甘肃武都万象洞石笋双重光性微层特征

[1] 山东开元洞发现典型“北方型”石笋微生长层 [J]. 第四纪研究, 2010, 30 (02) : 441 - 442

[2] Asian summer monsoon precipitation recorded by stalagmite oxygen isotopic composition in the western Loess Plateau during AD1875―2003 and its linkage with ocean-atmosphere system[J]. Kathleen R. JOHNSON.Chinese Science Bulletin. 2008(13)

[3] 中国黄土高原西缘甘肃万象洞MIS5石笋δ18O记录与南方地区石笋记录的对比研究 [J]. 第四纪研究, 2006, (06) : 985 - 990

[4] Modern systematics and environmental significance of stable isotopic variations in Wanxiang Cave, Wudu,Gansu, China[J]. ZHANG Pingzhong1,Kathleen R.Johnson2,CHEN Yimeng1,CHEN Fahu1,Lynn Ingram2,ZHANG Xinli3,ZHANG Chengjun1,WANG Sumin4,PANG Fushun5 & LONG Lude5 1.Center for Arid Environment and Paleoclimate Research(CAEP) and Key Laboratory of Western China’s Environmental Systems,Ministry of Education,College of Earth and Environment Sciences,Lanzhou University,Lanzhou 730000,China;2.Department

[5] 石笋与环境——石笋纹层形成的环境机理初探 [J]. 中国岩溶, 1999, (03) : 3 - 11

[6] Bioptical microcycles of laminated speleothems from China and their chronological significance[J]. TAN Ming, QIN Xiaoguang, SHEN Linmei, WANG Xianfeng, WANG Yongjin, LI Tieying, SONG Linhua, WANG Laihong and LIU Dongsheng (LIU Tungsheng) 1. Laboratory of Speleothem and Paleoclimatology , Institute of Geology , Chinese Academy of Sciences , Beijing 100029, China;2. Benxi Scenic Spots Resources Administration Bureau, Benxi 117100, China;3. College of Geography , Nanjing Normal University, Nanjing

[7] 石笋微层物质组成的二次离子质谱初步分析及其气候意义 [J]. 第四纪研究, 1999, (01) : 59 - 66+97

[8] 洞穴碳酸钙微层理在中国的首次发现及其对全球变化研究的意义 [J]. 第四纪研究, 1997, (01) : 41 - 51+97

[9] Applications of stalagmite laminae to paleoclimate reconstructions: Comparison with dendrochronology/climatology[J] . Ming Tan,Andy Baker,Dominique Genty,Claire Smith,Jan Esper,Binggui Cai.Quaternary Science Reviews . 2006 (17)

[10] Speleothern luminescence intensity and spectral characteristics: Signal calibration and a record of palaeovegetation change[J] . Andy Baker,W.L. Barnes,Peter L. Smart.Chemical Geology . 1996 (1)

[1] 山东开元洞发现典型“北方型”石笋微生长层 [J]. 第四纪研究, 2010, 30 (02) : 441 - 442

[2] Asian summer monsoon precipitation recorded by stalagmite oxygen isotopic composition in the western Loess Plateau during AD1875―2003 and its linkage with ocean-atmosphere system[J]. Kathleen R. JOHNSON.Chinese Science Bulletin. 2008(13)

[3] 中国黄土高原西缘甘肃万象洞MIS5石笋δ18O记录与南方地区石笋记录的对比研究 [J]. 第四纪研究, 2006, (06) : 985 - 990

[4] Modern systematics and environmental significance of stable isotopic variations in Wanxiang Cave, Wudu,Gansu, China[J]. ZHANG Pingzhong1,Kathleen R.Johnson2,CHEN Yimeng1,CHEN Fahu1,Lynn Ingram2,ZHANG Xinli3,ZHANG Chengjun1,WANG Sumin4,PANG Fushun5 & LONG Lude5 1.Center for Arid Environment and Paleoclimate Research(CAEP) and Key Laboratory of Western China’s Environmental Systems,Ministry of Education,College of Earth and Environment Sciences,Lanzhou University,Lanzhou 730000,China;2.Department

[5] 石笋与环境——石笋纹层形成的环境机理初探 [J]. 中国岩溶, 1999, (03) : 3 - 11

[6] Bioptical microcycles of laminated speleothems from China and their chronological significance[J]. TAN Ming, QIN Xiaoguang, SHEN Linmei, WANG Xianfeng, WANG Yongjin, LI Tieying, SONG Linhua, WANG Laihong and LIU Dongsheng (LIU Tungsheng) 1. Laboratory of Speleothem and Paleoclimatology , Institute of Geology , Chinese Academy of Sciences , Beijing 100029, China;2. Benxi Scenic Spots Resources Administration Bureau, Benxi 117100, China;3. College of Geography , Nanjing Normal University, Nanjing

[7] 石笋微层物质组成的二次离子质谱初步分析及其气候意义 [J]. 第四纪研究, 1999, (01) : 59 - 66+97

[8] 洞穴碳酸钙微层理在中国的首次发现及其对全球变化研究的意义 [J]. 第四纪研究, 1997, (01) : 41 - 51+97

[9] Applications of stalagmite laminae to paleoclimate reconstructions: Comparison with dendrochronology/climatology[J] . Ming Tan,Andy Baker,Dominique Genty,Claire Smith,Jan Esper,Binggui Cai.Quaternary Science Reviews . 2006 (17)

[10] Speleothern luminescence intensity and spectral characteristics: Signal calibration and a record of palaeovegetation change[J] . Andy Baker,W.L. Barnes,Peter L. Smart.Chemical Geology . 1996 (1)