LOWER DEVONIAN TENTACULITE BED IN THE SATUN AREA, SOUTHERN PENINSULAR THAILAND
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dc.contributor.author | Agematsu S. | |
dc.contributor.author | Sashida K. | |
dc.contributor.author | Salyapongse S. | |
dc.contributor.author | Sardsud A. | |
dc.date.accessioned | 2025-01-04T06:13:42Z | |
dc.date.available | 2025-01-04T06:13:42Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13855341 | |
dc.identifier.citation | Journal of Asian Earth Sciences, 2006, 26, 6, 605-611 | |
dc.identifier.issn | 1367-9120 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/47222 | |
dc.description.abstract | A Lower Devonian (Emsian) tentaculite fauna including Nowakia acuaria [Richer, R., 1854. Thüringische Tentaculiten. Zeitschr. Deutsch. Geol. Gesellsch. 6, 275-290] occurs in black shale in the basal part of a siliciclastic sequence exposed north of Satun, southern peninsular Thailand. Similar tentaculite beds with Nowakia have been reported from several areas in the Fang, Sri Sawat, and Trang areas of Thailand, the Langkawi Islands and the Mahang-Baling areas of Malaysia. The depositional environments in which the tentaculite-bearing black shale accumulated extended from modern northern Thailand to northwestern Malaysia during the Early Devonian (Emsian). © 2005 Elsevier Ltd. All rights reserved. | |
dc.subject | DEVONIAN | |
dc.subject | SATUN | |
dc.subject | TENTACULITE | |
dc.subject | THAILAND | |
dc.title | LOWER DEVONIAN TENTACULITE BED IN THE SATUN AREA, SOUTHERN PENINSULAR THAILAND | |
dc.type | Статья | |
dc.identifier.doi | 10.1016/j.jseaes.2004.12.002 | |
dc.subject.age | Paleozoic::Devonian::Lower::Emsian | |
dc.subject.age | Палеозой::Девонская::Нижний::Эмсский |
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