Lake Shira Level Changes in Late Holocene  

作　　者：Anrey DARIN Ivan KALUGIN Natalya MAKSIMOVA Tatiana MARKOVICHv Yakov RAKSHUN Dmitryi SOROKOLETOV Fedor DARIN Denis RAGOZIN 

机构地区：[1]Institute of Geology and Mineralogy SB RAS [2]Institute of Nuclear Physics SB RAS [3]Institute of Biophysics SB RAS

出　　处：《Acta Geologica Sinica(English Edition)》2014年第S1期3-4,共2页地质学报（英文版）

基　　金：supported by the RFBR projects 13-05-00871,14-02-00631

摘　　要：1 Introduction Meromictic Shira Lake is a good represfor detail climate modeling due to its locainformation and annually laminated bottomsediment column of 155 cm in length wahammer corer in the deepest(24 m)central in 2009.2 Sample Preparations and Measuring1 Introduction Meromictic Shira Lake is a good represfor detail climate modeling due to its locainformation and annually laminated bottomsediment column of 155 cm in length wahammer corer in the deepest(24 m)central in 2009.2 Sample Preparations and Measuring

关 键 词：Lake Shira VARVE synchrotron radiation scanning X_ray fluorescence microanalysis. 

分 类 号：P534.632[天文地球—第四纪地质学] P343.3[天文地球—古生物学与地层学]