ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
四川黄龙大湾-张家沟钙华沉积剖面的古气候记录研究
  
关键词:travertine  chronology  oxygen-carbon isotope  paleo-climate  Huanglong
基金项目:四川省地矿局区调队生态所科研项目
作者单位E-mail
王华 中国地质科学院岩溶地质研究所,广西桂林541004 wanghual@163.com 
杨更 四川省地矿局区域地质调查队,四川双流610213
成都理工大学地球科学学院,四川成都610059 
 
覃嘉铭 中国地质科学院岩溶地质研究所,广西桂林541004  
郭建强 四川省地矿局区域地质调查队,四川双流610213  
曹俊 四川省地矿局区域地质调查队,四川双流610213  
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摘要:
Records of Paleoclimate Changes Based on the Dawan-Zhangjiagou Travertine Deposition Profile in Huanglong, Sichuan
      The 14.0~85.0 ka B.P.deposition sequence along the Dawan-Zhangjiagou travertine profile in Huanglong was confirmed by a systematic investigation there.Not assuming the natural order that changes from bottom to top and from old to new,the travertine profile results probably from multi-stage deposition(at least two stages).Based on an oxygen-carbon stable isotope analysis,the authors reconstructed the palaeoclimate changes in the process of deposition.At the early stage of the travertine profile formation,the summer monsoon was powerful,the temperature was relatively high,and the precipitation was abundant in the summer season;at the middle stage and the last stage,the climate was dry,cold,and liable to change.According to deposition characteristics and chronological data of the travertine,a model for travertine deposition in this area was tentatively constructed.
WANG Hua,YANG Geng,QIN Jia-ming,GUO Jian-qiang,CAO Jun.2007.Records of Paleoclimate Changes Based on the Dawan-Zhangjiagou Travertine Deposition Profile in Huanglong, Sichuan[J].Acta Geoscientica Sinica,28(5):469-474.
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