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Last glacial-Holocene geochronology of sediment cores from a high-altitude Tibetan lake based on AMS C-14 dating of plant fossils: Implications for paleoenvironmental reconstructions
Watanabe; T (Watanabe; Takahiro); Matsunaka; T (Matsunaka; Tetsuya); Nakamura; T (Nakamura; Toshio); Nishimura; M (Nishimura; Mitsugu); Izutsu; Y (Izutsu; Yasuhiro); Minami; M (Minami; Motoyasu); Nara; FW (Nara; Fumiko Watanabe); Kakegawa; T (Kakegawa; Takeshi); Wang JB(王君波); Zhu LP(朱立平); Watanabe, T
Source PublicationCHEMICAL GEOLOGY
2010
Volume277Issue:1-2Pages:21-29
Subject Area自然地理学
WOS IDWOS:000282861700002
Language英语
Indexed BySCI
KeywordATMOSPHERIC RADIOCARBON CALIBRATION EAST-ASIA SUMXI CO YR BP PLATEAU MONSOON CLIMATE CHINA QINGHAI ISOTOPE
Cooperation Status国际
Citation statistics
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/1367
Collection图书馆
Corresponding AuthorWatanabe, T
Recommended Citation
GB/T 7714
Watanabe,T (Watanabe,Takahiro),et al. Last glacial-Holocene geochronology of sediment cores from a high-altitude Tibetan lake based on AMS C-14 dating of plant fossils: Implications for paleoenvironmental reconstructions[J]. CHEMICAL GEOLOGY,2010,277(1-2):21-29.
APA Watanabe.,T .,Takahiro).,Matsunaka.,T .,...&Watanabe, T.(2010).Last glacial-Holocene geochronology of sediment cores from a high-altitude Tibetan lake based on AMS C-14 dating of plant fossils: Implications for paleoenvironmental reconstructions.CHEMICAL GEOLOGY,277(1-2),21-29.
MLA Watanabe,et al."Last glacial-Holocene geochronology of sediment cores from a high-altitude Tibetan lake based on AMS C-14 dating of plant fossils: Implications for paleoenvironmental reconstructions".CHEMICAL GEOLOGY 277.1-2(2010):21-29.
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