• 제목/요약/키워드: daebo

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Precambrian Geology and Structure of the Central Region of South Korea

  • Kim, Ok Joon
    • 자원환경지질
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    • 제5권4호
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    • pp.231-239
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    • 1972
  • The central region of South Korea is composed of Precambrian formations and Jurassic Daebo granites and is divided tectonically into three provinces, that is, the Ok chon geosynclinal zone in the middle, the Kyonggi massif on the north and northwest side, and the Ryongnam massif on the south and southeast side. The general trend of the Okchon geosynclinal zone and the distribution of Daebo granites is northeast, the Sinian direction. The Kyonggi massif is composed of Precambrian Y onchon system, Sangwon system, gneisses, and Daebo granites, and the Ryongnam massif also Precambrian Ryongnam and Yulri systems, gneisses, and Daebo granites. Precambrian formations in both areas are of flysch type sediments and may be roughly correlated with each other. These formations except Sangwon and Yulri systems are thought to be early to middle Precambrian age and have acted as basement for the Okchon geosyncline where late Precambrian Okchon system was deposited. The Okchon geosynclinal zone is divided into paleogeosynclinal zone to southwestern parts where the Okchon system is distributed, and neogeosynclinal zone to northeastern parts where nonmetamorphosed Paleozoic sediments are dominantly cropped out. Both zones are separated by upthrust created by Daebo orogeny of Jurassic period, which continues southwesterly to bind the Okchon geosynclinal zone and the Ryongnam massif at southwestern parts bisecting Korea peninsula diagonally. Three periods of structural development are recognized in the area. Folds and faults of preTriassic age prevail in the Kyonggi massif. Many isoclinal folds and thrusts originated by Jurassic Daebo orogeny are aligned in the Okchon paleogeosynclinal zone paralleling to the geosynclinal axis so that same formation appears repeatedly in narrow strips, whereas fold axis in neogeosynclinal zone trerid west-northwesterly which might be of Triassic in age and modified by later Daebo orogeny. Discontinuity of geology and structure of Okchon geosynclinal zone is attributed to shifting of the geosyncline through geologic time.

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남한(南韓)의 신기화강암류(新期花崗岩類)의 관입시기(貫入時期)와 지각변동(地殼變動) (Study on the Intrusion Epochs of Younger Granites and their Bearing to Orogenies in South Korea)

  • 김옥준
    • 자원환경지질
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    • 제4권1호
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    • pp.1-9
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    • 1971
  • The "Younger Granites" in Korea were being believed to be late Cretaceous in age and named "Bulkuksa granites" by all previous works until the writer had discovered Jurassic granite in 1963. The present paper is to prove its validity by age dating on these granites which was carried out by Professor Y. Ueda, Tohoku University, Japan. The age of 37 granites samples from various localities ranges from 68 my to 181 my. Of these 10 samples belonged to early Jurassic, 6 samples to mid-Jurassic, 4 samples to late Jurassic, 5 samples to early Cretaceous, and 12 samples to late Cretaceous in age. It is of the writer's opinion that the granites intruded in from early Jurassic to early Cretaceous age belong to Daebo granites and are syntectonic plutons associated with Daebo orogeny, and only those of late Cretaceous age belong to Bulkuksa granites that were associated with Bulkuksa disturbance. Daebo granites are aligned along NE-SW Sinian direction in the middle parts of Korea and crop out in the cores of folded mountains which were formed by Daebo Orogeny, such as Charyong, Noryong, Sobaek, and Dukyu Ranges. On the contrary Bulkuksa granites are restricted in Kyongsang basin and adjacent few localities in distribution and show no alignment. Granites supposedly associated with other disturbances of post-precambrian Have not been found so far in S. Korea. Age dating of granites has revealed that Daebo orogeny might be continuous from Songrim distur bance of late Triassic age. From this viewpoint, it could be assumed that Daedong system of Jurassic age were deposited in separate intermontain basins while Daebo orogeny was active, so that Daedong system in separate localities in Korea could not been correlated in their lithology as well as stratig raphy.

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TMT 유도성 인지 기능 상실에 대한 대보(밤 품종) 내피 추출물의 효과 (Effect of Daebo (Castanea crenata) Inner Skin Extract on TMT-induced Learning and Memory Injury)

  • 김현주;정지희;조유나;진동은;진수일;김만조;허호진
    • 한국식품과학회지
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    • 제45권5호
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    • pp.661-665
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    • 2013
  • 본 연구에서는 국내 대표 밤 품종인 대보(Daebo)의 내피를 활용하여 TMT 유도성 인지 기능 상실에 대한 개선 효과를 연구하였다. 실험에서 각 농도별(5, 10, 20 mg/kg of body weight)로 대보 내피 에틸아세테이트 분획물을 섭취한 mouse를 TMT로 인지기능 손상을 유발하여 Y-maze test와 passive avoidance test한 결과, Y-maze test에서 분획물을 섭취한 group이 TMT 단독 처리군과 비교하였을 때 공간 인지기능을 개선시켰고, passive avoidance test 또한 latency time이 증가한 것으로 나타나 TMT에 의해 유발되는 뇌 신경독성 동물 모델로부터 기억 및 학습능력 개선 효과를 갖는 것으로 확인되었다. 또한 in vivo 동물 실험 후 mouse로부터 적출된 whole brain tissue를 대상으로 ex vivo AChE 활성 및 MDA 함량측정 실험한 결과, 에틸아세테이트 분획물이 TMT효과 대비 AChE의 활성을 일부 유의적으로 억제하는 것을 알 수 있었다. 결론적으로 대보 내피 에틸아세테이트 분획물은 신경전달물질인 AChE의 활성을 저해하고 뇌 신경세포 보호 효과를 통하여 인지기능 개선 효과를 유도할 수 있는 것으로 사료된다.

남한의 일부 중생대 화강암류의 지구화학적 연구 (Geochemical Study of Some Mesozoic Granitic Rocks in South Korea)

  • 김규한
    • 자원환경지질
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    • 제25권4호
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    • pp.435-446
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    • 1992
  • REE, major and trace elements analyses of the Jurassic Daebo granite and Cretaceous Bulguksa granite were carried out to interpet their petrogenesis and relationships between petrogenesis and tectonics. Analytical results are summarized as follows. (1) $SiO_2$ content of the Bulguksa granite (aver. 74.6%) are significantly higher than those of the Daebo granite (aver. 68.1%). Major elements of $TiO_2$, $Al_2O_3$, $P_2O_5$, CaO, MgO, Total FeO, and trace elements of Co, V and Sr are negatively correlated with $SiO_2$. Incompatible elements such as Ba, Sr, Y, Zr and HREE are contained differently in the Bulguksa granites distributed in between Okchon folded belt and Kyongsang sedimentary basin. (2) Trace element abundances show a good discrimination between two goups of granitic rocks. Ba, Sr and V are enriched in Daebo granites, while Zn and Cr are depleted in them. (3) Jurassic granites have quite different Eu anomalies and REE patterns from those of Cretaceous granites: Large negative Eu anomaly in the former and mild or absent Eu anomaly in the latter. The large Eu negative of Cretaceous granitic rocks are interpreted as a differentiated product of fractional crystallization of granitic magma from the upper mantle. Meanwhile, the Daebo plutonic rocks was resulted from the partial melting of subcrustal material or crustal contamination during ascending granitic magma from the mantle. Senario of igneous activities of Mesozoic age in South Korea was proposed based on Kula-Pacific ridge subduction model.

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십전대보탕(十全大補湯) 및 가미십전대보탕(加味十全大補湯)의 항산화 효과 및 신경교세포주 보호 효과 (Protective Effects and Anti-oxidative Effects of Sipjeon-Daebo-Tang and Gami-Sipjeon-Daebo-Tang in C6 Glioma Cell)

  • 이상영;김형우;김계엽;최찬헌;윤여충;정현우
    • 동의생리병리학회지
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    • 제23권6호
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    • pp.1292-1298
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    • 2009
  • Sipjeon-Daebo-Tang (SDT) is indicated for deficiency syndrome of both gi and blood, marked by pale or sallow complexion, dizziness, lassitude, shortness of breath, dislike for talking, poor appetite, pale tongue with thin whitish fur, thready and weak pulse. Gami-Sipjeon-Daebo-Tang(GSDT) is composed of 10 herbs within SDT and Cervi Pantotrichum Cornu (CPC). CPC can noursh kidney-yang, promote the production of the essence and blood, strengthen tendons and bones. Recently SDT is known as anti-cancer drug. Especially CPC is reported to have anti-oxidative action. For these reasons, we investigated the protective effects on cell death induced by chemicals such as paraquat, hydrogen peroxide and anti-oxidative effects in C6 glioma cells. In our results, GSDT accelerated proliferation rates of C6 cells in vitro. In addition, protective effects on cell death induced by hydrogen peroxide and rotenone. In addition, SOD activities were increased by treatment with both SDT and GSDT. In conclusion, these results suggest the possibility of GSDT to protect brain cell or neuronal cell from damage induced by oxidative stress. And also suggest that related mechanisms are involved in SOD activities.

고품질 쌀의 품종별 영양성분 및 취반 특성 (Nutritional Components and Cooking Characteristics of High Quality Rice)

  • 우관식;이석기;이병원;김정주;이지혜;이유영;이병규;김현주
    • 한국식품영양학회지
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    • 제31권2호
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    • pp.278-283
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    • 2018
  • The objective of this study was to evaluate quality properties of high quality rice. Seven rice varieties, Dabo, Daebo, Samkwang, Sindongjin, Sukwang, Jinsumi, and Haiami, were investigated for proximate contents and physicochemical characteristics. Moisture content was highest in the Jinsumi (13.13%). Protein and lipid content was highest in the Haiami. The amylose content of the rice cultivars was 20.15~22.51%. The degree of amylopectin polymerization (DP) was analyzed, and in all cultivars, DP 13-24 content was found to be highest, at more than 53%, whereas DP ${\geq}37$ content was lowest, at less than 5.81%. With regard to free sugar, maltose content in rice was the highest (${\geq}46%$). Toyo value of rice was highest in Samkwang, Daebo, and Jimsumi. Palatability characteristics were highest in Daebo and Jimsumi. Thus, the results of this study suggested that Samkwang, Daebo, and Jinsumi can be effectively used as processed cooked rice, though further studies should be required regarding changes in the quality of rice after cooking.

대보-구룡포-감포 지역의 해안단구(II) (Marine Terrace of Daebo-Guryongpo-Gampo, SE Korea(II))

  • 최성자
    • 자원환경지질
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    • 제37권2호
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    • pp.245-253
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    • 2004
  • 우리나라 남동해안의 대보-감포간 해안단구는 6개의 단구면으로 분류되며 이들은 각각 하위로부터 1단구(T1,0.5m), 2단구(T2, 10m), 3단구(T3, 30m), 4단구(T4, 40m), 5단구(T5, 60m), 6단구(T6, 75m)이다. 이가운데 3단구(T3)는 두개의 단구로 분류되며, 하위면을 T3b, 상위면을 T3a 정하였다. 3단구 하위면 (T3b)의 구정선을 보여주는 해식애의 발달이 뚜렷하지 않아 단구 세분이 어려운 곳은 통합하여 3단구(T3)로 정하였다. 단구형성시기를 직접적으로 지시해주는 화석은 없으나, 2단구의 퇴적층에서 OSL 연대 자료가 다량 도출되어 있으며, 이 자료를 통하여 단구 형성시기를 정할 수 있다. 2단구(T2) 퇴적층의 OSL 연대는 60-7Oka에 수렴하고 있어, 2단구의 형성시기는 MIS(산소동위원소에 의한 시대 분류)의 5a로. 추정할 수 있다. 따라서 3단구는 MIS 5e, 4단구는 MIS 7에 대비된다. 본 연구지역에서 MIS 5e인 3단구 상위면(T3a)은 현해수면으로부터 30m높게 융기되어 있으며, 따라서 이지역의 융기율은 약 0.19m/ka로 계산된다. 이와 같은 융기율은 국지적인 지구조운동에 기인한 것으로 해석되며, 이에 대한 추가 연구가 필요하다.

밤의 품종에 따른 Gallic acid 함량 비교분석 (Comparative Analysis of Gallic Acid Content by Chestnut Varieties)

  • 전홍남;박혜원;김동현
    • 한국산학기술학회논문지
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    • 제21권12호
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    • pp.362-368
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    • 2020
  • 본 연구에서는 밤의 품종(대보, 옥광, 축파, 삼조생)에 따른 Gallic acid 함량을 알아보았다. 밤나무 종류별로 알밤, 내피, 외피, 가지, 밤송이, 수꽃, 낙화수꽃의 추출물을 사용하여 HPLC로 정량분석하였다. Gallic acid의 동정은 표준품인 Gallic acid를 물에 녹여 100, 200, 250, 500ppm의 농도 범위에서 3회씩 분석하였고, 각 농도에서 피크면적비로 직선성을 확인하였다. 실험 기간은 2018년 5월부터 2019년 7월까지 진행했으며 밤 품종과 부위별 Gallic acid 함량을 확인한 결과는 다음과 같다. 밤에서 Gallic acid 함량은 축파가 0.0863%로 가장 높았고, 대보, 옥광, 삼조생순이었다. 밤나무의 부위별 Gallic acid 평균 함량에서는 낙화 수꽃에서 1.2100%로 가장 높았으며, 밤나무 잎, 밤송이, 가지의 순이었다. 내피에서는 대보 품종이 0.7463%로 가장 높았고, 축파, 옥광, 삼조생 순이었다. 외피에서는 삼조생품종이 0.4918%로 가장 높았고, 축파, 대보, 옥광 순이었다. 밤송이에서는 삼조생 품종이 1.3035%로 가장 높았고 대보, 축파, 옥광 순이었다.

보성(寶城)-순천(順天) 지역(地域)에 분포(分布)하는 정편마암류(正片麻岩類)의 지질시대(地質時代)와 성인(成因)에 대(對)한 연구(硏究) (Geochronology and Petrogenesis on Orthogneiss in the Bosung-Suncheon area)

  • 김용준
    • 자원환경지질
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    • 제21권1호
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    • pp.69-83
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    • 1988
  • Orthogneiss of the study area is meta-igneous complex that composed of granite gneiss, porphyroblastic gneiss and migmatitic gneiss. Migmatitic gneiss produced from granite gneiss and porphyroblastic gneiss by strong ductile shearing. These rocks show mostly gneissic and partly mortar textures by strong regional metamorphism and ductile shearing during several orogenies. $^{40}Ar-^{39}Ar$ incremental-release ages of these rocks have been determined for 1 hornblende. 1 biotite and 3 muscovite concentrates separated from orthogneisses in this area. Ages of regional metamorphism and ductile shearing of these rocks are more than 5 stages(1500 Ma, 260 Ma, 190 Ma, 180-170 Ma and 160 Ma) under $300^{\circ}C$ to $500^{\circ}C$. These rocks had not been nearly effected by Daebo orogeny, because this area is far from Daebo granite bodies. The general trend of major chemical composition and mineral composition of these orthogneisses suggest that these rocks are some series of differentiated products from magma.

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대보화강암내 함우라늄 광물의 산출특징과 존재형태의 중요성 (Characteristics of Uraniferous Minerals in Daebo Granite and Significance of Mineral Species)

  • 추창오
    • 한국광물학회지
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    • 제15권1호
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    • pp.11-21
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    • 2002
  • 지하수 중 우라늄이 높은 농도로 포함되어 있는 대보화강암 지역의 대수층구간에서 회수된 시추 코아에서 우라늄광물의 산출과 존재형태를 연구하였다. 우라늄광물은 일차적 기원으로 산출되며, 저어콘, 모나자이트, 제노타임 등과 같은 부성분 광물 내에 함유되는데 대부분 미량성분이나 포획물로 들어있다. 우라늄 광물은 $1~2mu$m 이하의 미림질의 결정으로 산출되므로 후방산란 전자영상(BSE)으로서도 구분이 매우 어렵다. 우라늄 광물을 포함하는 부성분 광물에서 이들이 빠져나간 용해동공이나 용해조직이 흔하게 관찰되는 것으로 보아 이들은 부분적으로 지하수로 용해되어 빠져나간 것으로 판단된다. 모암내의 우라늄함량과 지하수중 우라늄의 함량이 서로 별다른 관련성을 보이지 않는 사실은 우라늄광물이 용해될 수 있는 수리화학적 환경 외에도 우라늄 광물의 산출특징과 존재형태도 중요한 요소임을 지시해 준다.