UPPER ORDOVICIAN SEQUENCES OF WESTERN ESTONIA
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dc.contributor.author | Harris M.T. | |
dc.contributor.author | Sheehan P.M. | |
dc.contributor.author | Ainsaar L. | |
dc.contributor.author | Rubel M. | |
dc.contributor.author | Hints L. | |
dc.contributor.author | Männik P. | |
dc.contributor.author | Nõlvak J. | |
dc.date.accessioned | 2022-11-07T07:47:47Z | |
dc.date.available | 2022-11-07T07:47:47Z | |
dc.date.issued | 2004 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=14041370 | |
dc.identifier.citation | Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 210, 2-4, 135-148 | |
dc.identifier.issn | 0031-0182 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/39580 | |
dc.description.abstract | The Upper Ordovician (uppermost Caradoc-Ashgill) section of western Estonia consists of a series of seven open-shelf carbonate sequences. Depositional facies grade laterally through a series of shelf-to-basin facies belts: grain-supported facies (shallow shelf), mixed facies (middle shelf), mud-supported facies (deep shelf and slope) and black shale facies (basin). Locally, a stromatactis mud mound occurs in a middle-to-deep shelf position. Shallow-to-deep shelf facies occur widely across the Estonian Shelf and grade laterally through a transitional (slope) belt into the basinal deposits of the Livonian Basin. | |
dc.subject | Ordovician | |
dc.subject | Stratigraphy | |
dc.subject | Sedimentology | |
dc.subject | Baltic | |
dc.subject | Estonia | |
dc.title | UPPER ORDOVICIAN SEQUENCES OF WESTERN ESTONIA | |
dc.type | Статья | |
dc.subject.age | Paleozoic::Ordovician | |
dc.subject.age | Палеозой::Ордовикская | ru |
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