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NTIS 바로가기광물과 암석 = Korean journal of mineralogy and petrology, v.33 no.3, 2020년, pp.175 - 183
구효진 (경상대학교 지질과학과 및 기초과학연구소) , 최헌수 (한국지질자원연구원 석유해저연구본부) , 조현구 (경상대학교 지질과학과 및 기초과학연구소)
There have rarely been performed for the clay mineralogy of the East Sea sediments except for few studies about paleoenvironmental aspect. This study inferred the provenance of sediments based on the clay mineral characteristics and distribution pattern for the 120 sediment samples collected by the ...
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핵심어 | 질문 | 논문에서 추출한 답변 |
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서해와 남해의 지형적 특징은? | 삼면이 바다로 둘러싸인 한반도에서 동해는 서해나 남해와 다른 특성을 가지고 있다. 서해와 남해는 경사가 완만한 대륙붕 지형으로 이루어져 있는데 반해 동해는 대륙붕의 발달이 미약하며 해안에서부터 대륙붕, 대륙사면 및 심해분지로 급격한 지형 변화를 나타내고 있다(Chough, 1983; Yun et al., 2015). | |
동해의 대륙붕 특징은? | , 2015). 동해의 대륙붕은 황해와 남해에 비하여 상대적으로 좁고, 경사도는 심하다. 동해 대륙붕의 평균경사도는 0. | |
카올리나이트와 녹니석 함량으로 에틸렌글리콜 처리된 시료 몇 피크를 구했나? | 점토광물의 상대적 함량은 피크의 면적을 이용하여 반정량적으로 계산하였다. 에틸렌글리콜 처리된 시료의 17 Å 피크를 스멕타이트(smectite), 10 Å 피크를 일라이트(illite) 그리고 7 Å 피크를 카올리나이트(kaolinite)+녹니석(chlorite) 함량으로 계산하였다. 각 광물의 고유한 피크 강도 차를 보정하기 위하여 계산된 피크 면적에 일정한 중량비를 곱하였다(Biscaye, 1965). |
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