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우종윤 ( Jong Yoon Woo ) 충북대학교 사학회 2011 忠北史學 Vol.26 No.-
Donghak Peasants` Army`s exhumation is staying at basic grade because it have currently finished only 4 cases. Through analysis of exhumed 4 cases in nationalwide, we systematized exhuming procedure and progressive research, and checked it`s meaning of scholar the process of exhumation. Donghak Peasants` Army`s exhumation provides us with useful scholar information for understanding man who lived its time through finding historical fact, checking identity, recovery honor, and exhumed corpse. And various meterials of exhumation inherit Donghak Peasants`s ideology, it is valuable material about education, study, and pushing forward enhancement project. Therefore the basic research of Donghak Peasants` Army`s exhumation and exhumation need consistant process.
중원문화권안의 새로운 선사유적 (1) - 옥천지역 구석기유적을 중심으로 -
이융조 ( Yung Jo Lee ),우종윤 ( Jong Yoon Woo ),김우성 ( Woo Seong Kim ) 한국고대학회 2002 先史와 古代 Vol.17 No.-
The 8 sites newly discovered at Okcheon Area have been scrutinized so far. Following table is on those and artifacts. ◁표 삽입▷(원문을 참조하세요) Through these site and artifacts, we figure some characteristics out. First, each location of those sites has common aspect that they in end of ridgeline, where Kum-River flows U-shaped. And there are relatively large ground. With these factors, it is though that those areas could provide good condition with Paleolithic people. Moreover, all sites but Deodeok-I site were found within submerging line by Daecheong Dam(80m above sea level), and were identified to be located from 65 to 80m above sea level. In this region, because paleosol and geological terrace have developed to large extent, it seems that another Paleolithic site are likely to be found. Second, variety of raw material is quartz·quartzite, and any other peculiar material was not found. Most of them are round pebbles that can be easily obtained around sites. As it, is assumed that the area where raw material had been obtained was qualified to the Kum riverside. Third, retouched artifacts are mostly cores. On the contrary to that only one retouched tool with obvious characteristic of flake, all the other artifacts are cores but 2 pieces. Even though only limited surface-survey was conducted, that aspect can show certain characteristics of the sites. Forth, types of stone artifacts are relatively various that large and heavy artifacts have great portion(87.5%). Particularly, 12 pieces of bolas-stone and cores were found that it show good possibility that tool-making behaviors had been done in there. Besides, judging from technology and typology of artifacts, there is no artifact with upper Paleolithic characteristic, that it is though upper Paleolithic is not central phase. Near to upper stream of Kum river that occupies southem part of Jungwon region region, there has not been any excavation of paleolithic site, but just possibility of being paleolithic site has been suggested so far. However, this surface-survey presented remarkable result that 8 new paleolithic site were discovered. And it is expected that more extensive research would provide novel information on this region. Until now, there were 6 excavation for Kum-riverside of Jungwon Region that they were concentrated on the inland rather than area by main stream of Kum-River. In the situation, this survey has obtained excellent results, in that it gives the opportunity to understand the entity of paleolithic culture in Kum-riverside of Jungwon Region. However, those sites are location in submerged area by Daecheong Dam that paleosol·geological terrace has been damaged so rapidly. consequently, the excavation and further research is an urgency right now, so that the positive aid of governmental organization such as Water Resources Corporation should be needed.
금강 중류 구석기 유적의 제4기 지질 환경과 층서 고찰
김주용(Kim, Ju-Yong),양동윤(Yang, Dong-Yoon),이융조(Lee, Yung-jo),우종윤(Woo, Jong-yoon),홍세선(Hong, Se-Sun),이상헌(Yi, Sangheon),남욱현(Nahm, Wook-Hyun),이진영(Lee, Jin-Young),봉필윤(Bong, Phil-Yoon ),오근창(Oh, Keun-Chang),이승원( 한국구석기학회 2015 한국구석기학보 Vol.- No.32
금강 중류 유역의 하안단구 상면에서 사면프로세스와 연동된 여러 매의 사니질 고토양층은 구석기 인류의 삶의 증거가 포함되어 있다. 특히 청주 관내 오송 만수리, 옥산 소로리, 현도 노산리-하석리 일대 하안단구는 저위 I면(제2단구) 위에 하성퇴적층이 널리 발달하여 있다. 금강 중류 하안단구는 해발고도 약 30m 아래에 분포하는 하성 사력층은 전반적으로 최종빙기 초(약 60ka) 이후에 형성된 것으로 해석된다. 본 연구에서 검토한 3개 구석기 유적 지점에 나타나는 고토양층 형성은 만수리에서 약 45ka 이후(1지점 Q 28), 소로리에서 약 43ka 이후 (H-15 시추코아), 그리고 노산리에서 약 37ka(3지점 F5)~43ka(2지점 B-1)로 각각 나타나, 전반적으로 고토 양층의 형성은 플라이스토세 말 중에서도 주로 최종빙기 중기와 후기(MIS 3~2) 걸치는 것으로 해석되었다. 소로리에서 신기 하성퇴적층이 최종빙기최성기(MIS 2) 이후 뵐링-알러뢰드 간빙기에 걸쳐 형성되었다. 금강 중류의 3개 구석기 유적발굴 지점 토층단면의 고토양층에서 환경변화와 주기성에 대한 예비 결과, 대자율은 농갈 색이나 적갈색 고토양층 구간에서 증가하며, 갈색~암갈색 고토양층 구간에서는 상대적으로 낮아 지는 경향을 보이며, 대자율 상승 구간에서는 일반적으로 실트 함량이 증가(40~50 % 이상)함과 동시에 사질 함량은 감소 (20~30 이하)하는 경향을 강하게 지시하고 있다. 오송 만수리 1지점 대표단면(Q28칸)의 대자율 분포를 보면, 약 65,000년전 이후 약 만년주기의 하인리히 이벤트(H5~H3) 주기가 나타나는 것으로 간주되며, 금강 유역의 다른 구석기 유적에서도 나타나는지 추가 검토가 필요하다. A number of Paleosols, which contain relicts of the paleolithic peoples, are associated with slope-processed deposits on the fluvial terrace along the middle part of Keum River Basin, where Low Terrace-I(or 2nd Terrace) is prevailed with sand and gravel deposits, particularly at Mansuri(Osong-myeon), Sorori(Ogsan-myeon), and NosanriHaseogri(Hyeondo-myeon) in Cheongju City. Fluvial terrace deposits in middle part of Keum River are distributed below ca 30 m(asl) and interpreted to be formed after 60ka. Formation ages of paleosols of three paleolithic sites in this research are converged into the range between the MIS 2~MIS3 during the Last Glacial(Upper Pleistocene); Paleosols of Mansuri initially formed in the range of 45ka(Q28 pit in Loc. 1), Paleosols of Sorori formed after 43.6ka(H-15 core), and Paleosols of Nosanri after 37ka(F5 in Loc. 3). In Sorori site Young Fluvial Sequence(YFS) formed during the BøllingAllerød Interstadial after the Last Glacial Maximum(LGM). It can be manifested from the preliminary results of the soil-sedimentary profiles of three paleolithic sites that MS increases in reddish brown and dense brown Paleosols, while it decrease relatively in brown or dark brown Paleosols; MS increase is associated with both increasing silt fraction(> 40~50 wt %) and decreasing sand fraction(>20~30 wt %) in general. Lastly although it regards that the cyclicity of low MS peaks in the representative vertical profile(Q28) of Mansuri Loc. I site may be associated with the worldwide Heinrich events(H4~H6), it may be further examined from the other Paleosol profiles among the Paleolithic sites in the Keum River Basin.