B.P.

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