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RISS
For the purpose of proffering the field geologic materials, author introduces a course of route map which porvides not only many various informations for field work but also is very convenient to go there. Through an observation and survey, the geol...
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RISS 인기검색어
https://www.riss.kr/link?id=A2037526
- 저자
- 발행기관
- 학술지명
- 권호사항
-
발행연도
1990
-
작성언어
Korean
-
KDC
374.4
-
자료형태
학술저널
-
수록면
1-20(20쪽)
- 제공처
- 소장기관
-
0
상세조회 -
0
다운로드
부가정보
다국어 초록 (Multilingual Abstract)
For the purpose of proffering the field geologic materials, author introduces a course of route map which porvides not only many various informations for field work but also is very convenient to go there.
Through an observation and survey, the geological contents obtained in the field work are summarized as follows:
1. All the areas mainly consist of aqueous clastic sedimentary rocks.
2. Sedimentary structures are rich for instance;
ripple marks, cross stratifications, convolute bedding, sun crack, worm trail, ball and pillow structures, flaser bedding etc.
3. Tectonic structures are observable too.
4. It is clarified that Euiam(의암) has parted from the basal rocks. Therefore, moving rock theory is partially confirmable.
Through an observation and survey, the geological contents obtained in the field work are summarized as follows:
1. All the areas mainly consist of aqueous clastic sedimentary rocks.
2. Sedimentary structures are rich for instance;
ripple marks, cross stratifications, convolute bedding, sun crack, worm trail, ball and pillow structures, flaser bedding etc.
3. Tectonic structures are observable too.
4. It is clarified that Euiam(의암) has parted from the basal rocks. Therefore, moving rock theory is partially confirmable.
For the purpose of proffering the field geologic materials, author introduces a course of route map which porvides not only many various informations for field work but also is very convenient to go there.
Through an observation and survey, the geological contents obtained in the field work are summarized as follows:
1. All the areas mainly consist of aqueous clastic sedimentary rocks.
2. Sedimentary structures are rich for instance;
ripple marks, cross stratifications, convolute bedding, sun crack, worm trail, ball and pillow structures, flaser bedding etc.
3. Tectonic structures are observable too.
4. It is clarified that Euiam(의암) has parted from the basal rocks. Therefore, moving rock theory is partially confirmable.
목차 (Table of Contents)
- Ⅰ. 序 論
- Ⅱ. 地形 및 地質
- (1) 槪觀
- (2) 本域 地形發達史
- (3) 晋州層
- Ⅰ. 序 論
- Ⅱ. 地形 및 地質
- (1) 槪觀
- (2) 本域 地形發達史
- (3) 晋州層
- Ⅲ. 觀察地點과 觀察內容
- Ⅳ. 各及學校 敎育의 主題와 關聯된 觀察資料
- Ⅴ. 結論 및 提言
- 參考文獻
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