The Journal of the Petrological Society of Korea (암석학회지)

The Petrological Society of Korea (한국암석학회)
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The temperature condition for the mylonitization of the Cheongsan granite, Korea

변형된 청산 화강암의 압쇄암화작용시의 변형온도 - 변형된 청산 화강암의 구조 해석 -

  • 강지훈 (안동대학교 지구환경과학과)
  • Published : 1998.06.01
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Abstract

Microstructural and rock structural analyses on the deformed Cheongsan granite characterized by abundant K-feldspar megacrysts have been carried out to understand the temperature condition for the ductile shear deformation. In K-feldspar, microkinks, microfractures and core-and-mantle structures without the development of subgrains in outer core-zone are the most common microstructures observed. Myrmekites and flame perthites are developed at the strain-localized areas along the microfractured K-feldspar. In plagioclase, microfractures, deformation twins and kink bands are predominant. The deformation twins cut across the igneous zonation of the plagioclase. Patterns of c-axis fabrics of dynamically recrystallized new quartz grains display single girdle and type II crossed girdle where prism slip system is predominant. These characteristic microstructures produced during the ductile shearing suggest that the ductile shear deformation in the Cheongsan granite occurred under epidote-amphibolite conditions($400-500^{\circ}C$). Three main shear zones are recognized at outcrop scale: discrete shear zone with anastomosing high-strain domain, shear zone with pervasive S-C structure and shear zone with homogeneously foliated domain. Geometric features of these shear zones produced during the ductile shear deformation are controlled by amount of strain under the $400-500^{\circ}C$ deformation temperature.

거정 장석(주로 K-장석)반정을 다량 함유하는 변형된 청산 화강암에 대한 미구조 및 암석구조 연구를 통하여 연성전단변형 동안의 온도조건을 규명하고자 한다. K-장석에서 가장 중요한 미구조로는 미세킹크, 미세단열 그리고 코아 외부에 아입자 없는 코아-맨틀구조 등으로 인지된다. 밀메카이트와 플레임 퍼어사이트는 조각된 K-장석들의 입계에 고 변형량의 집중으로 그들 입계상에서 발달한다. 사장석에는 미세단열과 변형쌍정 그리고 킹크대가 우세하게 나타난다. 화성기원의 사장석 누대구조가 변형쌍정에 의해 중첩되는 미세조직은 저 변형암에서 종종 관찰된다. 연성전단변형 동안에 재결정된 석영에 대한 c-축 배열 형태는 주로 prism가 탁월한 미끄럼계로 작용하여 형성된 single girdle과 type II crossed girdle을 모여준다. 연성전단운동 동안에 형성된 이상과 같은 특징적인 미구조로부터 청산 화강암에서 연성전단변형은 녹염석-각섬석상 변성도($400-500^{\circ}C$)에서 발생한 것으로 해석된다. 청산화강암에 발달된 연성전단대는 고 변형대가 혈관상으로 나타나는 불연속 전단대와 S-C 압쇄구조면을 갖는 연속 전단대 그리고 일정한 폭의 균질엽리 영역을 보이는 균질 전단대로 형태 분류된다. 이들 연성전단대는 동일 변형단계에서 형성되었으며 이들 연성전단대의 형태 변화는 $400-500^{\circ}C$의 변형온도에서 변형량의 차이로부터 비롯된 것으로 해석된다.

Keywords

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