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RISSThis study examined geological characteristics of the clay in the area around Kaduck-do, Kangseo-gu, Pusan, to figure out the characteristic fundamentals of the clay. The results are shown in the following. (1) The physical and chemical characteristi...
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RISS 인기검색어
https://www.riss.kr/link?id=A346812
- 저자
- 발행기관
- 학술지명
- 권호사항
-
발행연도
2003
-
작성언어
Korean
-
KDC
505.000
-
자료형태
학술저널
-
수록면
503-511(9쪽)
- 제공처
-
0
상세조회 -
0
다운로드
부가정보
다국어 초록 (Multilingual Abstract)
This study examined geological characteristics of the clay in the area around Kaduck-do, Kangseo-gu, Pusan, to figure out the characteristic fundamentals of the clay. The results are shown in the following.
(1) The physical and chemical characteristics are summarized in he following table. There were no meaningful changes according to the depth degree.
◁ 원문 표 참조 ▷
(2) The geological characteristics
1) Sedimetological and geochemical characteristics showed that the clay layer was formed under oceanic circumstances.
2) The mineralogy mainly includes clay materials such as quartz, feldspar, illite, chlorite, and kaolinite.
3) The results of radiocarbon dating by AMS showed 3,692±50 yr.B.P for the upper samples and 16,650±200 yr.B.P. for the lower samples.
(1) The physical and chemical characteristics are summarized in he following table. There were no meaningful changes according to the depth degree.
◁ 원문 표 참조 ▷
(2) The geological characteristics
1) Sedimetological and geochemical characteristics showed that the clay layer was formed under oceanic circumstances.
2) The mineralogy mainly includes clay materials such as quartz, feldspar, illite, chlorite, and kaolinite.
3) The results of radiocarbon dating by AMS showed 3,692±50 yr.B.P for the upper samples and 16,650±200 yr.B.P. for the lower samples.
This study examined geological characteristics of the clay in the area around Kaduck-do, Kangseo-gu, Pusan, to figure out the characteristic fundamentals of the clay. The results are shown in the following.
(1) The physical and chemical characteristics are summarized in he following table. There were no meaningful changes according to the depth degree.
◁ 원문 표 참조 ▷
(2) The geological characteristics
1) Sedimetological and geochemical characteristics showed that the clay layer was formed under oceanic circumstances.
2) The mineralogy mainly includes clay materials such as quartz, feldspar, illite, chlorite, and kaolinite.
3) The results of radiocarbon dating by AMS showed 3,692±50 yr.B.P for the upper samples and 16,650±200 yr.B.P. for the lower samples.
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