정동진 단구 자갈층과 충진 물질의 입도 및 형상 특성에 대한 연구 (A study on the granulometric and clast shape characteristic of gravel terrace deposit at Jeongdongjin area)

서지정보

· 발행기관 : 한국지형학회
· 수록지 정보 : 한국지형학회지 / 23권 / 1호 / 17 ~ 33페이지
· 저자명 : 김종연, 양동윤, 신원정

초록

Samples from newly exposed outcrop of sedimentary layers forming Jeongdongjin coastal terrace in Gangreung area are collected and analyzed to find the sedimentary environment. The site are located at the gentle hillslope of the terrace surface area. The height of the outcrop is about 8m and the altitude of it’s highest part is 68~73m MSL.
The lowest part of this out crop is the partly consolidated sand layer with gravel veneer within it. It is found that this part is not in-situ weathered sand stone through the OSL method. This sand layer is overlain by the gravel layer with sand matrix. The shapes of the gravels from this part are mainly ‘platy’, ‘elongated’, and ‘bladed’ by the index of Sneed and Folk(1958). In addition, mean roundness is not so high. It is sceptical to regard this part as marine sediments which are continuously exposed to erosional processes. The boundary between the lowest sand layer and gravel layer showing the abrupt change in forming material without any mixture or transitional zone, so gravels are seemed to deposited after some degree of consolidation of the lowest sand layer. In addition, the hight of the boundary between layers are changed by the place, so the surface of the partly consolidated sand layer is not flat and has irregularity on topography when it buried by gravels.
Main part of this out crop is the poorly sorted coarse gravel(22.4mm) with sand matrix(1.36φ) layer with at least 2m thick covering the relatively fine gravels discussed above. Over 20% of particles have ‘very platy’, ‘very elongated’ and ‘very bladed’ shape and only less than 5% of particles have ‘compact’ shape, So this particles are also very hard to be regard as marine gravels which are abraded by marine processes. It can be concluded that this gravel layer formed by fluvial processes rather than coastal processes base on the form of the clast and sedimentary structure. The gravel layer is covered by fine(3~4φ) material layers of psudo-gleization which showing inter-bedding of red and white layers. Chemical composition of matrix and other fine materials should be analyzed in further studies.
It is attempted to fine the burial ages of the sediment using OSL method, but failed by the saturation. So it can be assumed that these sediments have be buried over 120ka.

영어초록

Samples from newly exposed outcrop of sedimentary layers forming Jeongdongjin coastal terrace in Gangreung area are collected and analyzed to find the sedimentary environment. The site are located at the gentle hillslope of the terrace surface area. The height of the outcrop is about 8m and the altitude of it’s highest part is 68~73m MSL.
The lowest part of this out crop is the partly consolidated sand layer with gravel veneer within it. It is found that this part is not in-situ weathered sand stone through the OSL method. This sand layer is overlain by the gravel layer with sand matrix. The shapes of the gravels from this part are mainly ‘platy’, ‘elongated’, and ‘bladed’ by the index of Sneed and Folk(1958). In addition, mean roundness is not so high. It is sceptical to regard this part as marine sediments which are continuously exposed to erosional processes. The boundary between the lowest sand layer and gravel layer showing the abrupt change in forming material without any mixture or transitional zone, so gravels are seemed to deposited after some degree of consolidation of the lowest sand layer. In addition, the hight of the boundary between layers are changed by the place, so the surface of the partly consolidated sand layer is not flat and has irregularity on topography when it buried by gravels.
Main part of this out crop is the poorly sorted coarse gravel(22.4mm) with sand matrix(1.36φ) layer with at least 2m thick covering the relatively fine gravels discussed above. Over 20% of particles have ‘very platy’, ‘very elongated’ and ‘very bladed’ shape and only less than 5% of particles have ‘compact’ shape, So this particles are also very hard to be regard as marine gravels which are abraded by marine processes. It can be concluded that this gravel layer formed by fluvial processes rather than coastal processes base on the form of the clast and sedimentary structure. The gravel layer is covered by fine(3~4φ) material layers of psudo-gleization which showing inter-bedding of red and white layers. Chemical composition of matrix and other fine materials should be analyzed in further studies.
It is attempted to fine the burial ages of the sediment using OSL method, but failed by the saturation. So it can be assumed that these sediments have be buried over 120ka.

참고자료

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