Grey characteristics of microbanding of stalagmite in Shihua Cave, Beijing and its climatic signification(I) - The study of microstructure of microbanding

Science in China, Series D: Earth Sciences

Volumn 41, Issue 2, 1998, Pages 151-157

  Qin, Xiaoguang ^a   Liu, Dongsheng ^a   Tan, Ming ^a   Li, Tieying ^b   Lü, Jinpo ^b   Gu, Zhaoyan ^a   Lü, Houyuan ^a   Ding, Zhongli ^a   Guo, Zhengtang ^a   Liu, Jiaqi ^a   Nie, Gaozhong ^c  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b Beijing Geological Survey   (China)

^c INSTITUTE OF GEOLOGY   (China)

Author keywords

Grey of microbanding; Microstructure; Stalagmite

Indexed keywords

MICROSTRUCTURE; PALAEOCLIMATE; STALAGMITE;

CHINA, BEIJING, SHIHUA CAVE;

EID: 0031868449     PISSN: 10069313     EISSN: None     Source Type: Journal    
DOI: 10.1007/BF02932434     Document Type: Article

References (5)

1. Liu Tungsheng, Tan ming, Qin Xiaoguang et al., Discovery of microbedding in speleothems in China and its significance in the study of global change, Quaternary Sciences (in Chinese), 1997, (1):41.
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3. Baker, A., Smart, P. L., Edwards, R. L. et al., Annual growthy banding in a cave stalagmite, Nature, 1993, 364:518.
4. Shopov, Y. Y., Ford, D. C., Schwarcz, H. P., Luminescent microbanding in speleothems: high-resolution chronology and paleoclimate, Geology, 1994, 22:407.
5. Chen Longxun, Zhu Qiangen, Luo Huibang, Eastern Asian Monsoon (in Chinese), Beijing: China Meteorological Press, 1991, 197.