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스콜라Placer gold deposits is mainly distributed in the Takaoi area. The alluvium is unconsolidated or semiconsolidated deposit consisting of gravel, sand, and soil beds in ascending order. They unconformably overlies the Carboniferous- Permian schist and C...
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RISS 인기검색어
https://www.riss.kr/link?id=A103486334
- 저자
- 발행기관
- 학술지명
- 권호사항
-
발행연도
2006
-
작성언어
-
-
주제어
placer gold deposit ; fluvial deposits ; gravel bed ; reserves of gold ; Takaoi 사금광상 ; 하성퇴적광상 ; 역암층 ; 금 매장량 ; 따까오이
-
KDC
452
-
등재정보
KCI등재,SCOPUS,ESCI
-
자료형태
학술저널
- 발행기관 URL
-
수록면
191-212(22쪽)
- 제공처
-
0
상세조회 -
0
다운로드
부가정보
다국어 초록 (Multilingual Abstract)
Placer gold deposits is mainly distributed in the Takaoi area. The alluvium is unconsolidated or semiconsolidated
deposit consisting of gravel, sand, and soil beds in ascending order. They unconformably overlies the Carboniferous-
Permian schist and Cretaceous granodiorite substratum. Based on detailed facies analysis, the alluvium can be
interpreted as a typical fluvial deposits containing gravel and sand beds of channel-fill unit and soil deposit of
floodplain. Gold grains are included mainly in the gravel bed and vein quartz is only contained gold among all
kinds of gravels. These features indicates that the source rock of the gold grain is vein quartz and gold grains are
separated from vein quartz during transport and abrasion. The reserves of gold in this area reach to at least 792 kg.
deposit consisting of gravel, sand, and soil beds in ascending order. They unconformably overlies the Carboniferous-
Permian schist and Cretaceous granodiorite substratum. Based on detailed facies analysis, the alluvium can be
interpreted as a typical fluvial deposits containing gravel and sand beds of channel-fill unit and soil deposit of
floodplain. Gold grains are included mainly in the gravel bed and vein quartz is only contained gold among all
kinds of gravels. These features indicates that the source rock of the gold grain is vein quartz and gold grains are
separated from vein quartz during transport and abrasion. The reserves of gold in this area reach to at least 792 kg.
Placer gold deposits is mainly distributed in the Takaoi area. The alluvium is unconsolidated or semiconsolidated
deposit consisting of gravel, sand, and soil beds in ascending order. They unconformably overlies the Carboniferous-
Permian schist and Cretaceous granodiorite substratum. Based on detailed facies analysis, the alluvium can be
interpreted as a typical fluvial deposits containing gravel and sand beds of channel-fill unit and soil deposit of
floodplain. Gold grains are included mainly in the gravel bed and vein quartz is only contained gold among all
kinds of gravels. These features indicates that the source rock of the gold grain is vein quartz and gold grains are
separated from vein quartz during transport and abrasion. The reserves of gold in this area reach to at least 792 kg.
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