δ18O VALUES OF MUDROCKS: MORE EVIDENCE FOR AN 18O-BUFFERED OCEAN

dc.contributor.author	Land L.S.
dc.contributor.author	Lynch F.L.
dc.date.accessioned	2020-11-22T04:11:54Z
dc.date.available	2020-11-22T04:11:54Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=490328
dc.identifier.citation	Geochimica et Cosmochimica Acta, 1996, , 17, 3347-3352
dc.identifier.issn	0016-7037
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19256
dc.description.abstract	The whole-rock δ18O of mudrocks, as well as the δ18O of the clay-sized silicate fraction, does not change in any systematic manner over Paleozoic and late Proterozoic time. Therefore, the δ18O of the ocean has not changed (except a per mil or so as the result of glaciation/deglaciation) over the last billion years of Earth history.
dc.subject	Proterozoic	en
dc.subject	Paleozoic	en
dc.title	δ18O VALUES OF MUDROCKS: MORE EVIDENCE FOR AN 18O-BUFFERED OCEAN
dc.type	Статья
dc.subject.age	Докембрий::Протерозой	ru
dc.subject.age	Precambrian::Proterozoic	en
dc.subject.age	Paleozoic	en
dc.subject.age	Палеозой	ru

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