Early labechiid stromatoporoids of the Yeongheung Formation (Middle Ordovician), Yeongwol Group, mideastern Korean Peninsula: Part I. Environmental distribution
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Park, Jino | - |
dc.contributor.author | Hong, Jongsun | - |
dc.contributor.author | Lee, Jeong-Hyun | - |
dc.contributor.author | Choh, Suk-Joo | - |
dc.contributor.author | Lee, Dong-Jin | - |
dc.date.accessioned | 2021-09-03T05:39:49Z | - |
dc.date.available | 2021-09-03T05:39:49Z | - |
dc.date.created | 2021-06-16 | - |
dc.date.issued | 2017-06 | - |
dc.identifier.issn | 1226-4806 | - |
dc.identifier.uri | https://scholar.korea.ac.kr/handle/2021.sw.korea/83316 | - |
dc.description.abstract | This study examines depositional facies and environmental significance of early labechiid stromatoporoids in the Yeongheung Formation (late Middle Ordovician), Yeongwol Group in the mideastern part of the Korean Peninsula. The formation is composed of five depositional facies: lime mudstone to wackestone (LM/W), peloidal, intraclastic and bioclastic packstone to grainstone (P/G), laminated dolomitic lime mudstone (LMdl), algal laminite (La), and oolitic packstone to grainstone (P/Go). Three types of shallowing upward cycles in the succession are identified, including subtidal (LM/W-P/G), subtidal to peritidal (LM/W-P/G-LMdl-La), and peritidal cycles (LMdl-La). The stromatoporoids occur exclusively in the packstone to grainstone (P/G) facies of the subtidal cycle. These early labechiids inhabited on a grainy substrate under moderate- to high-energy conditions, conforming to the previous notion that stromatoporoids primarily occupied level-bottom or reefs, surrounded by grainy calcareous sediments during the Middle Ordovician. | - |
dc.language | English | - |
dc.language.iso | en | - |
dc.publisher | GEOLOGICAL SOCIETY KOREA | - |
dc.subject | CARBONATES | - |
dc.subject | FACIES | - |
dc.subject | SEDIMENTATION | - |
dc.subject | LIMESTONE | - |
dc.subject | BIOHERMS | - |
dc.subject | ORIGIN | - |
dc.subject | REEFS | - |
dc.subject | ROCKS | - |
dc.subject | BASIN | - |
dc.title | Early labechiid stromatoporoids of the Yeongheung Formation (Middle Ordovician), Yeongwol Group, mideastern Korean Peninsula: Part I. Environmental distribution | - |
dc.type | Article | - |
dc.contributor.affiliatedAuthor | Choh, Suk-Joo | - |
dc.identifier.doi | 10.1007/s12303-017-0001-0 | - |
dc.identifier.scopusid | 2-s2.0-85018338238 | - |
dc.identifier.wosid | 000402868800001 | - |
dc.identifier.bibliographicCitation | GEOSCIENCES JOURNAL, v.21, no.3, pp.317 - 329 | - |
dc.relation.isPartOf | GEOSCIENCES JOURNAL | - |
dc.citation.title | GEOSCIENCES JOURNAL | - |
dc.citation.volume | 21 | - |
dc.citation.number | 3 | - |
dc.citation.startPage | 317 | - |
dc.citation.endPage | 329 | - |
dc.type.rims | ART | - |
dc.type.docType | Article | - |
dc.identifier.kciid | ART002228460 | - |
dc.description.journalClass | 1 | - |
dc.description.journalRegisteredClass | scie | - |
dc.description.journalRegisteredClass | scopus | - |
dc.description.journalRegisteredClass | kci | - |
dc.relation.journalResearchArea | Geology | - |
dc.relation.journalWebOfScienceCategory | Geosciences, Multidisciplinary | - |
dc.subject.keywordPlus | CARBONATES | - |
dc.subject.keywordPlus | FACIES | - |
dc.subject.keywordPlus | SEDIMENTATION | - |
dc.subject.keywordPlus | LIMESTONE | - |
dc.subject.keywordPlus | BIOHERMS | - |
dc.subject.keywordPlus | ORIGIN | - |
dc.subject.keywordPlus | REEFS | - |
dc.subject.keywordPlus | ROCKS | - |
dc.subject.keywordPlus | BASIN | - |
dc.subject.keywordAuthor | stromatoporoid | - |
dc.subject.keywordAuthor | labechiid | - |
dc.subject.keywordAuthor | late Middle Ordovician | - |
dc.subject.keywordAuthor | Yeongheung Formation | - |
Items in ScholarWorks are protected by copyright, with all rights reserved, unless otherwise indicated.
(02841) 서울특별시 성북구 안암로 14502-3290-1114
COPYRIGHT © 2021 Korea University. All Rights Reserved.
Certain data included herein are derived from the © Web of Science of Clarivate Analytics. All rights reserved.
You may not copy or re-distribute this material in whole or in part without the prior written consent of Clarivate Analytics.