Ash-Flow Tuffs of the Chisulryoung Volcanic Formation and Associated Welded Tuff Instrusion, Weolseong District, Southern Korea

월성(月城) 남부(南部) 치술령 지역(地域)의 화산암(火山岩)

  • 박기화 (한국동력자원연구소, 금속광상연구실) ;
  • 김선억 (한국동력자원연구소, 금속광상연구실)
  • Published : 1985.04.30

Abstract

The Chisulryoung Volcanic Formation comprises a thick sequence of pyroclastic flow deposits. Six members are distinguished, each representing separate flow units, comprising weakly to intensely welded acidic tuffs. A stock of welded acidic tuff, 1 km in diameter, intrudes hornblende granodiorite and sediments of Late Cretaceous age and the lower part of the Chisulryoung Volcanic Tuff Formation and may represent the vent through which the upper flows of the Chisulryoug Volcanic Formation were erupted.

치술령 지역(地域)에 분포(分布)하는 화산암(火山岩)은 Ash flow tuff, intrusive welded tuff 및 Diatreme으로 세분(細分)된다. 제삼기(第三紀) 초기(初期)에 분출(噴出)한 Ash flow tuff는 6개(個)의 층(層)(Member)으로 구분(區分)되고, 각층(各層)(Member)의 암상(岩相) 변화(變化)는 암주형(岩柱型)의 Intrusive welded tuff가 화산(火山) 분출(噴出) 화구(火口)였음을 암시(暗示)한다.

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