Fluid composition of granulite facies carbonate rocks in the Beit Bridge Complex near Tshipise in the Central Zone of the Limpop
スポンサーリンク
概要
著者
-
Van Reenen
Rand Afrikaans Univ. Zaf
-
TSUNOGAE Toshiaki
Institute of Geoscience, University of Tsukuba
-
Tsunogae Toshiaki
Institute Of Geoscience University Of Tsukuba
-
Miyano Takashi
Institute Of Geoscience University Of Tsukuba
関連論文
- Decompression process of mafic granulite from eclogite to granulite facies under ultrahigh-temperature condition in the Kontum massif, central Vietnam
- Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution -
- Sm-Nd garnet ages of retrograde garnet bearing granulites from Tonagh Island in the Napier Complex, East Antarctica: A preliminary study
- Multistage orthopyroxene formation in ultrahigh-temperature granulites of Ganguvarpatti, southern India : implications for complex metamorphic evolution during Gondwana assembly
- Spinel + Quartz association from the Kerala khondalites, southern India : evidence for ultrahigh-temperature metamorphism
- Ultrahigh temperature metamorphism and deep crustal processes : Introduction
- Carbonic fluid inclusions in ultrahigh-temperature metamorphic rocks from Tonagh Island in the Archean Napier Complex, East Antarctica: A preliminary report
- SHRIMP geochronology of a mylonite zone on Tonagh Island: characterisation of the last high-grade tectonothermal event in the Napier Complex, East Antarctica
- Ultrahigh-temperature metamorphism of the Southern Marginal Zone of the Archean Limpopo Belt, South Africa
- Fluid inclusion study on gedrite fromation in metapelites near Maratele in the Limpopo Central Zone, eastern Botswana
- Fluid composition of granulite facies carbonate rocks in the Beit Bridge Complex near Tshipise in the Central Zone of the Limpop
- 491 南アフリカ Limpopo Belt にみられる後退変成作用の影響
- 490 東トランスヴァール地域に分布する接触変成岩(Pretoria Group)から推定した Bushveld Complex の貫入面
- Texture and zonal structure of K-feldspar phenocryst from granitic rocks in the Tsukuba district