• The Korean Journal of Petroleum Geology
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• v.5 no.1_2 s.6
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• pp.16-26
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• 1997

The Yemi Breccia has been reported as a separate formation near Yemi area, Kangwondo. This formation overlies the Maggot Formation of the Joseon Supergroup unconformably, and is overlain by the Goseong Shale conformably. Based on the field observation and textural examination of the Yemi Breccia, the breccia beds are interpreted as soluton-collapse breccia beds, which were formed by the dissolution of the pre-existing evaporites. The evaporites were precipitated during the deposition of the upper part of the Maggot Formation. Therefore, the Yemi Breccia should not be regarded as a separate formation, instead, it should be considered to be a upper part of the Maggot Formation. This implies that the overlying Goseong Shale and Goseong Limestone can be correlated with the Jigunsan and Duwibong Formtions, respectively.

• Journal of the Korean earth science society
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• v.40 no.2
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• pp.163-176
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• 2019

The Potosinian geological basement in central Mexico is comprised of the Upper Paleozoic metamorphic rocks, which crop out on the Sierra de Catorce nucleus located in the northeastern part of the state. The sedimentary sequence that covers unconformably the Paelozoic basement is represented by an Upper Triassic marine sedimentary sequence, correlating to the Zacatecas Formation and the Upper Triassic continental Huizachal Formation red beds, which in turn are covered either by La Joja Formation Jurassic red beds or by Upper Jurassic marine sediments. This sequence is overlain by the conformable Cretaceous calcareous marine sedimentary rocks in all the state of San Luis Potosi. The Cenozoic sequence unconformably covers some of the aforementioned rocks and is represented by undifferentiated volcanic rocks as well as by marine clastic rocks. The existing intrusive igneous rocks are felsic to intermediate composition, and they intrude the metamorphic basement and sedimentary rocks. Conglomerates with evaporitic sediments were deposited during the Pleistocene. The Quaternary sequence includes basalt flows, piedmont deposits, alluvium, and occasionally evaporites and caliche layers. In the state of San Luis Potosi, a great diversity of mineral deposit types is known as both metallic and nonmetallic. The host rocks of these deposits vary from one another including formations that represent from Paleozoic up to Tertiary. The mineralization age corresponds approximately to Tertiary (75%), and is mainly epigenetic. Conclusively, the data on geology and mineralization in San Luis Potosi, Mexico are helpful to predict a hidden ore body and select promising mineralized zone(s) when the domestic company makes inroads in the mining sector of Mexico.

• Journal of the Korean earth science society
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• v.30 no.7
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• pp.801-809
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• 2009

The Salinas Grandes borate deposit located in Jujuy state, northern Argentina can be categorized into the playatype evaporite deposit. Major borate mineral is ulexite ($NaCaB_5O_9{\cdot}H_2O$), which boron could be originated from volcanic rocks nearby playa. The eastern part of the Jujuy state in northern Argentina belongs to the Altiplano-Puna platform which shows high altitude and semiarid climate. Lots of Mesozoic and Cenozoic volcanics that are source of boron as well as playas that are the basin for borate precipitation in the area are essential for boron evaporite deposit. Therefore, the extensive explorations for the playa-type evaporite deposit are need.

• Membrane Journal
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• v.4 no.1
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• pp.57-62
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• 1994

This study uses pervaporation process to separate small amount of organic trichloroethylene, chloroform and perchloroethylene from contaminated water, since chlorinated hydrocarbones are known to be cancer suspecting compounds. For the separation of small amount of halogenated organic compound dissolved in wastewater, pervaporation membranes should be polymers that possess affinity with orgnic compounds and hydrophobicity. We used polyisobutylene, polyetheramide and polydimethylsiloxane membranes. The degree of affinity between organics and polymers were measured by contact angle method. We had good separation results that separation factor ranged from 34 to 19100 and permeate flux was$19.7~140g/m^2hr$.

• 방재와보험
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• s.122
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• pp.36-44
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• 2007

BP 텍사스 시티의 석유정제소의 화재폭발은 2005년에 가장 많은 인명의 손실을 끼친 유동화자산의 화재폭발사고로서 15인의 생명을 앗아가고 200여 명의 사람을 다치게 하였다. 트럭 한 대의 역화(내연기관의 부정폭발)에서 시작된 점화원은 이성질체화시스템(ISOM) 대기암 통기구에서의 가연성 탄화수소 액체와 증발 기체를 발화시켰다. 화학안전위원회는 그 사고를 조사 및 검토한 후 BP사가 모든 면에서 기계적인 결함과 함께 안전성이 불완전하였음을 발견하였다. 본 고는 저자들이 미국화학안전위험조사위원회에 제출한 이들의 조사보고서를 번역 게재한 것이다.

• Journal of the Mineralogical Society of Korea
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• v.26 no.4
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• pp.331-342
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• 2013

동아프리카 열곡대는 아라비아반도와 아프리카 북동부의 경계에서 부채꼴 형태로 남쪽으로 뻗은 대단층 함몰지구대이다. 아프리카 판 내부에 발달한 열곡대의 폭은 35~60 km이며 연장은 약 4,000km로 알려져 있다. 열곡대는 에티오피아에서 남서방향으로 발달하다 에티오피아 남부에서 동, 서 및 남서 열곡대로 나누어진다. 이 열곡대는 제3기초 올리고세(30~35 Ma)부터 에티오피아 북부 아파르 침강대를 중심으로 주 에티오피아 열곡대가 형성되고, 남쪽으로 확장되면서 마이오세에 활성화된다. 서부 열곡대는 동아프리카대지의 가장자리와 빅토리아 호의 서편을 따라 발달하며, 고각의 정단층에 의해 특징되는 전형적인 반지구대이다. 동부 열곡대(주 에티오피아 열곡대와 케냐 열곡대)는 30 Ma 전 화산활동과 지구조활동이 시작되었으나, 서부 열곡대는 Albert 호 북부에서 12 Ma 전에, Tanganyika 열곡에서는 7 Ma 전부터 시작되었다. 서부 열곡대의 남서 방향으로 분기된 남서 열곡대는 DR-콩고 남부와 잠비아의 Tanganyika 호에서부터 남서 방향으로 확장되어 보츠와나 Okavango 열곡대와 연결된다. 주 에티오피아 열곡대(MER)의 화산암류와 관련 퇴적암류는 지열, 소다회, 포타쉬(K), 천열수 금, 벤토나이트, 유황 및 부석자원으로 중요한 관련암으로 역할을 한다. 열곡관련 대표적인 광상으로는 Afar 열곡대에 분포하는 Danakhil K-광상과 Megenta 및 Blackrock 천열수 금광상이다. Danakhil K-광상은 제4기 화산활동과 높은 지열류에 의해 열곡대 내 분포하던 소금 선상지(salt fan)에서 증발작용에 의해 형성된 증발형 K-광상으로서 총 자원량은 약 12.6억톤으로 평가되었다. 이 광상에서는 4종의 K-광물인 실바이트, 카날라이트, 포리하라이트, 카이나이트가 산출한다. 아파르 침강대 내 분포하는 대표적인 천열수 금광상은 텐다호 지구대에 위치하는 Megenta 및 Blackrock 광상이다. 제4기에 EMR에서 산성의 과알칼리 화산활동에 의해 열수활동이 초래되어 현재까지도 활동하여 지열대가 형성되고, 저유황형금 광상들이 형성되었다. Megenta 저유황형 금 광상은 2009년 발견되었으며, 현재 영국의 Startex International사에 의해 탐사가 진행 중이다. 지금까지의 탐사 결과 옥수질 규화 변질암 분포지에서 5개의 광체가 분포하며, 그중 Hyena 광체에서는 규화 변질된 열수각력암에서 최고 16.75 g/t의 금 품위가 보고되었다. 동아프리카 열곡대의 서편인 부룬디에 분포하는 Gakara REE 광상은 카보너타이트 유형의 REE 광상이다. 이 광상은 $400km^2$ 면적 내 수 cm부터 수 m까지의 폭을 가지는 맥상 또는 망상세맥상의 광체를 형성한다. 주로 조립의 바스트너사이트와 모나자이트로 구성된다. 바스트너사이트의 형성시기는 $587{\pm}4Ma$인 신원생대로 알려져 있으며, 이 지역에 분포하는 카보너타이트와 알칼리암들이 신원생대에서 신생대까지의 광범위한 연대를 보이는 것은 동일한 구조선을 따라서 일어나는 반복되는 열곡활동으로 해석된다. 또한 REE, U, 인회석 자원의 관련암체로 생각되는 알카리 조면암(네펠린-조면암 포함)과 카보너타이트는 동아프리카 열곡대의 남동부 끝자락인 말라위와 모잠비크에 우세하게 분포한다.

• Korean Journal of Mineralogy and Petrology
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• v.34 no.1
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• pp.69-81
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• 2021

The exposed rocks in the Zacatecas state include mainly Mesozoic sedimentary and volcanic, Cenozoic volcanic and plutonic rocks. Paleozoic metamorphic rocks found in the northwestern portion of the state are considered as the most ancient rocks. These rocks correspond to the Caopas Formation which underlays the Later Paleozoic Rodeo Formation. The Mesozoic sequences are represented by a marine sedimentary sequence of the Later Triassic and the red beds of the Triassic-Jurassic Nazas Formation. The marine sediments of the Upper Jurassic overlay the Nazas Formation or metamorphic rocks from the Paleozoic. The Cretaceous sequences comprises marine sedimentary rocks in the north and northeast, and a volcanosedimentary set in the center and southeast. The Cenozoic is represented by volcanic nondifferentiated rocks, intrusive igneous rocks of acid and intermediate composition, and continental conglomerates with evaporitic sediments. The Quarternary sequences includes basalts, piedmont deposits, alluviums and occasionally, layers of evaporites and saltpeter. Furthermore, a great diversity of mineral deposits of both metallic and nonmetallic types occur in Zacatecas state. The rocks composing these deposits are extremely varied and include formations from Paleozoic to Tertiary. The mineralization age of ore deposits corresponds to the Tertiary in approximately 90%, and their genesis is mainly considered as epigenetic.

• Radiation Oncology Journal
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• v.21 no.1
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• pp.82-93
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• 2003

Purpose : To reduce the Irradiation dose to the lungs and heart in the case of chest wail irradiation using an oppositional electron beam, we used an Individualized custom bolus, which was precisely designed to compensate for the differences In chest wall thickness. The benefits were evaluated by comparing the normal tissue complication probablilties (NTCPS) and dose statistics both with and without boluses. Materials and Methods : Boluses were made, and their effects evaluated in ten patients treated using the reverse hockey-stick technique. The electron beam energy was determined so as to administer 80% of the irradiation prescription dose to the deepest lung-chest wall border, which was usually located at the internal mammary lymph node chain. An individualized custom bolus was prepared to compensate for a chest wall thinner than the prescription depth by meticulously measuring the chest wall thickness at 1 emf intervals on the planning CT Images. A second planning CT was obtained overlying the individuailzed custom bolus for each patient's chest wall. 3-D treatment planning was peformed using ADAC-Pinnacle$^{3}$ for all patients with and without bolus. NTCPS based on 'the Lyman-Kutcher' model were analyzed and the mean, maximum, minimum doses, V$_{50}$ and V$_{95}$ for 4he heari and lungs were computed. Results .The average NTCPS in the ipsliateral lung showed a statistically significant reduction (p<0.01), from 80.2${\pm}$3.43% to 47.7${\pm}$4.61%, with the use of the individualized custom boluses. The mean lung irradiation dose to the ipsilateral iung was also significantly reduced by about 430 cGy, Trom 2757 cGy to 2,327 cGy (p<0.01). The V$_{50}$ and V$_{95}$ in the ipsilateral lung markedly decreased from the averages of 54.5 and 17.4% to 45.3 and 11.0%, respectively. The V$_{50}$ and V$_{95}$ In the heart also decreased from the averages of 16.8 and 6.1% to 9.8% and 2.2%, respectively. The NTCP In the contralateral lung and the heart were 0%, even for the cases with no bolus because of the small effective mean radiation volume values of 4.4 and 7.1%, respectively Conclusion : The use of an Individualized custom bolus in the radiotherapy of postrnastectorny chest wall reduced the NTCP of the ipsilateral lung by about 24.5 to 40.5%, which can improve the complication free cure probability of breast cancer patients.

• The Korean Journal of Petroleum Geology
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• v.4 no.1_2 s.5
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• pp.27-39
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• 1996

In the Cretaceous, the Gulf Coast Basin evolved as a marginal sag basin. Thick clastic and carbonate sequences cover the disturbed and diapirically deformed salt layer. In the Cretaceous the salinities of the Gulf Coast Basin probably matched the Holocene Persian Gulf, as is evidenced by the widespread development of supratidal anhydrite. The major Lower Cretaceous reservoir formations are the Cotton Valley, Hosston, Travis Peak siliciclastics, and Sligo, Trinity (Pine Island, Pearsall, Glen Rose), Edwards, Georgetown/Buda carbonates. Source rocks are down-dip offshore marine shales and marls, and seals are either up-dip shales, dense limestones, or evaporites. During this period, the entire Gulf Basin was a shallow sea which to the end of Cretaceous had been rimmed to the southwest by shallow marine carbonates while fine-grained terrigengus clastics were deposited on the northern and western margins of the basin. The main Upper Cretaceous reservoir groups of the Gulf Coast, which were deposited in the period of a major sea level .rise with the resulting deep water conditions, are Woodbinefruscaloosa sands, Austin chalk and carbonates, Taylor and Navarro sandstones. Source rocks are down-dip offshore shales and seals are up-dip shales. Major trap types of the Lower and Upper Cretaceous include salt-related anticlines from low relief pillows to complex salt diapirs. Growth fault structures with rollover anticlines on downthrown fault blocks are significant Gulf Coast traps. Permeability barriers, up-dip pinch-out sand bodies, and unconformity truncations also play a key role in oil exploration from the Cretaceous Gulf Coast reservoirs. The sedimentary sequences of the major Cretaceous reseuoir rocks are a good match to the regressional phases on the global sea level cuwe, suggesting that the Cretaceous Gulf Coast sedimentary stratigraphy relatively well reflects a response to eustatic sea level change throughout its history. Thus, of the three main factors controlling sedimentation (tectonic subsidence, sediment input, and eustatic sea level change) in the Gulf Coast Basin, sea-level ranks first in the period.

• Journal of the Korea Computer Industry Society
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• v.8 no.2
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• pp.97-102
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• 2007

[ $CO_2$ ] laser sees that is most suitable to get this effect through minimum formation damage and advantage that is root enemy of effect that happen in minimum cellular tissue depth of 0.1mm is stable living body organization or internal organs institution. Formation damage by ten can be related in formation's kind or energy density, length of evaporation time. If shorten evaporation time, surroundings cellular thermal damage 200 - because happen within 400um laser beam in rain focus sacred ground surroundings cellular tissue without vitiation me by evaporation Poe of very small floor as is clean steam can . Application is possible to vulva cuticle cousins by a paternal aunt quantity, uterine cancer, cuticle tumor by laser system that $CO_2$ laser gets into standard in obstetrics and gynecology application. Because effect that super pulse output is ten enemies of laser if uniformity one pulse durations are short almost is decreased, most of all pulse module special quality of Pulse style $CO_2$ laser for obstetrics and gynecology mode stabilization by weight very, in this research to get into short pulse duration and higher frequency density, do switching by high frequency in DC-DC Converter output DC's ripple high frequency to be changed, high frequency done current ripple amount of condenser for output filter greatly reduce can . Ripple of output approximately to Zero realization applying possible inductor realization through a special quality experiment do.