• Journal of the Korean Society of Food Science and Nutrition
• /
• v.31 no.2
• /
• pp.284-289
• /
• 2002

The effects of Okcheonsan powder on the body weights, the organ weights, the blood glucose level, the lipid and protein concentrations of serum and liver in diabetic rats were studied. Female rats (Sprague-Dawley, mean weight 313.6$\pm$18.5 g) were randomly assigned to one normal and two diabetic groups. They were fed experimental diets for 5 weeks. The diabetic groups were divided into the diabetic control (D-control group) and 3% Ok-cheonsan groups (D-Okcheonsan group). Rats were injected with streptozotocin intraperitoneally to induce diabetes. The body weights, the concentrations of total lipid and triglyceride of liver, the concentrations of total protein and albumin of serum in tole D-control and the D-Okcheonsan groups were significantly decreased compared with those in the normal group. The pancreatic weight in the D-control group was significantly more increased than that in the D-Okcheonsan group, but in the D-Okcheonsan group it was similar to that in the normal group. The fasting blood glucose levels and the atherogenic index in all the diabetic groups were significantly higher than those in the normal group. The concentrations of triglyceride, total cholesterol and LDL-cholesterol of serum, and the cholesterol of fiver in the D-Okcheonsan group were significantly lower than those in the D-control group. The concentration of HDL-cholesterol and HDL-cholestrol/total cholesterol ratio of serum were similar to those in all the groups. The concentrations of phospholipid of serum and liver in the D-Okcheonsan group were significantly decreased compared with those of the normal group, In conclusion, the Okcheonsan powder feeding could decrease the pancreatic weight, the concentrations of the triglyceride, the total cholesterol and LDL-cholesterol of serum, and the cholesterol of liver in the diabetic rats. But the concentrations of the blood glucose, the hepatic triglyceride and the atherogenic index seems to be not affected by it.

• Korean Journal of Oriental Medicine
• /
• v.11 no.2
• /
• pp.167-178
• /
• 2005

As a part of the quality control of herbal prescriptions which has been used for diabetes and related diseases, a reversed-phase liquid chromatographic method was developed for the simultaneous quantification of the three marker compounds, puerarin (Puerariae Radix), glycyrrhizin (Glycyrrhizae Radix), schizandrin (Schizandrae Fructus) in Oc Chun San. The HPLC analysis method was validated for parameters such as linearity, Limits of Detection(LOD), quantification(LOQ), repeatability, stability and recovery.

• Proceedings of the Mineralogical Society of Korea Conference
• /
• 2003.05a
• /
• pp.50-50
• /
• 2003

옥천변성대의 변성진화사를 밝히기 위한 많은 연구의 결과, 중온-중압형의 최고변성조건(약 490-63$0^{\circ}C$, 4.2-9.4 kbar)과 함께 시계방향의 압력-온도-시간 경로가 알려졌다. 이는 드러스트 나페에 의해 옥천변성대의 지각 두께가 증가했으리라는 제안과 일치한다. 하지만 변성작용에 관련된 조산운동을 규명하는데는 여러 가지 어려움이 남아 있다. 특히 변성시기에 대한 논란은 오랫동안 거듭되어 왔으며, 최근의 연구 결과는 옥천변성대의 최고변성작용 시기를 석탄기와 페름기의 경계 부근인 약 300-280 Ma로 규정짓는다. 또한 소위 황강리층의 화강암질 역에서 구한 SHRIMP U-Pb 저어콘 연대도 오차범위가 크긴 하지만, 석탄기의 열 사건을 지지한다. 이상의 연구결과는 지체구조적으로 중요한 의미를 지니며, 특히 옥천변성대와 태백산분지가 서로 다른 진화 과정을 경험한 별개의 지구조구임을 시사한다. 두 지구조구의 봉합은 약 250-220 Ma 사이에 이루어졌으리라 추정되지만, 보다 자세한 해석을 위해서 신뢰할만한 연대 자료의 축적이 필요하다. 그럼에도 불구하고, 이러한 결과들은 옥천대의 진화과정에 대한 기존의 생각과 일부 배치되며, 새로운 지체구조적 파라다임을 요구한다.

• Korean Journal of Food Science and Technology
• /
• v.47 no.2
• /
• pp.158-163
• /
• 2015

Fustin comprised >98 and 73.0-86.7% of the total flavonoid content in the bark, and the stems and lignum of Rhus verniciflua, respectively. The butein, fisetin, and sulfuretin content varied between 0.31-2.17, 0.27-3.32, and 0.15-0.80 mg/g on a dry weight basis, respectively, in different parts of Rhus verniciflua. The urushiol content was 5.09-6.29, 55.05-56.30, and 0.38-0.39 mg/100 g on a dry weight basis in the stems, bark, and lignum, respectively. This showed that the bark of the tree had the highest urushiol content. C15:3 (pentadecatrienyl catechol), C15:1 (pentadecenyl catechol), and C15:2 (pentadecadienyl catechol) comprised 63, 33-35, and 2-3% of urushiol congeners in the tree bark, respectively.

• The Journal of the Petrological Society of Korea
• /
• v.11 no.3_4
• /
• pp.121-137
• /
• 2002

Metamorphic evolution of the Ogcheon metamorphic belt has been studied by many investigators for the past few decades. P-T conditions of the Ogcheon metamorphic belt were estimated as 4.2-9.4 kbar and $490-630^{\circ}C$, corresponding to the medium-pressure type. In addition, the clockwise P-T-t path suggests a crustal-thickening event in association with the formation of thrust nappes. However, some details on deformation and orogeny of the Ogcheon metamorphic belt have been ambiguous yet. Although the metamorphic age has been also equivocal, recent isotopic studies strongly suggest that the peak metamorphism in the Ogcheon metamorphic belt has occurred at ca. 300-280 Ma between Late Carboniferous and Early Permian. It is thus inferred that the Ogcheon metamorphic belt and the Taebaegsan basin have evolved as separate terranes and that both were sutured at ca. 250-220 Ma. These results are partly in contrast with those of previous workers and require a revised framework for tectonic evolution of the Ogcheon belt. In addition, it is likely that the Ogcheon belt is correlative with the Hida marginal belt and the Hida metamorphic belt.

• 한국석유지질학회:학술대회논문집
• /
• autumn
• /
• pp.65-65
• /
• 2000

• Proceedings of the KSEEG Conference
• /
• 1999.04a
• /
• pp.166-166
• /
• 1999

• Proceedings of the Petrological Society of Korea Conference
• /
• 2000.05a
• /
• pp.86-86
• /
• 2000

• Journal of the Speleological Society of Korea
• /
• v.5 no.6
• /
• pp.31-39
• /
• 1980

우리나라에는 캠브로-오오도비스(Cambro-Ordovician)기에 속하는 조선누층군의 대석회암통이 넓게 분포되어 있어 석회암지대 특유의 Karst지형을 이루는 곳이 많다. 본 논문의 연구대상지역은 고생대 캠브로-오오도비스기의 조선계 대석회암통에 속하는 옥천지향사의 북부태백산지구를 중심으로 한 석회암 분포지역 중에서 Sinkhole terrain이 비교적 잘 발달되고 해발고도가 상이한 3개 지역을 선정하였다.(중략)

• The Journal of the Petrological Society of Korea
• /
• v.21 no.2
• /
• pp.129-150
• /
• 2012

The tectonic evolution of the Central Ogcheon Belt has been newly analyzed in this paper from the detailed geological maps by lithofacies classification, the development processes of geological structures, microstructures, and the time-relationship between deformation and metamorphism in the Ogcheon, Cheongsan, Mungyeong Buunnyeong, Busan areas, Korea and the fossil and radiometric age data of the Ogcheon Supergroup(OSG). The 1st tectonic phase($D^*$) is marked by the rifting of the original Gyeonggi Massif into North Gyeonggi Massif(present Gyeonggi Massif) and South Gyeonggi Massif (Bakdallyeong and Busan gneiss complexes). The Joseon Supergroup(JSG) and the lower unit(quartzose psammitic, pelitic, calcareous and basic rocks) of OSG were deposited in the Ogcheon rift basin during Early Paleozoic time, and the Pyeongan Supergroup(PSG) and its upper unit(conglomerate and pelitic rocks and acidic rocks) appeared in Late Paleozoic time. The 2nd tectonic phase(Ogcheon-Cheongsan phase/Songnim orogeny: D1), which occurred during Late Permian-Middle Triassic age, is characterized by the closing of Ogcheon rift basin(= the coupling of the North and South Gyeonggi Massifs) in the earlier phase(Ogcheon subphase: D1a), and by the coupling of South China block(Gyeonggi Massif and Ogcheon Zone) and North China block(Yeongnam Massif and Taebaksan Zone) in the later phase(Cheongsan subphase: D1b). At the earlier stage of D1a occurred the M1 medium-pressure type metamorphism of OSG related to the growth of coarse biotites, garnets, staurolites. At its later stage, the medium-pressure type metamorphic rocks were exhumed as some nappes with SE-vergence, and the giant-scale sheath fold, regional foliation, stretching lineation were formed in the OSG. At the D1b subphase which occurs under (N)NE-(S)SW compression, the thrusts with NNE- or/and SSW-vergence were formed in the front and rear parts of couple, and the NNE-trending Cheongsan shear zone of dextral strike-slip and the NNE-trending upright folds of the JSG and PSG were also formed in its flank part, and Daedong basin was built in Korean Peninsula. After that, Daedong Group(DG) of the Late Triassic-Early Jurassic was deposited. The 3rd tectonic phase(Honam phase/Daebo orogeny: D2) occurred by the transpression tectonics of NNE-trending Honam dextral strike-slip shearing in Early~Late Jurassic time, and formed the asymmetric crenulated fold in the OSG and the NNE-trending recumbent folds in the JSG and PSG and the thrust faults with ESE-vergence in which pre-Late Triassic Supergroups override DG. The M2 contact metamorphism of andalusite-sillimanite type by the intrusion of Daebo granitoids occurred at the D2 intertectonic phase of Middle Jurassic age. The 4th tectonic phase(Cheongmari phase: D3) occurred under the N-S compression at Early Cretaceous time, and formed the pull-apart Cretaceous sedimentary basins accompanying the NNE-trending sinistral strike-slip shearing. The M3 retrograde metamorphism of OSG associated with the crystallization of chlorite porphyroblasts mainly occurred after the D2. After the D3, the sinistral displacement(Geumgang phase: D4) occurred along the Geumgang fault accompanied with the giant-scale Geumgang drag fold with its parasitic kink folds in the Ogcheon area. These folds are intruded by acidic dykes of Late Cretaceous age.