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pro vyhledávání: '"Loosli, Heinz Hugo"'
Autor:
Shedlovsky, Julian P., Honda, Masatake, Reedy, Robert C., Evans,, John C., Lal, Devendra, Lindstrom, Richard M., Delany, Anthony C., Arnold, James R., Loosli, Heinz-Hugo, Fruchter, Jonathan S., Finkel, Robert C.
Publikováno v:
Science, 1970 Jan . 167(3918), 574-576.
Externí odkaz:
https://www.jstor.org/stable/1728763
Akademický článek
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Autor:
Loosli, Heinz Hugo, Völkle, Hansruedi
Publikováno v:
Sozial- und Präventivmedizin/Social and Preventive Medicine; July 1991, Vol. 36 Issue: 4-5 p286-293, 8p
Autor:
Loosli, Heinz Hugo, Oeschger, Hans
Cosmic-ray produced atmospheric 39Ar activity (T1/2 = 269 yr) has been determined at 0.11 ±0.012 dpm/lt argon. Ice samples from two profiles in Greenland bore holes showed conclusively that 39Ar dating leads to correct ages. Corrections can be made
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a2020486ddf95691a64b543399d27c5
Autor:
Loosli, Heinz Hugo.
Publikováno v:
Solange vorrätig, können Sie diese Dissertation kaufen (für Bibliotheken evtl. auch Tauschexemplare erhältlich), hier anklicken.
Diss. Bern, 1968.
Externí odkaz:
http://www.ub.unibe.ch/content/bibliotheken_sammlungen/sondersammlungen/dissen_bestellformular/index_ger.html
Publikováno v:
Schlitzer, Reiner; Roether, Wolfgang; Weidmann, Urs; Kalt, Peter; Loosli, Heinz Hugo (1985). A meridional 14C and 39Ar section in northeast Atlantic deep water. Journal of Geophysical Research: Oceans, 90(C4), pp. 6945-6952. American Geophysical Union 10.1029/JC090iC04p06945
14C, 39Ar, and complementary hydrographic and nutrient data are presented for deep water below 2500 m depth, from stations along a meridional section (8°S to 45°N) through the Romanche Trench and along the deep northeast Atlantic basins (F/S Meteor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::95222364f3f7efb527bcad7fc7db9770
https://boris.unibe.ch/158710/1/schlitzer85jgr.pdf
https://boris.unibe.ch/158710/1/schlitzer85jgr.pdf
Autor:
author unknown
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