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慶尙北道 軍威-大栗洞-新寧 一帶의 上部白堊系 層序및 地史
孫晋潭 慶北大學校 自然科學大學 地質學科 地質學硏究會 1976 伏賢地質 Vol.- No.2
The stratigraphic interval (the lower part of the Hayang Group) between the lower boundaries of the Chilgok and the Banyawol Formations is subdivided into 11 lithozones: namely, (1) pebble bearing reddish zone, (2) dark-grayish zone, (3) tuffaceous reddish zone, (4) variegated-conglomerate bearing zone (5) reddish zone (6) alternation zone. (7) dark-grayish zone (8) alternation zone. (9) pyroclastic-breccia-bearing zone. (10) alternation zone, and (11) reddish zone. Zones (1) to (3) are correlated with the lower part of the Chilgok Formation: zone (10) and (11) are correlated with the upper part of the Haman Formation: and zones (4) to (9) are correlated with the Hakbong Member, Sinla Conglomerate, and the middle and the upper parts of the Chilgok Formation together. The radical lateral lithologic change of the lower part of the Hayang Group between the northern and the southern sides of the Palgongsan line is interpreted to have been caused by differential sedimentation due to the Palgongsan synsedimentational fault The Hamaji member of the Banyawol Formation and Sinryong conglomerate (good key bed of the boundary between the Haman and the Banyawol Formations) are newly described