volume 199 issue 4893 pages 583

Radiogenic and Atmospheric Argon Content of Tektites

Publication typeJournal Article
Publication date1963-08-01
scimago Q1
wos Q1
SJR18.288
CiteScore78.1
Impact factor48.5
ISSN00280836, 14764687
Multidisciplinary
Abstract
IN previous publications it has been shown that tektites can be dated by the potassium/argon method1–3. The potassium/argon ages give the time of their formation and also show which tektite localities belong together. It has been found that tektites from North America, the moldavites and tektites from Indo-China, Indonesia and from Australia form three independent strewn fields. The size of the strewn fields is of crucial interest to all hypotheses concerned with the origin of tektites. Therefore, these experiments have been extended with improved techniques and with a larger variety of samples. The results are given in Table 1.
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GOST Copy
Zähringer J., Gentner W. Radiogenic and Atmospheric Argon Content of Tektites // Nature. 1963. Vol. 199. No. 4893. p. 583.
GOST all authors (up to 50) Copy
Zähringer J., Gentner W. Radiogenic and Atmospheric Argon Content of Tektites // Nature. 1963. Vol. 199. No. 4893. p. 583.
RIS |
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RIS Copy
TY - JOUR
DO - 10.1038/199583a0
UR - https://doi.org/10.1038/199583a0
TI - Radiogenic and Atmospheric Argon Content of Tektites
T2 - Nature
AU - Zähringer, J.
AU - Gentner, W.
PY - 1963
DA - 1963/08/01
PB - Springer Nature
SP - 583
IS - 4893
VL - 199
SN - 0028-0836
SN - 1476-4687
ER -
BibTex |
Cite this
BibTex (up to 50 authors) Copy
@article{1963_Zähringer,
author = {J. Zähringer and W. Gentner},
title = {Radiogenic and Atmospheric Argon Content of Tektites},
journal = {Nature},
year = {1963},
volume = {199},
publisher = {Springer Nature},
month = {aug},
url = {https://doi.org/10.1038/199583a0},
number = {4893},
pages = {583},
doi = {10.1038/199583a0}
}
MLA
Cite this
MLA Copy
Zähringer, J., and W. Gentner. “Radiogenic and Atmospheric Argon Content of Tektites.” Nature, vol. 199, no. 4893, Aug. 1963, p. 583. https://doi.org/10.1038/199583a0.