The Journal of the Petrological Society of Korea (암석학회지)

The Petrological Society of Korea (한국암석학회)
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Petrological Characteristics of the Satkatbong Pluton, Yeongdeok, Korea

영덕 삿갓봉암체의 암석학적 특성

  • Lim, Hoseong (Department of Geology, Kyungpook National University) ;
  • Kim, Jung-Hoon (Department of Geology, Kyungpook National University) ;
  • Woo, Hyeondong (Department of Geology, Kyungpook National University) ;
  • Do, Jinyoung (Department of Cultural Properties, Gyeongju University) ;
  • Jang, Yun-Deuk (Department of Geology, Kyungpook National University)
  • 임호성 (경북대학교 자연과학대학 지질학과) ;
  • 김정훈 (경북대학교 자연과학대학 지질학과) ;
  • 우현동 (경북대학교 자연과학대학 지질학과) ;
  • 도진영 (경주대학교 문화재학과) ;
  • 장윤득 (경북대학교 자연과학대학 지질학과)
  • Received : 2016.04.06
  • Accepted : 2016.05.13
  • Published : 2016.06.30
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Abstract

The Satkatbong pluton was studied with other plutons together, but some fundamental petrological characteristics were missing. This study mainly reports the petrography and geochemistry of the Satkatbong pluton comparing with the Daebo and the Bulguksa granitoids in south Korea. The Satkatbong pluton, which is host rock including a number of Mafic Magmatic Enclaves (MME), is north-south shaped dioritic pluton, located along the east coast of south Korea. The Satkatbong pluton seems to be unconformable with Cretaceous sedimentary rocks from fieldwork result. In geochemistry, the Satkatbong pluton, which is roughly similar with the Daebo granitoids, is classified into calc-alkali series rock and volcanic arc granitoid Tectonically. The fact that AlT value in marginal parts of amphiboles in the Satkatbong pluton is lower than other granitoids implies emplacement depth of the Satkatbong pluton was relatively shallow. The Satkatbong pluton shows different geochemical feature compared to the adjacent adakitic Yeongdeok granite. This seems to be caused by mafic mantle material expected from the occurrence of MMEs.

삿갓봉암체는 기존에 다른 암체들과 함께 연구된 바는 있으나 몇몇 기초적인 암석학적 특성은 다뤄지지 못했다. 본 연구에서는 삿갓봉암체에 대해 보다 자세한 암석학적 특성을 보고하고, 남한의 다른 대보화강암, 불국사화강암과 지화학적 특성을 비교하고자 한다. 삿갓봉암체는 영덕군 경정리에서 장사리에 걸쳐 남북으로 길게 신장된 형태로 발달한다. 삿갓봉암체는 대부분 섬록암질암으로 구성되어있으며, 염기성미립포유암(이하 MME)을 다량 포획하고 있다. 야외조사결과 삿갓봉암체와 인접하는 백악기 퇴적암은 상호 부정합관계가 예상된다. 지화학적 특성을 대보, 불국사 암군과 비교했을 때, 삿갓봉암체는 주원소와 미량원소 특성에서 대보화강암에 보다 유사한 분포 특성을 보였으며, 칼크알칼리 계열의 암석으로 분류되었다. 조구조적으로 삿갓봉암체는 섭입대 화강암의 특징을 보이며, 각섬석에서의 AlT 값은 타 암체들보다 낮은 값을 가져, 보다 얕은 정치 심도를 가졌던 것으로 예상된다. 삿갓봉암체는 뚜렷한 아다카이트 특성을 보이는 인근의 영덕화강암과는 다른 지화학적 특성을 가지고 있으며, 이는 MME의 산출로 예상되는 고철질 맨틀물질의 혼성에 의한 영향으로 예측된다.

Keywords

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