The Journal of the Petrological Society of Korea (암석학회지)

The Petrological Society of Korea (한국암석학회)
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Cretaceous to Early Tertiary Granites and Magma Mixing in South Korea : Their Spatio-temporal Variations and Tectonic Implications (Multiple Slab Window Model)

남한의 백악기-제3기초 화강암과 마그마 혼합 : 시공간적 변화와 지구조적 의미(다중 슬랩 윈도우 모델)

  • Kim, Jong-Sun (Department of Geological Sciences, Pusan National University) ;
  • Kim, Kun-Ki (Department of Earth & Environmental Sciences, Gyeongsang National University) ;
  • Jwa, Yong-Joo (Department of Earth & Environmental Sciences, Gyeongsang National University) ;
  • Son, Moon (Department of Geological Sciences, Pusan National University)
  • 김종선 (부산대학교 지구환경시스템학부) ;
  • 김건기 (경상대학교 지구환경과학과) ;
  • 좌용주 (경상대학교 지구환경과학과) ;
  • 손문 (부산대학교 지구환경시스템학부)
  • Received : 2012.04.16
  • Accepted : 2012.05.03
  • Published : 2012.06.30
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Abstract

Based on the petrologic and age data of the Cretaceous to early Tertiary granites in south Korea, we propose a new tectonic model reflecting their temporal and spatial variations. A number of petrographic and geochemical studies on the granites suggest that they originated from the magma formed by subduction of oceanic crust in continental margin and were emplaced in epizone. The MMEs with various shapes and sizes, which were produced due to the magma mixing caused by the injection of mafic magma from mantle during the crystallization of the granitic magma, are observed in the granites. The distributions of the MMEs and ages of the granites show a distinctive spatio-temporal distribution pattern. The distribution pattern can be explained by a multiple slab window model related to the ridge subduction of Izanagi-Pacific plates during the Late Cretaceous.

한반도 남부의 백악기-제3기초 화강암의 암석학적 특징과 연대측정 자료들을 종합하여 시공간적 변화를 반영하는 지구조 모델을 제안하고자 하였다. 여러 암석기재와 지화학적 연구결과로부터 이들 화강암류는 대륙 연변부에서 해양지각의 섭입에 의해 형성된 마그마 기원으로 지각 천처에서 정치된 특징을 보인다. 또한 화강암류 내에는 고화과정 중 맨틀에서 유래한 염기성 마그마의 주입에 의한 마그마 혼합을 지시하는 다양한 형태와 크기의 MME들이 분포한다. MME의 분포와 화강암의 연령자료를 함께 살펴보면 시공간적으로 일정한 시기의 것들이 일정한 지역에 한정되어 분포하는 양상을 보인다. 이러한 특징은 후기 백악기의 이자나기-태평양판의 해령섭입으로 인한 다중 슬랩 윈도우 모델에 의해 설명될 수 있다.

Keywords

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