後期 石炭紀 테티스海內 한국 三陟炭田의 淺海流 分析

• 영문명: Neritic paleocurrent analysis of Pennsylvanian Tethyan sea at Samcheog coalfield, Korea
• 발행기관: 대한자원환경지질학회
• 저자명: Hang Mook Kim(金恒默)
• 간행물 정보: 『자원환경지질』11권 1호, 21~37쪽, 전체 17쪽
• 주제분류: 자연과학 > 지질학
• 파일형태: PDF
• 발행일자: 1978.03.30

영문 초록

The depositional environment of the Manhang and the Geumcheon Formation of the Pennsylvanian Gomog Croup is revealed to the shallow neritic marine milieu in this paper also as the results of Park(1963), Cheong(1975) and Kim (1976), through the analyses of stratigraphy, paleocurrent, properties of cross-beddings and sedimentational features. The formations contains some possible terrestrial sediments suggesting the paralic environment, which are however not recognized definitely within them. The paleocurrent analysis is made to the Manhang rormation only. The paleocurrent of the formation is known to belong to the shallow neritic longshore current. The paleocurrent analysis is based chiefly on the cross-bedding analysis, and subordinately on the texture of clastic coarse sediments. The paleocurrent mean is determined to 269˚, that is, from east to west, of which direction is interpreted to the right angle to the slope of the basinal depository plane and also the parallel with the depositional strike, according to Klein (1960) and Selley’s (1968) criteria. The variance value of paleocurrent directions of the Manhang Formation in the whole area studied is 6,374, and the values range from 3,394 to 6,957 according to the dirstricts. The paleocurrent pattern of the whole area shows polymodel, and the patterns in each district range from trimodel to quadrimodel. Those models approach to the shallow marine or paralic model of Tohill and Picard (1966), Picard and High (1968 a), Pisnak (1957) and Pettijohn (1962). The mean value of maximum inclinations of cross-beddings of the whole area is 19.9˚ with the standard deviation of 8.4, and ranges from 15.6˚ to 21.7˚ in the districts. Comparing the histogram showing the frequency distribution of the maximum inclinations of cross-beddings of the Manhang Formation with the Pettijohn’s (1962) histogram, it is found that the model approaches to his marine model. The Pennsylvanian Gomog Group of the coalfield is considered to have had been deposited in the pseudogeosynclinal zone on the plateau by the transgression of the Tethyan sea caused by the epirogenic movements during the Pennsylvanian Period.

목차

Abstract

1. 머리말

2. 石炭系 古木層群의 堆積

3. 古木層群 晩項層 斜層理의 屬性分析

4. 古木層群의 堆積營力(Depositional process)

5. 후기 석탄기 삼척탄전의 테티스해 천해류

6. 結論

REFERENCES