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.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.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.subject | Proterozoic | en |
| dc.subject.age | Precambrian::Proterozoic | en |
| dc.title | δ18O VALUES OF MUDROCKS: MORE EVIDENCE FOR AN 18O-BUFFERED OCEAN | |
| dc.type | Статья |