지원사업
학술연구/단체지원/교육 등 연구자 활동을 지속하도록 DBpia가 지원하고 있어요.
커뮤니티
연구자들이 자신의 연구와 전문성을 널리 알리고, 새로운 협력의 기회를 만들 수 있는 네트워킹 공간이에요.
논문 기본 정보
- 자료유형
- 학술대회자료
- 저자정보
- 발행연도
- 2021.10
- 수록면
- 202 - 202 (1page)
이용수
이 논문의 연구 히스토리 (15)
2019
Fluid-present partial melting of Paleoproterozoic Okbang amphibolite in the Yeongnam Massif, Korea
Yuyoung Lee
,
Moonsup Cho
대한지질학회 학술대회
2019.10
학술대회자료
Temporal relationship between high-temperature metamorphism and charnockite formation in the Yeongnam Massif, Korea
Yuyoung Lee
,
Moonsup Cho
,
Taehoon Kim
한국암석학회 학술발표회 논문집
2019.05
학술대회자료
2014
High-temperature low-pressure metamorphism associated with the Sancheong-Hadong anorthosite complex, Yeongnam Massif, Korea
Yuyoung Lee
,
Moonsup Cho
대한지질학회 학술대회
2014.10
학술대회자료
A massif-type (~1.86 Ga) anorthosite complex in the Yeongnam Massif, Korea: Syn- to late-orogenic emplacement associated with the mantle delamination in the North China Craton
Yuyoung Lee
,
Moonsup Cho
,
Wonseok Cheong
외 1명
한국암석학회 학술발표회 논문집
2014.05
학술대회자료
2007
Grain-scale melt distribution in tonalitic migmatites, Daeijak Island, western Gyeonggi massif : Relationship between anatexis and deformation
Yuyoung Lee
,
Moonsup Cho
대한지질학회 학술대회
2007.10
학술대회자료
Syn-deformational Anatexis of the Neoarchean Migmatites in Daeijak Island, western Gyeonggi Massif : Evidence for Disequilibrium Melting
Yuyoung Lee
,
Moonsup Cho
한국암석학회 학술발표회 논문집
2007.05
학술대회자료
- 이 논문의 후속연구가 궁금하신가요?
- 연관 학술논문 또는 학술발표를 통해 보다 발전된 연구결과를 확인하실 수 있습니다.
- 이 논문의 연구 히스토리 확인하기
초록· 키워드
오류제보하기
The fluid-fluxed melting of igneous protoliths provides an opportunity to assess the role of fluids during the high-temperature metamorphism and anatexis for the formation and reworking of continental crust. We combined multiple datasets of field, microstructural, geochemical, geochronological, and oxygen isotopic studies in order to investigate the fluid-fluxed melting of the Buncheon granitic gneiss, Yeongnam Massif, which is a representative for the Paleoproterozoic Korean arc complex. The Buncheon granitic gneiss, long known for its penetrative foliation in contrast to the occurrence of deformation-free Hongjesa granite, is typified by metatexitic migmatites containing (un)segregated leucosomes; but interestingly enough, neither melanosomes nor peritectic phases are associated with neosomes. The migmatitic gneiss underwent syn-kinematic wet melting via the reaction, plagioclase + K-feldspar + quartz + H²O = melt, at ~650-700° C and 4-5 kbar, particularly along a ca. 15 km-long and ca. 5 km-wide shear zone. The leucosomes are significantly variable in the contents of rare earth elements, Zr, Y and Th, and their Eu anomalies are either positive or negative. Such geochemical variations are attributed to the segregation and migration of melts together with the entrainment of residual phases. Sensitive high-resolution ion microprobe (SHRIMP) U-Pb ages of zircon and monazite were analyzed from three samples of migmatitic gneiss and leucosome. Zircons show oscillatory zonings in the absence of overgrowth rims and are dated at ca. 1.98-1.97 Ga, suggesting an Orosirian crystallization of igneous protoliths. On the ot ... 전체 초록 보기
목차
등록된 정보가 없습니다.
참고문헌 (0)
참고문헌 신청이 논문의 저자 정보
최근 본 자료
댓글(0)
0