Late Middle Cambrian (Cambrian Series 3) Trilobite Faunas from the Lowermost Part of the Sesong Formation, Korea and Their Correlation with North China
Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Choi, Duck K. | - |
| dc.contributor.author | Kim, Ji-Hoon | - |
| dc.contributor.author | Park, Tae-Yoon S. | - |
| dc.date.accessioned | 2018-03-20T14:04:40Z | - |
| dc.date.available | 2018-03-20T14:04:40Z | - |
| dc.date.issued | 2013 | - |
| dc.identifier.uri | https://repository.kopri.re.kr/handle/201206/6618 | - |
| dc.description.abstract | 그동안 잘 알려지지 않았던 세송층 최하부의 생층서대를 정확하게 정립하고 북중국과 정밀한 층서대비를 시도함. | - |
| dc.language | English | - |
| dc.title | Late Middle Cambrian (Cambrian Series 3) Trilobite Faunas from the Lowermost Part of the Sesong Formation, Korea and Their Correlation with North China | - |
| dc.type | Article | - |
| dc.identifier.bibliographicCitation | Choi, Duck K., Kim, Ji-Hoon, Park, Tae-Yoon S.. 2013. "Late Middle Cambrian (Cambrian Series 3) Trilobite Faunas from the Lowermost Part of the Sesong Formation, Korea and Their Correlation with North China". <em>JOURNAL OF PALEONTOLOGY</em>, 87(6): 991-1003. | - |
| dc.citation.title | JOURNAL OF PALEONTOLOGY | - |
| dc.citation.volume | 87 | - |
| dc.citation.number | 6 | - |
| dc.identifier.doi | 10.1666/13-010 | - |
| dc.citation.startPage | 991 | - |
| dc.citation.endPage | 1003 | - |
| dc.description.articleClassification | SCI | - |
| dc.description.jcrRate | JCR 2011:52 | - |
| dc.subject.keyword | Cambrian | - |
| dc.subject.keyword | Sesong Formation | - |
| dc.subject.keyword | Taebaeksan Basin | - |
| dc.subject.keyword | trilobite | - |
| dc.identifier.localId | 2013-0315 | - |
| dc.identifier.scopusid | 2-s2.0-84901020546 | - |
| dc.identifier.wosid | 000327359000003 | - |
- Appears in Collections
- 2012-2015, Paleogeographical, paleoenvironmental, and paleoecological researches of the Paleozoic fossils from the Taebaeksan Basin, Korea (12-15) / Park, Tae-Yoon S. (PN12090, PN13090, PN14090)
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