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《Journal of Anhui Agricultural Sciences》 2010-09
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Changing Mechanisms of Calcium Carbonate in Heilinding Section of Linxia Basin from 11.6 to 5.0 Ma

ZHANG Qi-bo et al (Key Laboratory of Western China's Environmental Systems,Ministry of Education of China & College of Resources and Environment,Lanzhou University,Lanzhou,Gansu 730000)  
As a good indication of the Loess-paleosol sequence's occurrence and climate changes,the calcium carbonate content is referred as an effective substitute indicator for climate and expends into other sedimentary types continuously. Heilinding Section of Linxia Basin appears a set of successive and integral lacustrine-fluvial strata of Late Cenozoic. Through the experimental measurement of calcium carbonate in this set of strata,It was found that the CaCO3 content is relatively stable and the average is 10.1%. While it decreases obiviously from 8.6 Ma and the average is 8.4%. Comparing with the magnetic susceptibility and chromatic indicators of this section and the climate records of surrounding areas,it is believed that the transition of calcium carbonate in the 8.6 Ma should not be simply explained as climate changes but is most probably related to quantity and rapid deposition of clast caused by the rapid stage uplift of the Tibetan Plateau.
【Fund】: 国家自然科学基金项目(40771214;40872029);; 中国科学院知识创新工程重要方向项目(kzcx2-yw-104)
【CateGory Index】: S718.5
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