• Title/Summary/Keyword: "조선의 지질"

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C. Gottsche's Journey through Korea in 1884 and Its Geographic Implications (1884년 곳체(C. Gottsche)의 조선 기행과 그 지리적 의미)

  • SON, ILL
    • Journal of the Korean Geographical Society
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    • v.51 no.6
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    • pp.739-759
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    • 2016
  • C. Gottsche(1855-1909), the Deutsch geologist, was invited by $M{\ddot{o}}llendorff$ who was the viceminister of foreign affairs in Korea, and travelled through the inland of Korean peninsula in 1884. He covered 2,550km in 138 days. After that journey, he wrote three academic papers about the geography and geology of Korea with the data of that field trip. Those paper bear considerable significance in that they included the first approaches to Korean geography and geology by a field-scientist with a modern academic training. Unlike other two papers focusing on the geology or the minerals, "The Geography of Korea(${\ddot{U}}ber$ Land und Leute in Korea(1886))" has its own value as a historical document, because it shows how the contempory Korea actually appeared to the eye of a $19^{th}$ western field-scientist. As this has not been introduced in Korean acdemic journals yet, this study might contribute to the understanding of how westerners regarded Korea in the end of 19th century.

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Orientations of Tecto-lineaments and Discontinuities for Different Rock Types in Andong Area (안동지역의 암종별 선구조선과 불연속면의 방위특성)

  • Kim Gyo-Won;Ihm Myeong-Hyeok
    • The Journal of Engineering Geology
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    • v.16 no.1 s.47
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    • pp.23-30
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    • 2006
  • This study was carried out to understand the relationship between orientation of tecto-lineaments obtained from aero-photograph and orientation of discontinuities measured at field for the rock types of igneous, sedimentary and metamorphic rocks in Andong area. Total 847 tecto-lineaments were extracted from the aero-photographs and total 1,940 discontinuities including joints, foliations and faults were measured during geologic survey. By using the software DIPS, preferred trends of tecto-lineaments were deduced as N30E-N40E for igneous rocks and N50E-N60E for both sedimentary and metamorphic rocks, while the trends of discontinuities were found as N40E-N50E for igneous rocks, N50E-N80E for sedimentary rocks and N50E-N60E for meta morphic rocks. Even though both orientations for a given rock type showed relatively good agreement in its trend, some discrepancy is also appeared. Since construction safety of geo-structures such as tunnel and slope, etc., is significantly affected by the orientation of discontinuities in rock masses, it is highly recommended to perform a detailed geologic survey as well as an aero-photograph interpretation at a design stage.

Performance Review of the Geological Research in Korean Peninsula by Japanese Geologist Tateiwa Iwao during the Japanese Occupation (일제강점기 일본인 지질학자 다테이와 이와오의 한반도 지질연구 성과고찰)

  • Kim, Seong-Yong;Lee, Jae-Wook;Park, Jung-Kyu
    • Economic and Environmental Geology
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    • v.48 no.5
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    • pp.401-408
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    • 2015
  • The achievements of Tateiwa Iwao's work in Korea are assessed as follows. Firstly, he pioneered the practice of stratigraphy in the Korean peninsula and completed geological maps of 21 sheets at 1:50,000 scale. Secondly, he published the results of a geological survey as bulletins, technical reports, and papers. Thirdly, he faithfully carried out the handover of assets and research outputs to Korea. Finally, after returning to Japan, Tateiwa wrote a book entitled The Korea-Japanese Tectonic Zone: History of a Geological Survey in Korea. However, he neglected to educate and train the next geologists for conducting geological surveys and exploration in Korea.

천곡동굴 부근의 지질개관

  • 정창희
    • Proceedings of the Speleological Society Conference
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    • 1993.07a
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    • pp.76-88
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    • 1993
  • 1962년 대한지질학회에서 조사 발표한 태백산지구지질단 제4쪽과 제8쪽에 의하면 동해시 부근의 지질은 [그림 1]과 같다. 이 지질도 남반부에 천곡동 동굴지대가 포함되어 있는데 동해시 일대의 지질은 조선계층군의 중부와 평안계층군의 대부분, 이들에 관입한 편마상화강암과 우질화강암을 주로하고 이들을 부정합으로 덮은 홍적층(단구층), 중적층으로 이루어져 있다.(중략)

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천곡동굴 부근의 지질개관

  • 정창희
    • Journal of the Speleological Society of Korea
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    • v.27 no.28
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    • pp.53-67
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    • 1991
  • 1962년 대한지질학회에서 조사 발표한 태백산지구지질권 제4쪽과 제8쪽에 의하면 동해시 부근의 지질은 [그림 1]과 같다. 이 지질도 남반부에 천곡동 동굴지대가 포함되어 있는데 동해시 일대의 지질은 조선계층군의 중부와 평안계층군의 대부분, 이들에 관입한 편마상화동굴과 우질화강암을 주로 하고 이들을 부정합으로 덮은 홍적층, 중적층으로 이루어져 있다.(중략)

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Study on Survey Activities for Geology and Mineral Resources in the Goryeo and Joseon Dynasty Based on the Records of Ancient Literatures (고문헌 기록에 나타난 고려시대와 조선시대의 지질자원 조사활동 연구)

  • Won, Byeongho;Lee, Sung-rock;Kim, Seong-Yong
    • Economic and Environmental Geology
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    • v.50 no.1
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    • pp.45-59
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    • 2017
  • In this research, we have extracted historical records regarding the geotechnology from the Goryeosa and the Annals of the Joseon Dynasty which are rated as ancient books that have objective views in the Goryeo Dynasty and the Joseon Dynasty in order to understand the national awareness and the social situation of the past events. We used the Korean history database system of National Institute of Korean History (NIKH) and collected related records by searching specific keywords such as volcano, mining, hot spring, and meteorite. According to the historical records, geological events such as the volcano and meteorite were regarded as important issues which were enough to be recorded in annals and surveyed by the dispatched government officials to the fields of events. In case of the hot springs, government officials conducted explorations of hot springs at king's orders and developed the potential areas of hot springs. Among the historical records on mining, the contents of geotechnology including the contents about discovered minerals and its locations can be easily found from those ancient books. Especially, it is possible to understand the history of geotechnology such as an establishment of modern organizations and a capitalistic flow for development through the history of the mining in the late Joseon Dynasty.

울산광역시 울주군 삼남면 상천리와 가천리 일원의 지질구조와 제4기단층의 발달 특성

  • 류충렬;최위찬;최성자
    • Proceedings of the KSEG Conference
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    • 2002.04a
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    • pp.193-200
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    • 2002
  • 울산광역시 울주군 삼남면 가천리와 상천리 일원에 발달하는 양산단층대 중남부의 발달특성과 제4기단층을 기재한다. 이 지역에는 중생대 백악기의 퇴적암과 화강암의 경계부 근처에 양산단층대의 주단층대와 부단층대로 확인되는 대규모의 단층파쇄대가 북북동-서남서 내지 남-북의 주향에 거의 수직으로 발달하고 있다. 단층조선은 수평에 가까우며 단층대내의 구조에 의하면, 주로 우향의 주향이동운동이 우세하다. 한편, 상천리와 가천리에는 이들 기반암과 제4기의 하성 사력층의 경계부 부근에서 제4기단층이 2조 발달하고 있다. 이들은 가천 제1단층과 가천 제2단층으로 기존의 양산단층대 일부가 제4기에 재활동한 것으로, 북북동 방향의 주향에 동측으로 고각의 경사를 보인다 단층조선은 거의 수평이며, 제4기 역들이 단층끌림에 의해 배열된 상태나 단층엽리내의 구조에 의하면 우향의 주향이동성운동이 우세하다.

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