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Timing on Cave Deposit (Stalagmites) by High Precision Thermal Ionization Mass Spectrometry (TIMS)

WANG Zhao rong PENG Zi cheng SUN Wei dong (University of Science and Technology of China,Hefei 230026) (Advanced Centre for Earth Science and Astronomy,USTC.Third world Academy of Sciencs Hefei 230026)  
Cave calcium has turned out to be a very important data bank of paleoclimatic evolution.Stalagmite,flow stone and calcite veins in caves,like tree rings,ice cores,loess and lacustrine deposits,contain precise records of past environmental variation.Deciphering of these "codes" would contribute significantly to a better understanding of environmental changes on a global scale and would thereby enable us to make a better prediction of the future trend of climatic and environmental evolution. Highly precise dating is one of the problems in global change study and is recently considered as a hot point in the Quaternary geology.With high sensitive and high precision U Th disequilibrium method,Quaternary geology age by thermal ionization mass spectrolmetry (TIMS) has been determined.This has obtained significant achievements in palaeoclimate,palaeoenvironment,palaeo ocean,archaeology and modern volcanism magmatism studies.In this paper,we have determined Chinese standard sample stalagmite (GBW4412,GBW4413) and international standare sample Cpra;s(RKM 4) By MAT 262 mass spectrometer.The measured U content,isotopic ration and age value comply with that of the standard sample very well,indicating that an ideal tool for precise timing,which is the TIMS method is analysis also of advantages such as rapid,high precision and low sample comsuption.
【Fund】: 国家自然科学基金! (批准号 :498772 0 61);;中国科学院西安黄土研究室开放实验室资助
【CateGory Index】: P642.25
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