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Titlebook: Radiocarbon After Four Decades; An Interdisciplinary R. E. Taylor,Austin Long,Renee S. Kra Conference proceedings 1992 Springer Science+Bus

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書目名稱Radiocarbon After Four Decades
副標題An Interdisciplinary
編輯R. E. Taylor,Austin Long,Renee S. Kra
視頻videohttp://file.papertrans.cn/821/820705/820705.mp4
圖書封面Titlebook: Radiocarbon After Four Decades; An Interdisciplinary R. E. Taylor,Austin Long,Renee S. Kra Conference proceedings 1992 Springer Science+Bus
描述.Radiocarbon After Four Decades: An Interdisciplinary . .Perspective. commemorates the 40th anniversary of radiocarbon dating. The volume presents discussions of every aspect of this dating technique, as well as chronicles of its development and views of future advancements and applications. All of the 64 authors played major roles in establishment, development or application of this revolutionary scientific tool. The 35 chapters provide a solid foundation in the essential topics of radiocarbon dating: Historical Perspectives; The Natural Carbon Cycle; Instrumentation and Sample Preparation; Hydrology; Old World Archaeology; New World Archaeology; Earth Sciences; and Biomedical Applications.
出版日期Conference proceedings 1992
關鍵詞archaeology; carbon; climate change; earthquake; environment; evolution; gas; geoscience; hydrology; iron; mas
版次1
doihttps://doi.org/10.1007/978-1-4757-4249-7
isbn_softcover978-1-4757-4251-0
isbn_ebook978-1-4757-4249-7
copyrightSpringer Science+Business Media New York 1992
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Radiocarbon Fluctuations and the Geomagnetic Fieldver the past 40 years. The simultaneous pursuit of these fields of research was an important factor in the recognition of long-term radiocarbon fluctuations because a plausible physical mechanism was provided. This chapter will review both the paleomagnetic and radioisotope research that bears on th
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Solar Forcing of Global Climate Change?e millennia. These data have been summarized in the “Calibration Issue” of . (Stuiver & Kra 1986). Discrete Fourier Transform (DFT) power spectral analysis of the atmospheric .C variations, after removal of the longterm geomagnetic field-induced trend, reveals three fundamental periods. By using oth
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