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NTIS 바로가기암석학회지 = The journal of the petrological society of korea, v.22 no.2, 2013년, pp.153 - 177
윤현수 (한국지질자원연구원 국토지질연구본부) , 이진영 (한국지질자원연구원 국토지질연구본부) , 홍세선 (한국지질자원연구원 국토지질연구본부) , 양동윤 (한국지질자원연구원 국토지질연구본부) , 김주용 (한국지질자원연구원 국토지질연구본부) , 조등룡 (한국지질자원연구원 국토지질연구본부)
To get the various data on geological information, distributional ratios and characteristics of constituent rocks with geologic ages and rock types were obtained by ArcGIS 10.1 program, digital geologic and geomorphic maps of 1:250,000 scale in Jeonnam and Gwangju areas. In the Jeonnam area, geologi...
핵심어 | 질문 | 논문에서 추출한 답변 |
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전남지역 의 지질시대 분포율은 어떤 순서로 감소하는가? | 1 프로그램, 1 대 250,000의 수치지질도 및 지형도를 사용하여 전남과 광주지역 구성암류의 지질시대별 및 암층별 분포율과 분포특성을 도출하였다. 전남지역 의 지질시대는 모두 7개로 대분되며, 분포율은 백악기, 선캠브리아기, 쥬라기, 제4기, 시대미상, 석탄기-삼첩기 및 삼첩기의 순으로 감소하며, 그 중 전자 넷이 94.80%를 이루어 거의 대부분을 차지한다. | |
나주와 망운도폭이 각각 변성사질암류와 하부천매암대의 경계부에 해당될 것으로 볼 수 있는 근거는? | 1). 즉 전남지역 서부에서 하부천매암대는 함평군의 함평읍-무안군의 무안읍에 발달하며, 이에 연속된 변성사질암류는 무안군의 무안읍-청계면에 길게 연장된다. 이와 관련하여 나주, 망운, 무안도폭(Choi and Ko, 1971; Lee et al., 1971; Hong and Choi, 1990)에서는 주로 운모 편암과 회색천매암, 석영편암과 운모편암, 규암과 운모편암으로 구성된다. 따라서 나주와 망운도폭이 각각 변성사질암류와 하부천매암대의 경계부에 해당될 것으로 볼 수 있다. | |
광주지역의 지질시대 분포율은 어떤 순서로 감소하는가? | 그 중 뚜렷하게 우세한 Kav는 전남지역의 북부, 서부, 중부, 동부 및 남부에 보다 넓게 발달하며, 특히 서부인 신안 및 목포-영암, 남부인 해남일대에 더 우세하게 분포하는 양상을 보인다. 광주지역의 지질시대는 모두 5개로 대분되고 분포율은 쥬라기, 제4기, 백악기, 선캠브리아기 그리고 시대미상의 순으로 감소하며, 그 중 전자 넷이 98.95%를 가져 거의 전부를 이룬다. |
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