• Economic and Environmental Geology
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• v.49 no.4
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• pp.249-267
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• 2016

The Hongseong area of the central-western Korean Peninsula is considered to be a part of collision zone that is tectonically correlated to the Qinling-Dabie-Sulu belt of China. The area includes the elliptical-shaped serpentinized ultramafic bodies, together with mafic rocks. The studied bodies are in contact with the surrounded Neoproterozoic alkali granites at the Baekdong and Wonnojeon bodies and the Paleoproterozoic Yugu gneiss at the Bibong body. The Baekdong body contains the blocks of the Neoproterozoic alkali granites and the Late Paleozoic metabasites. The Bibong body also includes the Neoproterozoic alkali granite blocks. The Mesozoic intrusive rocks are also recognized at the Baekdong, Wonnojeon and Bibong bodies. On the other hand, the Early Cretaceous volcanic rocks are occurred at the Bibong body. The detrital zircon SHRIMP U-Pb ages of the serpentinites at three bodies range variously from Neoarchean to Middle Paleozoic at the Baekdong body, and from Neoarchean to Early Cretaceous at the Wonnojeon and Bibong bodies. Although serpentinization does not generally produce minerals suitable for direct isotopic dating, the youngest Middle Paleozoic age at the Baekdong body and the Early Cretaceous age at the Wonnojeon and Bibong bodies indicate the possible upper age limit for the (re)serpentinization. Especially, the Early Cretaceous serpentinization ages may be related to the widespread Early Cretaceous igneous activity in the central-southern Korean Peninsula. Age results for the serpentinite bodies and the included blocks of the studied serpentinized ultramafic bodies in the Hongseong area, therefore, provide several possible interpretations for the serpentinization ages of the ultramafic rocks as well as the geotectonic implications of serpentinization, requiring more detailed study including other serpentinized ultramafic bodies in the Hongseong area.

• 월간산업보건
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• s.107
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• pp.2-10
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• 1997

직업성 피부질환은 1988년 미국 전체 직업성 질환중 20%에 해당된다(미 노동부 자료 참고). 그 비율은 주에 따라 크게 달라지기도 한다. 피부질환은 어떤 주에서는 보상되는 직업성 질환의 대다수를 차지하기도 한다; 예를 들어, 캘리포니아와 플로리다주에서는 농작물에 의한 접촉성 피부염이 흔하다. 접촉성 피부염은 직업성 피부질환으로 보고되는 가장 흔한 피부질환이다. 이러한 사례의 4/5는 유기용제, 절삭유, 세척유, 알칼리, 산 등과 같은 자극성 화학물질에 대한 노출과 관련이 있다. 자외선은 어떤 화학물질(예를 들면, 코울 타르, 크레오소오트)과 반응하여, 이 화학물질 및 빛에 노출되는 부위에 자극성 접촉성 피부질환을 유발하기도 한다. 1/5의 사례는 에폭시 수지, 크롬, 식물 수지, 그 밖의 많은 것 등 특수 접촉 감광제와 관련될 수 있다. 강한 자극제에 노출되어 발상하는 화학적 화상은 비교적 흔하게 일어난다. 백반과 유사한 피부탈색은 드물게 일어나며 피부 접촉을 통하여 야기하는 특수 화학물질과 관련될 수 있다. 여드름과 모낭염은 기름 및 유지들과의 피부 접촉을 통하여 생겨날 수 있다. 10대 여드름과 구별되는 염소성 여드름이라고 불리는 질환은 여러 종류의 염화 탄화수소들(예를들면 다브롬화 디페닐, 다염화 디페닐, 디옥신)에 노출되어 발생되기도 한다. 신체적인 손상으로 반복되는 외상부위에 가골이 형성되기도 한다. 여러 종류의 일에 특징적인 것(예를 들면 바이올린 연주자의 목에 가골)이 소위 "직업적인 표지" 이다. 전기톱 작동 기술자, 분쇄기 작동기술자, 지하 광산 암석 천공 기술자에게서 발생하는, 손 - 팔 부위의 진동은 오랜기간 혹은 심하게 노출된 노동자에 있어서 - 손에 혈관수축질환 - 진동장애 백색 수지질환을 일으킬 수 있다. 피부암은 직업과 관련이 있다고 할 수 있다. 하지만 몇몇 사례가 산재 관련 기관에 보고외어 있지만, 암등록소에 보고는 불완전하며, 피부암으로 인한 사망은 드물기 때문에 피부암의 발생률은 알 수 없다. 예방적인 방법은 개인보호구(장갑, 구두 등), 기계공학적 통제, 노동자 교육, 피부에 노출되는 것을 피하기 위해 주어진 일을 맡는 노동자들의 교대와 같은 관리적인 통제가 있다. 이러한 방법들은 화학적 화상, 알러지성 접촉성 피부염과 같은 피부염, 진동장애, 직업관련성 질환(예를 들면, 건선, 단순태선, 백반)을 예방하는데 도움이 된다. 만성 자극성 접촉성 피부염은 아직 잘 이해하고 있지 못하여 현재 예방하는 방법은 아직 만족스럽지 못하다.

• 월간산업보건
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• s.105
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• pp.16-25
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• 1997

직업성 피부질환은 1988년 미국 전체 직업성 질환중 20%에 해당된다(미 노동부 자료 참고). 그 비율은 주에 따라 크게 달라지기도 한다. 피부질환은 어떤 주에서는 보상되는 직업성 질환의 대다수를 차지하기도 한다; 예를 들어, 캘리포니아와 플로리다주에서는 농작물에 의한 접촉성 피부염이 흔하다. 접촉성 피부염은 직업성 피부질환으로 보고되는 가장 흔한 피부질환이다. 이러한 사례의 4/5는 유기용제, 절삭유, 세척유, 알칼리, 산 등과 같은 자극성 화학물질에 대한 노출과 관련이 있다. 자외선은 어떤 화학물질(예를 들면, 코울 타르, 크레오소오트)과 반응하여, 이 화학물질 및 빛에 노출되는 부위에 자극성 접촉성 피부질환을 유발하기도 한다. 1/5의 사례는 에폭시 수지, 크롬, 식물 수지, 그 밖의 많은 것 등 특수 접촉 감광제와 관련될 수 있다. 강한 자극제에 노출되어 발상하는 화학적 화상은 비교적 흔하게 일어난다. 백반과 유사한 피부탈색은 드물게 일어나며 피부 접촉을 통하여 야기하는 특수 화학물질과 관련될 수 있다. 여드름과 모낭염은 기름 및 유지들과의 피부 접촉을 통하여 생겨날 수 있다. 10대 여드름과 구별되는 염소성 여드름이라고 불리는 질환은 여러 종류의 염화 탄화수소들(예를들면 다브롬화 디페닐, 다염화 디페닐, 디옥신)에 노출되어 발생되기도 한다. 신체적인 손상으로 반복되는 외상부위에 가골이 형성되기도 한다. 여러 종류의 일에 특징적인 것(예를 들면 바이올린 연주자의 목에 가골)이 소위 "직업적인 표지" 이다. 전기톱 작동 기술자, 분쇄기 작동기술자, 지하 광산 암석 천공 기술자에게서 발생하는, 손 - 팔 부위의 진동은 오랜기간 혹은 심하게 노출된 노동자에 있어서 - 손에 혈관수축질환 - 진동장애 백색 수지질환을 일으킬 수 있다. 피부암은 직업과 관련이 있다고 할 수 있다. 하지만 몇몇 사례가 산재 관련 기관에 보고외어 있지만, 암등록소에 보고는 불완전하며, 피부암으로 인한 사망은 드물기 때문에 피부암의 발생률은 알 수 없다. 예방적인 방법은 개인보호구(장갑, 구두 등), 기계공학적 통제, 노동자 교육, 피부에 노출되는 것을 피하기 위해 주어진 일을 맡는 노동자들의 교대와 같은 관리적인 통제가 있다. 이러한 방법들은 화학적 화상, 알러지성 접촉성 피부염과 같은 피부염, 진동장애, 직업관련성 질환(예를 들면, 건선, 단순태선, 백반)을 예방하는데 도움이 된다. 만성 자극성 접촉성 피부염은 아직 잘 이해하고 있지 못하여 현재 예방하는 방법은 아직 만족스럽지 못하다.

• The Journal of the Petrological Society of Korea
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• v.24 no.1
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• pp.25-54
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• 2015

Syenite is not a common rock, unlike granitic rocks formed the major component of the continental crust. The aim of this study is to decipher the occurrences and detailed descriptive characteristics of the syenite distributed in Sancheong area, and to investigate the petrogenesis of the syenitic magma based on geochemical study. The dominant minerals in syenite are alkali feldspar (usually orthoclase and rarely microcline), plagioclase, amphibole, biotite, and quartz. Syenites are found in a wide variety of colors. The anhedral hornblende and biotite filling the boundary of feldspar and quartz indicate that the hydrous minerals were crystallized lately, and that water was insufficient at the beginning of crystallization in magma. According to the analysis of mineral composition, amphibole in syenite is mostly ferro-edenite, and the pressure is calculated as 3.3~4.9 kb with 11.9~17.3 km of emplacement depth. Biotite and pyroxene are plotted in the region of annite and hedenbergite, respectively. Based on petrochemical studies of major elements, syenite belongs to alkaline series, metaluminous, and I-type. On the other hand, the variation patterns of trace and rare earth elements of syenite differ from the patterns of diorite and granite. In the geochemical characteristics, syenite is different from gabbro-diorite spatially adjacent to syenite, as well as granite. These results suggest that each rock has been generated from the different sources of magma. Additionally, based on the experimental data, the syenitic magma can be formed (1) by the partial melting at a high pressure and dry system, (2) when the initial crystallization minerals to be residue with migration of the residual melts separated from the ascending cotectic magma (3) when fluorine compositions to be plentiful in the protolith and/or at depth of the magma. Based on the petrographic characteristics of the syenite, Sancheong syenitic magma may have been formed by partial melting in a dry system.

• Journal of the Korean earth science society
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• v.21 no.1
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• pp.67-80
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• 2000

We studied petrological and geochemical characteristics of the Mesozoic volcanic rocks in the Da Hinggan Ling area northeast China, and discussed tectonic settings and origin of the Mesozoic volcanic rocks in northeast Asia. Volcanic rocks in Da Hinggan Ling area are composed of alkaline to subalkaline basalt-basaltic andesite-andesite-dacite-rhyolite, showing typical BAR(basalt-andesite-rhyolite) association. However, most of the volcanic rocks are basaltic and rhyolitic in composition, and andesitic rocks are relatively rare, which shows bimodal characteristics. Rb, Ba, Th and other incompatible element contents in the volcanic rocks are enriched, but the contents decrease with increasing the compatibility. REEs are fractionated and REE patterns of volcanic rocks are characterized by a high LILE/HFSE. On the tectonomagmatic discriminant diagram of Hf-Th-Nb, they fall into the fields for subduction-related destructive plate margin basalts and its differentiates. We suggest that the tectonomagmatic setting of Da Hinggan Ling area was located at the continental margin arc related with subduction environment during the Mesozoic time or may be derived from mantle plume contaminated geochemically from subducting slabs, although it is, at present within the Asia continent.

• Korean Journal of Mineralogy and Petrology
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• v.33 no.4
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• pp.325-337
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• 2020

The Jurassic granitic rocks in the area of Gwangdeoksan located along the boundary between Hwacheon and Cherwon in northern Gyeonggi Massif consist of two-mica granite, garnet-bearing two-mica granite, mica-granite, and porphyritic biotite granite. These granitic rocks are calc-alkaline series and plotted in peraluminious domain in A/CNK vs. A/NK diagram. Petrographical and geochemical data indicate that the porphyritic biotite granite which intruded at the last period originated from distinct parental magma from two-mica granite, garnet-bearing two-mica granite, and mica-granite. On the basis of Rb/Sr vs. Rb/Ba diagram and Al2O3/TiO2 vs. CaO/Na2O, it is inferred the porphyritic biotite granite originated from protolith with less pelitic composition than 3 other granitic rocks. The enriched values of lithophile elements of Cs, Rb, and Ba and negative trough of Nb, P, Ti on spider diagram suggest that the peraluminous Jurassic granitic rocks in Gwangdeoksan area formed in subduction tectonic environment. Whole-rock zircon saturation thermometer indicates that the granitic rocks in the study area were melted at 692-795℃.

• Economic and Environmental Geology
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• v.32 no.4
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• pp.353-363
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• 1999

The Cretaceous and the Upper Jurassic strata of the Korean Peninsula, entirely of continental facies, form a sedimentary mega-unit subdivided into three unconformity-bounded units. The lower, Upper Jurassic-early Lower Cretaceous unit (Jasong Synthem) occurs profusely in North Korea and is characterized by volcanic rocks of intermediate to acidic, calc-alkaline to alkaline compositions; but strata of this unit is very rare in South Korea. The middle, Hauterivian-Lower Albian unit occurs commonly in the Korean Peninsula, but some alkalinesubalkaline basalt and andesite occur only in South Korea. A recently obtained U-Pb isochron age about 113.6 Ma (Chang et at, 1998) from the zircon grains of the Kusandong Tuff in the uppermost part of the Haman Formation has thrown much light on the age of this unit. The stratotype of this Hauterivian-L. Albian unit is the Sindong and Hayang Groups of the Kyongsang Basin, where the unit is about twice thick and has more conglomerates than in sedimentary basins in North Korea. The unit shows various sedimentary cycles in different basins showing that the cyclicity is controlled by local crustal motion. The upper, Upper Albian-Upper Cretaceous unit is abundant in South Korea with prolific volcanic rocks which are intermediate to acidic and notably calc-alkaline. In North Korea, however, this unit occurs in only one locality without volcanic rocks and is not voluminous. The distribution of these three unconformity-bounded units shows a stepwise younging toward the Pacific Ocean: the lower unit occurs mainly in N Korea, the middle unit occurs in both N and S Korea, and the upper unit occurs mainly in the southern part of S Korea. The Cretaceous sedimentary basins of S Korea were genetically controlled by paralleling sinistral strike-slip faults parallel to the Pacific margin.

• Economic and Environmental Geology
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• v.53 no.5
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• pp.565-583
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• 2020

In recent years, various social issues related to the natural radioactive elements detected in household goods and building materials are addressed, and should be solved promptly. In Korea, for more than 20 years, the Ministry of Environment has investigated the natural radioactive materials such as heavy metals, uranium, and radon in soil or groundwater. The origins of natural radioactive materials in them may have a close correlation with the geological factors including classification of rocks, petrogenetic origins, and deformation characteristics, but the exact geological correlations are not clarified because of the absence of the government policy preserved in the basement rocks, soils as well as groundwater in fault-related reservoirs. This study aims to perform a research on the correlation between the petrogeneses of the Phanerozoic plutonic rocks and natural radioactive concentrations in rocks (radon, uranium, thorium, potassium etc.) in Korea. Among the Phanerozoic plutonic rocks, alkaline plutonic rocks (syenite, monzonite and monzodiorite and alkali granite) show high U and Th concentrations by high solubilities of U, Th, Zr, REE, and Nb until the most extreme stages of magmatic fractionation (viz. crystal fractionation) due to high magma temperature and high alkalinity tendency. The highly fractionated high-K calalkaline and peraluminous granitic rocks (leucogranite, two-mica granite and leucocratic pegmatite are also U and Th concentrations compared with other less or medium fractionated granitic rocks (diorite, granodiorite and granite). The alkaline plutonic rocks are associated with intracontinental rifting and extensional environment after crustal thickening by collisional and subductional processes. In contrast, the dominant calc-alkaline granitic rocks in Korea are related to the arc environment of the subduction zone. In summary, the trends of the U, Th and K concentration from the Phanerozoic plutonic rocks in Korea are closely linked to the petrogenesis of the rocks in tectonic environment. The preliminary data for gamma-spectrometric mesurments of natural radionuclide contents (²²⁶Ra, ²³²Th and ⁴⁰K) in the Phanerozoic plutonic rocks show high values in the alkaline and highly fractionated granitic rocks.

• Economic and Environmental Geology
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• v.30 no.6
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• pp.603-612
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• 1997

Cretaceous sedimentary-volcanoclastic formations of the Kyeongsang Supergroup were intruded by granitic rocks in the late Cretaceous and early Tertiary. In the Euiseong and Shinryeong area, these intrusives have various compositions including gabbro, diorite，biotite granite and feldspar porphyry. Associated volcanic rocks consist of two chemically distinct types: the bimodal suite of basalt and rhyolite in the Keumseongsan caldera, and the felsic suite of andesite and rhyolite in the Sunamsan-Hwasan calderas. Most rocks are subalkaline, and follow a typical differentiation path of the calc-alkaline magma. The granitic rocks can be distinguished chemically from the volcanics by high Zr/Y ratios. Differences in Zr/Y and K/Y ratios between the two volcanic suites can be accounted for by mantle source and fractionation. Chondrite-normalized trace element abundances of granitic rocks are depleted in Th and K, whereas those of the Keumseongsan rhyolites are depleted in Sr and Ti. Rb, La and Ce is enriched in rhyolites of the Sunamsan-Hwasan calderas. $Rb-SiO_2$ and Rb-Y+Nb discrimination diagrams suggest that the intrusives and volcanics have a volcanic arc setting. K-Ar ages indicate four plutonic episodes : diorite (89 Ma), granite (66~62 Ma), granite and porphyry (55~52 Ma) and gabbro (52~45 Ma), and two volcanisms : bimodal basaltic and rhyolitic volcanism (71~66 Ma) in the Keumseongsan caldera, and felsic andesitic and rhyolitic volcanism (61~54 Ma) in the Sunamsan-Hwasan calderas. Geochemical and age data thus suggest that the igneous rocks are related to several geologic episodes during the late Cretaceous to early Tertiary.

• The Journal of the Petrological Society of Korea
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• v.11 no.1
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• pp.30-48
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• 2002

Phenocrysts with rapakivi texture are easily observed in Bangeojin granite. The rapakivi texture is composed of inner pinkish alkali feldspars and white-colored mantling plagioclase. The Bangeojin granite distinctively includes lots of mafic microgranular enclaves and can be divided into five rock facies: (1) enclave-poor granite (EPG); (2) enclave-rich granite (ERG); (3) mafic microgranular enclave (MME); (4) hybrid zone between mafic microgranular enclave and granite (HZ); (5) hybrid zone-like enclaves (HLE). The rapakivi textures are observed in these five rock facies with no difference in shape and size. Plagioclase mantle commonly shows dendritic texture that is an important indicator to know the rapakivi genesis. The mantling texture would indicate supercooling condition during magma solidification process. In addition, mafic microgranular enclaves would imply the magma mingling environment. The magma mixing process had possibly caused the mantling texture. An abundance of rapakivi phenocrysts in HZ and the influxing phenomenon of the phenocrysts into MME support that there were physical chemical exchanges during the mingling. And this model of the magma mixing/mingling explain well the heterogeneous distribution of the rapakivi phenocrysts in the five rock facies. Therefore the rapakivi textures in the Bangeojin granite would have been formed by magma mixing process.