• 자원환경지질
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• 제17권3호
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• pp.215-230
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• 1984

Petrological, paleomagnetic, geomorphological and structural studies on the southern part of, so called, Chugaryeong rift valley, have been carried out in order to clarify the nature of the rift valley. Three stages of volcanic activities characterized by Jijangbong acidic volcanic rocks and tholeiitic and andesitic basalt of Cretaceous age(?), and Jongok Quaternary olivine basalt occurred along the Dongducheon fault line. Jijangbong acidic volcanic rocks distributed in the central part of the studied area consist of rhyodacite, acidic tuff and tuff breccia, which are bounded by Dongsong fault on the east and Daegwangri fault on the west. The Jongok basalt differs from those of Ulrung and Jeju islands in mineralogy, chemical composition and differentiation. Jongok basalt distributed along the Hantan river dilineates the vesicles curved toward downstream direction and increment of numbers and thickness of lava flow toward upstream direction. These facts suggest that lava flowed from upstream side of the river. Rectangular drainage patterns also support the presence of the Dongducheon, Pocheon, Wangsukcheon and Kyonggang faults which were previously known. LANDSAT image, however, does not show any lineaments which could be counted as a graben or rift valley. Displacement of Precambrian quartzite and Jurassic Daedong supergroup along the southwestern extension of the Dongducheon fault shows the right lateral movement. The Paleomagnetic study of the tholeiitic and andesitic basalts from Baegeuri, Jangtanri and Tonghyeonri located at 2. 3km east, 0km east, and 1.5km west of Dongducheon fault respectively shows that their VGP(Virtual Geomagnetic Pole) being to intermediate geomagnetic field of short duration which suggests that they formed in almost same period. Mean VGP of Jongok basalt is located 82.4N and 80.6E. This is in good coincidence with worldwide VGP of Plio-Pleistocene indicating that Jongok basalt was extruded during Plio-Pleistocene epoch, and suggesting that the studied area has been tectonically stable since then. From the present study, the tectonic episode of the region is concluded as following three stages. 1. The 1st period is worked by the Daebo orogeny of Jurassic during which granodiorite was intruded in Precambrian basement. 2. The 2nd period is the time when right lateral strike-slip fault of NNE-SSW direction was formed probably during late Cretaceous to Paleogene and the Jijangbong acidic volcanic rocks and the older basalts were extruded. 3. The 3rd period is the time when the fault was rejuvenated during Pliocene or Pleistocene accompanied by the eruption of Jongok basalt. As a conclusion, geologic structure of the studied area is rather fault line valley than graben or rift valley, which is formed by differential erosion along the Dongducheon fault suggesting a continuation of the Sikhote-Alin fault. The volcanic rocks including the Jijangbong acidic rocks, tholeiitic-andesitic basalt and olivine basalt are associated with this fault line.

• 한국치위생학회지
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• 제9권2호
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• pp.111-124
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• 2009

This study analyzes through the review of literature and laws the exposure time, clinical frequency, and radiation exposure of intraoral and extraoral radiography as well as of panoramic radiography performed by dental hygienists in dental clinics, compares the dental radiology curriculums of radiological science and dental hygiene departments, and proposes the expansion of dental hygienists' radiography operations. The radiology curriculums were compared between the radiological science and dental hygiene departments of colleges. For new analysis by radiography for dental diagnosis, the exposure time, radiation absorbed dose, effective dose, and number of days of natural radiation were compared by the type of oral radiation films and radiographical techniques proposed by domestic and international studies. The exposure time of panoramic radiography is 15 seconds and it takes about two minutes for completion, whereas the exposure time of the standard radiography is 0.2~0.8 seconds and it takes 10 times longer for completion of the radiography of full mouth than the panoramic radiography. The standard radiography can cause distortions of radiation at severely curved parts of dental arch and palatopharyngeal reflex. However, panoramic radiography can be performed even for lock jaw patients, causes less inconvenience to patients and is much simpler than the standard radiography. The percentage of dental clinics where radiography is performed by dental hygienists was 92.0%, and the percentage of standard film radiography by dental hygienists was 98% whereas the percentage of panoramic radiography by dental hygienists was 92%. For the absorbed dose which is an indicator of radiation exposure, the When the effective dose which is an indicator of the danger of radiation exposure was converted to the number of days of natural radiation, it was 3.3 days for panoramic radiography, but 13.9 days for the full mouth standard radiography by bisecting angle technique which was 4.2 times longer than the panoramic radiography. There were two colleges that had a dental radiology course with two credits in the departments of radiological science. The credits for dental radiology courses in the department of dental hygiene ranged varied by college, ranging from 3 to 8; on average, the theory course was 2.2 credits and the practice course was 2.02 credits. To summarize the above results, the percentage of dental clinics where panoramic radiography is performed by dental hygienists under the guidance of dentists is high. Panoramic radiography has become an essential facility for dental clinics. It is faster than standard film radiography and less dangerous due to low radiation exposure. Panoramic radiography is a simple mechanical job that does not require training of oral radiography by radiotechnologist. Because panoramic radiography is one of major operations which must be performed at all times in dental clinics, it must be designated as intraoral technique rather than extraoral technique, or legalized for inclusion in the scope of operations of dental hygienists.

• 대한원격탐사학회지
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• 제24권2호
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• pp.125-131
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• 2008

Hyperion, AVIRIS 등의 초분광 영상은 기존의 다중분광 영상보다 넓은 파장대의 영상을 좁은 폭의 많은 밴드로 취득하기 때문에 다양한 분야의 연구에 이용되고 있다. 하지만 밴드별로 취득하는 파장대가 짧고 밴드수가 많아 계산량이 증가하며, 밴드간의 높은 상관관계 및 노이즈 밴드가 발생하는 한계가 존재한다. 이런 한계로 인해 기존에 알려진 분석기법의 적용결과가 제대로 도출되지 않는 경우도 발생한다. 따라서 초분광 영상을 사용할 경우, 노이즈가 포함된 밴드를 제거한 후 영상분석을 하는 것이 보다 정확하고 효율적이다. 본 연구에서는 초분광 영상(Hyperspectral Image)의 전처리 과정 중 노이즈 밴드 제거에 초점을 맞추었으며, 이를 위해 프랙탈 차원을 이용하였다. 프랙탈 차원 측정방법 중 대표적인 곡면차원 측정 방법인 삼각기둥 표면적 기법을 이용하였다. 각 밴드별 프랙탈 차원을 측정하고, 이를 정규화 하기 위해 Continuum Removal 기법을 적용한 뒤 경향을 살펴보았다. 경험적으로 구한 임계값을 통해 상대적으로 정보량이 적은 35개 밴드를 노이즈 밴드로 판단하여 제거하였다. 실험 영상으로는 EO-1 위성에서 취득되는 Hyperion 초분광 영상을 사용하였다. 실험 결과 프랙탈 차원 및 Continuum Removal 기법을 통해 Hyperion 초분광 영상의 노이즈 밴드를 추출하여 제거할 수 있음을 확인하였다.

• Radiation Oncology Journal
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• 제27권2호
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• pp.103-110
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• 2009

목 적: 피부와 같이 표면이 넓고 굴곡이 있는 부분을 치료할 때 토모테라피의 유용성과 치료 계획에서 계산된 표면 조사량의 정확성을 알아보고자 하였다. 대상 및 방법: 실린더 모양의 치즈 팬텀을 이용하여 2가지의 치료 계획을 세웠다. 첫 번째 계획은 표면에서 1 cm 깊이까지 고리 모양의 치료 부위를 설정하고, 여기에 2 Gy의 선량을 처방하였다. 다른 계획은 표면에서 5 mm 바깥쪽부터 1 cm 깊이까지 고리 모양의 치료 부위를 설정하고, 여기에 2 Gy의 선량을 처방하였다. 표면에서 2 cm 밑의 안쪽 부분은 차폐하여 방사선이 직접 들어가지 않도록 하였다. 표면 선량과 깊이에 따른 선량 분포를 측정하기 위하여, EDR2 필름을 팬텀 안에 넣었으며, TLD 칩 6개를 표면에 부착하였다. 결 과: 필름을 분석한 결과, 표면 선량은 첫 번째 계획에서 118.7 cGy였고 두 번째 계획에서 130.9 cGy였다. TLD 칩을 분석한 결과, 필름에 비하여 표면 선량이 높게 나왔는데 이것은 TLD 칩의 두께로 인한 것으로 생각된다. 처방 선량의 95%에 다다르는 깊이는 첫 번째 계획의 경우 2.1 mm, 두 번째 계획의 경우 2.2 mm였다. 최대 선량은 처방 선량의 110%였다. 표면에서 깊어질수록, 선량은 빠르게 감소하였고, 표면에서 2 cm 깊이에서는 처방 선량의 20%만 측정되었다. 결 론: 토모테라피는 피부와 같은 넓고 굴곡진 부위를 치료하는데 유용하다. 하지만 표면에서 2 mm 깊이 이내의 경우 실제 선량이 계획된 선량보다 적게 나타나기 때문에, 이 깊이보다 얕게 위치한 부위를 치료할 경우에는 보상체가 필요하다.