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Autor:
Volodymyr M. Kovalevych, Oleh Y. Petrychenko, Svitlana A. Zhukova, Tadeusz Marek Peryt, Torey Marshall
Publikováno v:
Precambrian Research. 144:39-51
Data on chemical composition of brines in primary inclusions of marine halites and on mineralogy of marine evaporites and carbonates lead to the conclusion that during the Phanerozoic two long-term cycles of chemical composition of seawater existed.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::022d4f4d0484bb00bda1ffe4317a73c2
https://doi.org/10.1016/j.precamres.2005.10.004
https://doi.org/10.1016/j.precamres.2005.10.004
