• Title/Summary/Keyword: 석류

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선캠브리아 홍제사 화강암의 진화과정(한국 북동부지역의 원생대의 화성활동과 변성작용)

  • 김정민;조문섭
    • The Journal of the Petrological Society of Korea
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    • v.3 no.1
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    • pp.76-93
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    • 1994
  • The Precambrian Hongjesa granite is lithologically zoned from biotite granite in central part to biotite-muscovite granite towards the margin. The X_{Fe}$ (=Fe/(Fe+Mg)) value and the aluminum saturation index of biotite systematically vary as a function of mineral assemblage, and are positively related with those of bulk rock. This relationship as well as the lithological zoning are attributed to the fractional crystallization of the Hongjesa granitic magma. The trace element data corroborate that biotite-muscovite granite is more fractionated than biotite granite. The evolution of the Hongjesa granite is elucidated by using the AFM liquidus topology, where A=$Al_2O_3-CaO-Na_2O-K_2O$; F=FeO+MnO; and M=MgO. At an early magmatic stage where biotite is the only ferromagnesian mineral to crystallize, the X_{Fe}$ value and the alumina content of granitic magma continuously increase.. Muscovite subsequently crystallizes with biotite along the biotitemuscovite cotectic curve where biotite-muscovite granite forms. Local enrichments in Mn and B further crystallize garnet and tourmaline, respectively. The unique zonal pattern characterized by the occurrence of the evolved biotite-muscovite granite at the margin may be accounted for by the passive stoping during the emplacement of the Hongjesa granite. This emplacement may have occurred in continental collision environment, according to the tectonic discrimination diagram using major element chemistry.

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Microstructure Related to the Growth of Rare-earth Mineral in the Eoraesan Area, Chungju, Korea (충주 어래산 지역에서 희토류 광물의 성장과 관련된 미구조)

  • Kang, Ji-Hoon
    • The Journal of the Petrological Society of Korea
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    • v.28 no.2
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    • pp.129-141
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    • 2019
  • The Eoraesan area, Chungju, which is located in the northwestern part of Ogcheon Metamorphic Zone, Korea, mainly consists of the Neoproterozoic Gyemyeongsan Formation and the Mesozoic igneous rocks which intruded it. The metaacidic rocks (MAR) of the Gyemyeongsan Formation show a maximum radioactive value, and the Early Jurassic biotite granite is regionally distributed in this area. In this paper is researched the microstructure related to the growth of rare-earth mineral of allanite in the MAR, and is considered the source and occurrence time of rare-earth element (REE) mineralization. The MAR is mainly composed of alkalic feldspar (mainly microcline), quartz, iron-oxidizing mineral, biotite, muscovite, plagioclase, hornblende, allanite, zircon, epidote, fluorite, apatite, garnet, (clino)zoisite etc. The radioactive elements contained in the allanite cause a dark brown hale in the surrounding biotite, and the allinte also occurs as aggregate along the regional foliation. The deflection of regional foliation and the strain shadows, which are common to the pre-tectonic porphyroblast grown before the formation of regional foliation, can't be observed around most allanites (aggregates). The grain size and orientation of ironoxidizing mineral included in the allanite aggregate are the same as those in the matrix. It is recognized the hydrothermal conversion of hornblende to biotite due to the intrusion of igneous rock, and the secondary biotite occurs and contacts with allanite, zircon, epidote etc. These microstructures indicate that the rare-earth mineral of allanite (aggregate) grew by the hydrothermal alteration due to the intrusion of igneous rock after the formation of regional foliation. It is considered that the REE mineralization is closely related to the intrusion of Early Jurassic biotite granite which is regionally distributed in this area.

Effect of Fermented Natural Materials Mixtures with Lactobacilluse acidophilus on Anti-obesity Activity (유산균 발효 천연소재 혼합물의 항비만 효과)

  • Jeong, Hee Gyeong;Bak, Ok Ran;Kim, Kyung Je;Jin, Seong Woo;Koh, Young Woo;Im, Seung Bin;Ha, Neul-I;Seo, Kyoungsun
    • Proceedings of the Plant Resources Society of Korea Conference
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    • 2019.04a
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    • pp.103-103
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    • 2019
  • 최근 식생활의 변화로 인한 동물성 포화지방, 고칼로리 식품의 섭취 증가와 운동 부족, 스트레스 등의 여러 요인으로 비만인구 비율이 증가 추세를 보이고 있다. 유자, 석류등 천연소재 추출액에는 플라보노이드 성분이 풍부하여 항암, 항산화, 항염증, 항미생물 활성 등 생리활성이 있는 것으로 보고된 바 있다. 발효유로 대표되는 유산균 제품은 장 건강, 항산화 등 다양한 장점을 지니고 있으나, 짧은 유통기간 및 냉장유통 등 보존성에 있어 취약점을 가지고 있다. 따라서 천연 추출물을 주원료로 Lactobacillus acidophilus로 발효한 천연소재발효물을 활용하여 항비만 효과에 관한 연구를 수행하였다. 유산균 발효유의 풍미 유지하면서 유통기간을 늘릴 수 있는 가공법을 개발하고 건강식품 소재 개발 및 산업화를 통하여 국민의 건강 증진을 도모하고자 본 연구를 수행하였다. 천연소재 프로바이오틱스 발효물을 제조하여 세포독성, NO생성 억제능, 항비만 활성, 관능검사를 수행한 결과는 다음과 같다. 천연소재 추출물 및 천연소재추출발효혼합물을 각각 10, 50, 100, $500{\mu}g/mL$의 농도로 처리한 시험구들의 세포생존율을 측정한 결과 가장 고농도인 $500{\mu}g/mL$의 농도에서 각각 96.2, 95.1, 97.3, 96.2, 98.1, 97.0 %로 확인되어, 높은 수준의 안전성이 확인되었다. 천연소재 추출물 및 천연소재추출발효혼합물의 항염증효과를 분석하고자 수행한 Nitrite 생성저해 효과를 분석한 결과, NO 생성율은 $500{\mu}g/mL$의 농도에서 각각 98.1, 98.2, 96.2, 97.3, 91.2, 95.3 %로 확인되어 시험구 D의 항염증 활성이 가장 높은 것으로 나타났다. 동일한 농도로 처리하였을 때 lipid accumulation은 각각 100.0, 99.1, 98.2, 98.5, 87.6, 91.8 %로 나타나 D시험구와 E시험구에서 지방세포 분화억제효과가 확인되었다. 관능검사 시행 결과, 농축비율에 따른 관능적 기호도는 5 brix > 3 brix > 1 brix > 10 brix 순으로 나타났다.

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Spatio-Temporal Variation of Polymetallic Mineralization in the Wooseok Deposit (우석광상 다금속 광화작용의 시공간적 특성변화)

  • Im, Heonkyung;Shin, Dongbok;Jeong, Junyeong;Lee, Moontaek
    • Economic and Environmental Geology
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    • v.51 no.6
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    • pp.493-507
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    • 2018
  • The Wooseok deposit in Jecheon belongs to the Hwanggangri Mineralized Distict of the northeastern Ogcheon Metamorphic Belt. Its geology consists mostly of limestone of the Choseon Supergroup and the Cretaceous Muamsa granite intruded at the eastern area of the deposit. The deposit shows vertical occurrence of skarn and hydrothermal vein ores with W-Mo-Fe and Cu-Pb-Zn mineralization and skarn is developed only at lower levels of the deposit. Skarn minerals are replaced or cut by ore minerals in paragenetic sequence of magnetite-hematite, molybdenite-scheelite-wollframite, and higher abundances of pyrrhotite-chalcopyrite-pyrite-sphalerite-galena. Garnet has chemical compositions of $Ad_{65.9-97.8}Gr_{0.3-32.0}Pyr_{0.9-3.0}$, corresponding to andradite series, and pyroxene compositions are $Hd_{4.5-49.7}Di_{42.3-93.9}Jo_{0.5-7.9}$, prevailing in diopside compositions, both of which suggest oxidized conditions of skarnization. On the FeS-MnS-CdS ternary diagram, FeS contents of sphalerite in vein ores decrease with increasing MnS contents from bottom to top levels, possibly relating to W mineralization in deep and Pb-Zn mineralization in shallow level. Sulfur isotope values of sulfide minerals range from 5.1 to 6.8‰, reflecting magmatic sulfur affected by host rocks. W-Mo skarn and Pb-Zn vein mineralization in the Wooseok deposit were established by spatio-temporal variation of decreasing temperature and oxygen fugacity with increasing sulfur fugacity from bottom to top levels.

Mulseon-Jinsang Related Document Analysis in First Half of the 18th Century (18세기 전반 물선진상 관련 자료 분석 - 『진상별단등록』을 중심으로 -)

  • Jeon, Sang-wuk
    • Korean Journal of Heritage: History & Science
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    • v.47 no.4
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    • pp.178-191
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    • 2014
  • Jin-Sang is a local specialty donation to the palace. A local specialty donation to the palace is classified Jehyang, Bangmul, Mulseon, Medicine according to characteristic, when, use. Among these, Mulseon Jin-Sang is Most foods. And King was reduced Mulseon Jin-Sang in order to obtain a good image of the king. King Suk-Jong was frequently reduced Mulseon. But frequently changes of goods did not reflect to document. So type of goods, quantity is not clear in early 18th century. In 1728, King Yeong-Jo was published a Jingsangbyeldandngrok to clear type of goods, quantity. This book is written area, timing, quantity of Mulseon. Among these, type of goods, quantity are important. This book was written 176 kinds of goods. These goods was most of the fishery. And raw materials are largely accounted. In addition to processing the various creatures become like dried, pickled. By analyzing the regional allocation features, there are many types order by Gyeongsang-do, Hamgyeong-do. Gangwon-do. This area is faced east sea, so many fisheries have become records. In Gyeongsang-do, Cholla-do, these area were occupied a large portion of the fruit. And Jeju Island was assigned oranges. Finally, it has been assigned dried, pickled foods than living thing in distant area.

Geology and Mineralization of the Iscaycruz Pb-Zn-Cu Project, Central Peru (페루 중부 이스카이크루즈 연-아연-동 프로젝트의 지질 및 광화작용)

  • Heo, Chul-Ho;Nam, Hyeong-Tae
    • Korean Journal of Mineralogy and Petrology
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    • v.34 no.1
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    • pp.57-67
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    • 2021
  • The geology of the Iskaycruz project are mainly composed of sedimentary rocks within Cretaceous basin. The basal part is composed up of dark-gray shale, gray sandstone, and clastic rock of Oyon formation interbedded with coal measures. In the folded zone in the eastern part of the survey area, there is Chimu formation that has medium-grained massive and white quarztite. In terms of geological structure, the Iskaykruz region is located in the folded and overthrust zones of the central part of the Occidental Mountains. Ore body was formed by hydrothermal replacement process and consists of zinc, lead, silver, and copper. Stratabound-type deposits are hosted in limestone of Santa formation. It extends 12 kilometers discontinuously from northern Canaypata to southern Antapampa. Irregular iron oxide and sulfide minerals hosted in Santa and Parihuanca formations are observed. The mineralization observed on the surface consist of primary sulfides consisting of sphalerite with galena and chalcopyrite, and iron and manganese oxide produced from oxidation of primary sulfides. Skarn minerals are accompanied by tremolite, garnet, epidote and quartz.

SHRIMP Zircon U-Pb Ages of Basement Rocks in the Danyang National Geopark (단양 국가지질공원 기반암류의 SHRIMP 저어콘 U-Pb 연령)

  • Cheong, Wonseok;Han, Giun;Kim, Taehwan;Aum, Hyun Woo;Kim, Yoonsup
    • Korean Journal of Mineralogy and Petrology
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    • v.33 no.4
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    • pp.339-347
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    • 2020
  • We carried out the U-Pb age dating of zircon from basement rocks in the southern part of the Danyang National Geopark. Two migmatitic gneisses composed of biotite±sillimanite±garnet+feldspar+quartz were dated. Leucosomes in the samples were clearly distinguished from their melanosomes. The U-Pb isotopic compositions of zircon from sillimanite- and garnet-bearing migmatitic samples were measured using a secondary ion microprobe, yielding metamorphic ages, 1870±10 Ma (2σ)와 1863±6 Ma (2σ), respectively. 1.87~1.86 Ga metamorphic ages are consistent with those of the Paleoproterozoic low-P and high-T regional metamorphism (1.87~1.85 Ga) in the Yeongnam Massif. The maximum depositional age based upon the apparent 207Pb/206Pb ages of detrital zircon in the samples was estimated as 2.06 Ga, and thus sedimentation age of the protolith of the migmatitic gneisses ranges between 2.06 and 1.87 Ga.

Mantle Source Lithologies of Late Cenozoic Basaltic Rocks and Two Varieties of Enriched Mantle in the Korean Peninsula (한반도 신생대 후기 현무암의 근원 맨틀 암상과 두 종류의 부화 맨틀)

  • Choi, Sung Hi
    • Korean Journal of Mineralogy and Petrology
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    • v.35 no.3
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    • pp.183-197
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    • 2022
  • Geochemical data, including Sr-Nd-Pb-Mg-Zn isotopes, reported on the late Cenozoic intraplate basaltic rocks in the Korean Peninsula (Mt. Baekdu, Jeongok, Baengnyeong Island, Pyeongtaek, Asan, Ganseong, Ulleung Island, Dok Island, and Jeju Island) are summarized to constrain their mantle source lithologies, and the nature of mantle end-members required. In the Sr-Nd isotope correlation diagram, Jeju basalts plot in the field of EM2-type oceanic island basalts (OIB), while the other basalts fall in the EM1-type OIB field. In Pb-Pb isotope space, Jeju basalts show a mixing array between Indian MORB and EM2 component, whereas the other basalts display an array with EM1 component. The Korean basalts were derived from a hybrid source of garnet lherzolite and recycled stagnant slab materials (eclogite/pyroxenite, pelagic sediments, carbonates) in the mantle transition zone. The EM1 component could be ancient (~2.0 Ga) K-hollandite-bearing pelagic sediments that were isolated for a long period in the mantle transition zone due to their neutral buoyancy. The EM2 component might have been relatively young (probably Pacific slab) and recently recycled clay-rich pelagic sediments. Eclogite and carbonates are unlikely to account for the EM components, but they are common in the mantle source of the Korean basalts.

이온현미분석기를 사용한 남서부 경기육괴 변성암류의 U-Pb 저어콘 연대: 남중국지괴와의 대비 가능성

  • 조문섭
    • Proceedings of the Mineralogical Society of Korea Conference
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    • 2001.06a
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    • pp.141-142
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    • 2001
  • 남서부 경기육괴의 편마암류로부터 분리된 저어콘(zircon) 입자를 대상으로, 이온현미분석기(ion microprobe)를 사용한 U-Pb 연대를 구하였다. 그 결과는 후기 원생대(약 820 Ma) 뿐만 아니라 오르도비스기에 상당한 화성활동이 한반도에 있었음을 지시한다. 우리 나라 후기 원생대의 화성-변성 활동에 대해 알려져 있는 바는 극히 제한적이어서 후속연구가 필수적이며, 이러한 연구는 한반도의 지체구조적 변천사를 로디니아 초대륙(Rodinia supercontinent)의 생성-분리와 관련해 재조명할 수 있는 기회를 제공할 것이다. 또한 오르도비스기의 화성작용은 그동안 논란이 되어 왔던 소위 “칼레도니아(Caledonian)” 변동 (cf. 조문섭, 2000)에 대한 또 다른 증거를 제공해준다. 저어콘의 연대측정은 서호주의 커튼공업대학교에 설치되어 있는 SHRIMP-II(Sensitive High-Resolution Ion Microprobe-II; 고감도-고분해능 이온현미분석기)를 사용하였으며, 시료 준비 및 분석방법은 기존에 보고된 바와 같다 (e.g., Kinny et al., 1999). 분석된 3개의 암석 시료(1006-5, 8, 9)는 경기육괴의 남서부에 위치한 홍성 지역의 정편마암들이다. 1006-8 시료는 Turek and Kim (1996)이 전통적인 방법을 사용해 687$\pm$5 Ma의 U-Pb 저어콘 연대를 보고한 바 있는 화강암질 편마암 (시료번호, KJ43)에 해당된다. 두 개의 다른 시료는 1006-8 주변에서 산출하는 전형적인 경기육괴의 편마암류로서 화강암질 정편마암이다. 이들 시료로부터 분리된 저어콘 입자들은 대부분 화성기원의 누대구조와 자형의 결정형태를 보여준다. 과성장띠(overgrouth rims)는 1006-5 시료에서 흔하게, 그리고 1006-9 시료에서 매우 드물게 관찰된다. 음극선발광(cathodoluminescence) 영상의 해석을 통해 저어콘 결정의 성장사를 유추하였으며, 이를 바탕으로 이온현미분석 점(spot)을 정하였다. U-Pb-Th 자료는 퍼스(Perth) 저어콘 스탠다드 (CZ3, 564 Ma, $^{206}$Pb/$^{238}$U=0.0914)를 사용하였다. 아래에 기술하는 연대는 모두 $^{206}$Pb/$^{238}$U 연대에 해당된다. 두 개의 화강암질 편마암 시료로부터 구한 U-Pb 저어콘 연대는 각각 812 $\pm$ 14 Ma(1006-8)와 822 $\pm$ 17 Ma(1006-9)로 분석오차 내에서 서로 일치한다. 이 결과는 춘천 및 전곡 지역의 석류석 각섬암에서 보고된 Sm-Nd 전암연대(852 $\pm$ 24 Ma 및 824 $\pm$ 143 Ma; Lee and Cho, 1995; Ree et al., 1996)와 잘 부합한다. 따라서 후기 원생대 기간 중 화성활동이 한반도에서 광범위하게 일어났음을 시사한다. 한편, 1006-9 시료에서는 예외적으로 한 개의 저어콘 입자 주변부(rim)에서 매우 얇은 과성장띠가 관찰되었으며, 두 개의 점 분석으로부터 구한 U-Pb 저어콘 연대는 약 235 Ma이다. 이 띠는 또한 변성기원의 저어콘에서 흔히 관찰되는 작은 W (<0.05) 비를 보인다. 1006-5 시료는 위 두 시료로부터 수 km 떨어진 지점에서 채집하였으나, 저어콘 연대는 상이한 기록을 보여준다. 즉 매우 작은 Th/U (<0.01) 값을 갖는 저어콘의 주변부에서 223 $\pm$ 5 Ma의 연대가 잘 정의되며, 이는 1006-9 시료에서 관찰된 결과와 함께 트라이아스기의 고온변성작용이 백립암상에 가까운, 매우 높은 온도에 달하였음을 지시한다. 한편 저어콘의 중심부는 335-473 Ma의 비교적 넓은 연대 분포를 보인다. 이는 저어콘이 실제 성장한 연대를 지시하기보다는 트라이아스기의 변성작용에 따른 납손실(Pb loss) 그리고 누대 규모보다 더 큰 빔 크기(beam size, 약 30 $\mu\textrm{m}$)의 영향일 것으로 해석된다. 또한 저어콘이 다양한 외래물질로부터 기원했다는 증거가 관찰되지 않으므로, 이 정편마암의 모암은 오르도비스기(약 430-470 Ma)에 관입하였을 것으로 생각된다. 따라서 그동안 논란이 되어 왔던 소위 “칼레도니아” 변동이 한반도 내에 실존하였을 가능성을 시사한다. 이상의 결과를 종합하여 볼 때, 경기육괴의 변성암류는 후기 원생대 이후 다양한 저어콘의 성장사를 기록하고 있음을 알 수 있다: 즉 (1) 후기원생대(약 820 Ma)의 화성작용; (2) 오르도비스기(약 450 Ma)의 화성작용: 그리고 (3) 트라이아스기 (약 223 Ma)의 부분용융을 수반한 고온 변성작용으로 대표된다. 이러한 지질연대는, 옥천변성대에서 얻어진 756 Ma의 저어콘 연대(Lee et al., 1998)와 더불어, 친링-다비-수루(Qinling-Dabie-Sulu) 대륙 충돌대와 양쯔 지괴에서 보고된 지질연대 결과와 잘 부합한다. 따라서 지구연대학적으로 경기육괴가 북중국보다는 대륙충돌대를 포함하는 남중국지괴에 속할 것으로 결론지을 수 있다.

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Petrological Characteristics and Origin of Volcaniclasts within the Massive Tuff Breccia Formation from Dokdo Island, Korea (독도 괴상 응회질 각력암층에서 나타나는 화산암편의 암석학적 특성과 기원)

  • Shim, Sung-Ho;Im, Ji-Hyeon;Jang, Yun-Deuk;Choo, Chang-Oh;Park, Byeong-Jun;Kim, Jung-Hun
    • The Journal of the Petrological Society of Korea
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    • v.19 no.2
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    • pp.141-156
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    • 2010
  • Dokdo Island, Korea, is located in the East Sea belonging to back arc basin. In this study we examined petrology and geochemistry of massive tuffaceous breccia (MTB) from Dongdo (Eastern islet) and Seodo(Western islet), the two largest islands of Dokdo. Field studies and chemical analysis distinguish the MTB in Dongdo and Seodo. The Dongdo MTB (DMTB) is exposed up to 50 m on the ocean cliff and it has dominant basalt and trachybasalt with moderate amount of trachyte and scoria. On the other hand, Seodo MTB (SMTB), which is preserved between trachyte dike and trachyandesite, is composed of roughly equal amounts of basalt, trachybasalt and trachyte. The location of the islets were related to the source vent having in contact with underlying trachyte lava and differential pyroclastic deposits made them different characteristics. According to trace element analysis of trachytic volcanic clasts, the Ba concentration ranges from 66 to 103 ppm and Sr varies from 44 to 56 ppm in DMTB. However, Br and Sr in SMTB correspondingly showed relatively wide ranges: Br 785-1259 ppm and Sr 466-1230 ppm. These differential trends between DMTB and SMTB, along with the difference in P and Ti, indicate that the crystallization of alkali feldspar, feldspathoid, biotite, apatite and titanium took place differently. Nevertheless, DMTB and SMTB are similar in REE patterns and they are correspondingly characterized by high LREE, low HREE and similar $(La/Yb)_N$ values with 23.9-40.2 in DMTB and 27.4-32.9 in SMTB. These patterns suggest that Dongdo and Seodo might be originated from coeval magma suites. Dokdo island shows high concentrations of Ba, K and Rb. These signatures mark a result attributed to the mantle upwelling because the magma derived from the asthenosphere was metasomatized with subduction-related fluids.