scholarly journals Behavior of zircon in the upper-amphibolite to granulite facies schist/migmatite transition, Ryoke metamorphic belt, SW Japan: constraints from the melt inclusions in zircon

2012 ◽  
Vol 165 (3) ◽  
pp. 575-591 ◽  
Author(s):  
Tetsuo Kawakami ◽  
Isao Yamaguchi ◽  
Akira Miyake ◽  
Tomoyuki Shibata ◽  
Kenshi Maki ◽  
...  
Keyword(s):  
Melt Inclusions ◽  
Granulite Facies ◽  
Metamorphic Belt ◽  
Sw Japan

Melt Inclusions in Eclogites from High-Pressure and Ultra-High Pressure Metamorphic Belt in the Dabie Mountains, China

Mineralogy ◽  
2020 ◽  
pp. 255-263
Author(s):  
Han Yujing ◽  
Zhang Zeming ◽  
Liu Rong
Keyword(s):  
High Pressure ◽  
Melt Inclusions ◽  
Dabie Mountains ◽  
Metamorphic Belt ◽  
Ultra High Pressure

Mid-crustal horizontal shear zone in the forearc region of the mid-Cretaceous SW Japan arc, inferred from strain analysis of rocks within the Ryoke metamorphic belt

2009 ◽  
Vol 35 (1) ◽  
pp. 34-44 ◽  
Author(s):  
Takamoto Okudaira ◽  
Yuki Beppu ◽  
Ryosuke Yano ◽  
Mio Tsuyama ◽  
Kazuhiko Ishii
Keyword(s):  
Shear Zone ◽  
Strain Analysis ◽  
Horizontal Shear ◽  
Metamorphic Belt ◽  
Forearc Region ◽  
Sw Japan

Tourmaline and boron as indicators of the presence, segregation and extraction of melt in pelitic migmatites: examples from the Ryoke metamorphic belt, SW Japan

2004 ◽  
Vol 95 (1-2) ◽  
pp. 111-123 ◽  
Author(s):  
Tetsuo Kawakami
Keyword(s):  
High Temperature ◽  
Partial Melting ◽  
Correct Recognition ◽  
High Temperature Side ◽  
Metamorphic Belt ◽  
Melt Extraction ◽  
Mode Of Occurrence ◽  
Temperature Side ◽  
Sw Japan

The mode of occurrence of borosilicates and the breakdown fronts of prograde tourmaline (tourmaline-out isograd) in three anatectic migmatite regions of the Ryoke metamorphic belt, SW Japan, are reported. The breakdown of tourmaline in the migmatite zones and release of boron into the melts, followed by the extraction of the boron-bearing melts from the migmatite zones occurred throughout the Ryoke metamorphic belt. Retrograde, magmatic tourmaline in interboudin partitions filled with leucosome is useful for calculating the degree of partial melting in the migmatites. Using boron contents in the leucosomes and pelitic schists, the degree of partial melting at the migmatite front of the Aoyama area is estimated to be 12 wt.%. Extraction of the boron-bearing melt is suggested by the boron-depleted nature of the migmatites. Connection of boudinage structures probably supplied the vertical pathways of the segregated melts, and major transport of the melts was accomplished by dyking. Irregularly shaped, amoeboid tourmaline locally occurs on the high-temperature side of the tourmaline-out isograds in the Yanai and Komagane areas, implying incomplete extraction of boron-bearing melts from those areas. Discriminating retrograde from prograde tourmaline enables correct recognition of the tourmaline-out isograd. The amount of retrograde tourmaline in migmatites can potentially be used as an indicator of the degree of melt extraction from them.

Variety and genesis of the pyroxene-bearing S- and I-type granitoids from the Hidaka Metamorphic Belt, Hokkaido, northern Japan

2004 ◽  
Vol 95 (1-2) ◽  
pp. 161-179 ◽  
Author(s):  
Toshiaki Shimura ◽  
Masaaki Owada ◽  
Yasuhito Osanai ◽  
Masayuki Komatsu ◽  
Hiroo Kagami
Keyword(s):  
Partial Melting ◽  
Granulite Facies ◽  
Mafic Granulite ◽  
Granitic Rocks ◽  
Metamorphic Rocks ◽  
Metamorphic Belt ◽  
Model Calculations ◽  
Magmatic Arc ◽  
River Region ◽  
Northern Japan

ABSTRACTThe high-dT/dP-type Hidaka Metamorphic Belt in Hokkaido, northern Japan, represents a tilted crustal section of a magmatic arc of Tertiary age. The highest metamorphic grades reached are granulite facies, and the syn-metamorphic granitic rocks are widely distributed in this metamorphic terrane. The granitic rocks are mainly tonalitic and granodioritic in composition, and are classified into peraluminous (S-type) and metaluminous (I-type) granitoids. A large amount of pyroxene-bearing S-type tonalites (garnet-orthopyroxene tonalite) is distributed in the Niikappu river region in the northern part of the Hidaka Metamorphic Belt. Pyroxene-bearing I-type tonalite (two-pyroxene hornblende tonalite) bodies are also distributed in this area.The pyroxene-bearing tonalites are classified into several sub-types on the basis of their field occurrence, texture, mineral assemblage and geochemical features. Homogeneous IH- and SH-type tonalite are thought to represent original magmas, i.e. those which have been generated by partial melting of mafic metamorphic rocks and pelitic-psammitic metamorphic rocks, respectively. Model calculations assuming batch partial melting indicate that possible restites are garnet-two-pyroxene mafic granulite for IH-type and garnet-orthopyroxene aluminous granulite for SH-type. The unexposed lowermost crust of the ‘Hidaka crust’ is thought to be composed of garnet-two-pyroxene mafic granulite, garnet-orthopyroxene aluminous granulite and metagabbros.

scholarly journals EVOLUÇÃO PETROLÓGICA E ESTRUTURAL DA PORÇÃO ORIENTAL DO ESTADO DE MINAS GERAIS E SUAS IMPLICAÇÕES GEOTECTÔNICAS

1993 ◽  
Author(s):  
Antonio Gilberto Costa ◽  
Carlos Alberto Rosière ◽  
Lydia Maria Lobato ◽  
Fernando V. Laureano
Keyword(s):  
Shear Zones ◽  
Granulite Facies ◽  
Minas Gerais ◽  
Magmatic Differentiation ◽  
Metamorphic Belt ◽  
Quartz Crystals ◽  
Granulite Facies Metamorphism ◽  
Minas Gerais State ◽  
Positive Correlations ◽  
Basic Rocks

A metamorphic terrain with high-grade rocks of the Atlantic Metamorphic Belt underlies the eastern part of Minas Gerais State, from south of the town of Manhuaçu to Caratinga. This terrain comprises peraluminous gneisses, igneous and meta-igneous rocks. Granulites occur as small nucleus and vary in composition between peraluminous and basic  to intermediate, the latter represented by enderbitic mobilizate. Their formation, as well as that of migmatites of granitic composition, is considered to be related to mafic and ultramafic intrusions. In basic granulites, garnet-bearing mineral assemblages, with the development of corona textures, attest the effects of granulite facies metamorphism, although igneous assemblages and textures are still well preserved. Retrograde alteration assemblages are locally preserved. Despite of the diversity of metamorphic  phenomena in this area, T and P calculations reveal consistent results. Temperature and pressure calculations were undertaken in basic granulites slightly affected by the retrograde process. Using Fe +²/Mg exchange between garnet and ortopyroxene as geothermometers  and the exchange reaction:  An +En = 2/3Pyr + 1/3Grs + Qz as geobarometers peak metamorphic temperatures in the range of 660 to 760°C, at 4,8 to 6,6 Kbar are obtained. Mineral, textural and geochemical evidences indicate that the  metamorphic conditions have changed with time and suggest that the formation of the granulites is caused by the underplating of magmas, probably mantle-derived, at the base of the crust. Several rations between major, trace and rare earth elements have been employed. The basic rocks are similar in composition to tholeiites generated in within-plate tectonic settings. Positive correlations netween K2O and SiO2 and negative between MgO and SiO2 in fresh gabbro-noritic rocks and enderbites indicate magmatic differentiation. The geochemical character of altered basic rocks displays an unsystematic dispersion in correlations diagrams. This lack of correlation coupled with field and petrographic suggest the effects of a late metasomatic event on these rocks. This metasomatism comprises the dispersed development of charnockitic rocks with large K-feldspars and quartz crystals. Later dynamic processes gave place to subvertical shear zones with a well defined foliation.

scholarly journals Chemical characteristics and trapping P-T conditions of fluid inclusions in quartz veins from the Sanbagawa metamorphic belt, SW Japan

2008 ◽  
Vol 103 (2) ◽  
pp. 94-99 ◽  
Author(s):  
Koshi NISHIMURA ◽  
Kazuhiro AMITA ◽  
Shinji OHSAWA ◽  
Tomoyuki KOBAYASHI ◽  
Takao HIRAJIMA
Keyword(s):  
Fluid Inclusions ◽  
Chemical Characteristics ◽  
Metamorphic Belt ◽  
Quartz Veins ◽  
Sw Japan

scholarly journals P-T CONDITIONS OF GRANULITE-FACIES ROCKS FROM THE HIDAKA METAMORPHIC BELT, HOKKAIDO, JAPAN

1986 ◽  
Vol 92 (11) ◽  
pp. 793-808 ◽  
Author(s):  
YASUHITO OSANAI ◽  
KAZUNORI ARITA ◽  
MITSUTAKA BAMBA
Keyword(s):  
Granulite Facies ◽  
Metamorphic Belt
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