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National Taiwan University Radiocarbon Measurements II

Published online by Cambridge University Press:  18 July 2016

Yuin-Chi Hsu
Affiliation:
Department of Physics, National Taiwan University, Taipei, Taiwan, China
Muh-Chen Chou
Affiliation:
Department of Physics, National Taiwan University, Taipei, Taiwan, China
Yi-Chuan Hsu
Affiliation:
Department of Physics, National Taiwan University, Taipei, Taiwan, China
Song-Yun Lin
Affiliation:
Department of Physics, National Taiwan University, Taipei, Taiwan, China
Shih-Chong Lu
Affiliation:
Department of Physics, National Taiwan University, Taipei, Taiwan, China
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The C14 dates given below have been obtained by counting CO2 at 2 atm pressure in a 1 L proportional counter. Details of procedure are given in our previous list (R., 1970, v. 12, p. 187–192). Radiocarbon dates in this list are based on 95% of activity of NBS oxalic acid as the modern standard and were calculated using 5570 yr as the half-life of C14. Errors quoted with the dates are standard deviation originating from the statistical nature of radioactive disintegration process. Results obtained during 1970 and 1971 are described here.

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Research Article
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Copyright © The American Journal of Science 

References

Hsu, Y. C. et al., 1970, National Taiwan University radiocarbon measurements I: Radiocarbon, v. 12, p. 187192.CrossRefGoogle Scholar
Lin, C. C., 1967, Quaternary of Taiwan VIII, Quaternary system of the Hengchun Peninsula: Rept., Natl. Council on Sci. Development.Google Scholar
Lin, C. C., 1969, Holocene geology of Taiwan: Acta Geol. Taiwanica, no. 13, Dec., p. 83126.Google Scholar
Sung, W. H., 1969, Changpin: a newly discovered Preceramic culture from the Agglomerate Caves on east coast of Taiwan: Newsletter Chinese Ethnol., no. 9.Google Scholar
Yamaguchi, S. and Lin, T. H., 1971, The decision of moving cycle of landslide in past time by the age measurement of bogwood obtained from landslide area: Landslide, v. 7, p. 16.Google Scholar
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