Lin Yushi;ZhangMeiliang;Qin Jiaming.Study on the structure types of stalagmite lamina or lamella in cave[J].Carsologica Sinica,2001(01)
[2]
林玉石;张美良;覃嘉铭.洞穴石笋纹(壳)层构造类型研究[J].中国岩溶,2001(01)
[3]
Zhang Meiliang;ChengHai;Lin Yushi.High resolution paleoclimatic environment records from a stalagmite of Dongge cave since 15000 a in Libo,Guizhou Province,China[J].Geochimica,2004(01)
[4]
Zhang Meiliang;YuanDaoxian;Cheng Hai,The record of pa leoclimatic change from stalagmites and the determination of termination Ⅱ in the south of Guizhou Province,China,中国科学D辑(英文版),2003(11).
[5]
Zhang Meiliang;LinYushi;Qin Jiaming,The form combinations and dynamic conditions of dropping water of deposition laminate from stalagmites in caves,Journal of Southwest China Normal University(Natural Science),2001(04).
[6]
Zhang Meiliang;YuanDaoxian;Lin Yushi,Ages and paleoclimatic meanings of a stalagmite from Xiangshui cave at Guanyang county,Guilin,Carsologica Sinica,1998(04).
[7]
Yuan Daoxian;LiuZhaihu;Jiang Zhongcheng,The carbon cycle and karst geological environment,Beijing:Science Press,2003.
[8]
Yuan Daoxian;QinJiaming;Lin Yushi,High resolution paleoenvironmental reconstrction up to 200,000 years B.P.with speleothems from Guilin,Guangxi Teachers University Press,1999.
Qin Jianming;YuanDaoxian;Cheng Hai,The younger dryas and climate abrupt events in the Early and Middle Holocene:stalagmite oxygen isotope record from Maolan,Guizhou,China,中国科学D辑,2004(07).
[13]
Lin Yushi;ZhangMeiliang;Cheng Hai.The geological time scale and climatic events from stalagmites in the late or recent quaternary period in the Libo area,Guizhou,southwest China[J].Earth Science Frontiers,2003(02)
Lin Yushi;ZhangMeiliang;Qin Jiaming.Study on the sediment disconnected types of stalagmite in cave[J].Acta Geologica Sinica,2002(01)
[21]
Lin Yushi;ZhangMeiliang;Qin Jiaming.A study on the sedimentation rate of stalagmite in cave[J].Carsologica Sinica,2001(02)
[22]
张美良;程海;林玉石.贵州荔波15万年以来石高分辩率古气候记录[J].地球化学,2004(01)
[23]
Zhang Meiliang;YuanDaoxian;Lin Yushi,Isotopic ages and paleoclimatic implications of No.3 stalagmite from Dongge cave in Libo,Acta Sedimentologica Sinica(in Chinese),2001(03).
[24]
Yuan Daoxian;LiuZhaihu;Lin Yushi,Karst dynamic systems of China,北京:地质出版社,2002.
[25]
Tan Ming;QinXiaoguang;Sheng Linmei.The doubling light characteristics of the micro-cycles in speleothems in China and its significance in the study of global change[J].科学通报,1999(06)
QIN Xiaoguang;LiuDongsheng;Liang Handong,Preliminary analyses by Sims on trace components of stalagmite microla-yers and their climate ignificance,Quaternary Sciences,1997(01).
[29]
Qin Jiaming,Studies on stalagmite isotope records of paleoclimatic changes,Acta Geoscientia Sinica,1997(03).
[30]
Qin Jiaming;YuanDaoxian;Lin Yushi,Short-term abrupt climatie events of Last glaciation:The evidences from stalagmite records in Southwest China,Bulletin of Mineralogy,Petrology and Geochemistry,2001(04).
[31]
Qin Jiaming;YuanDaoxian;Lin Yushi.Records of high-resolution climate events from stalagmites since 160 000 a B.P.in Guangxi and Guizhou Provinces,China[J].Earth Science Frontiers,2001(01)
[32]
Liu Dongsheng;TanMing;Qin Xiaoguang,Discovery of microbedding in speleothems in China and its significance in the study of global change,Quaternary Sciences,1997(01).
