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《Journal of Desert Research》 2009-02
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Environment Evolution and Salt Forming Process of Jilantai Salt Lake since 22ka BP

PANG Xi-lei1,HU Dong-sheng1,2(1.College of Resources and Environmental Science,Hunan Normal University,Changsha 410081,China;2.State Key Laboratory of Continental Dynamics,Northwest University,Xi'an 710069,China)  
According to quaternary geological investigation,sedimentary characteristic records and some comprehensive analysis of the study area and its adjacent areas,we take an exploratory analysis on the environment changing processes of Jilantai Salt Lake since 22 ka BP by using the analysis method of Sequence Stratigraphy.The evolution of the salt lake has experienced six stages: cold-dry period(22.0~14.0 ka BP),freshwater lake period;cold-wet period(14.0~9.782 ka BP),Dryas period;warm-wet period(9.782~7.0 ka BP),saline water period;period of climate changing from warm-wet to dry(7.0~6.0 ka BP),still saline water period,also the preparatory stage for the salt formation of the lake;cold-dry period(6.0~4.7 ka BP),the climate alternating between wet and dry frequently,salt water period,also the salt formation developing period of the salt lake;cool-dry period(4.7 ka BP~),it was the animated salt forming period,during which the lake water decreased rapidly and the around desert encroached,so the lake developed to sand covered lake gradually.The environmental change and climate transition in Jilantai area since 22 ka BP are responses to the global paleoclimate change,which have great significance in researches of salt resources formation events and the sustainable development of regional economy.
【Fund】: 湖南省重点学科建设项目(DL2007001)资助
【CateGory Index】: P532
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