Phase equilibria and the pressure-temperature path of the highest-grade Ryoke metamorphic rock in the Yanai district, SW Japan
Article Abstract:
An investigation of the phase equilibria of the garnet-cordierite zone of the Ryoke metamorphic rocks in the Yanai district of Japan examined the influence of manganese and other minor elements, including titanium, zinc and calcium. Moreover, this study determined the pressure-temperature path of the zone based on the microstructures of component materials. The assemblages examined were the combinations of spinel, cordierite and biotite; garnet, cordierite and biotite; and garnet and biotite. All assembles have quartz, K-feldspar and plagioclase.
Publication Name: Contributions to Mineralogy and Petrology
Subject: Earth sciences
ISSN: 0010-7999
Year: 1998
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Phase equilibria and the pressure-temperature path of the highest-grade Ryoke metamorphic rock in the Yanai district, SW Japan
Article Abstract:
An investigation of the phase equilibria of the garnet-cordierite zone of the Ryoke metamorphic rocks in the Yanai district of Japan examined the influence of manganese and other minor elements, including titanium, zinc and calcium. Moreover, this study determined the pressure-temperature path of the zone based on the microstructures of component materials. The assemblages examined were the combinations of spinel, cordierite and biotite; garnet, cordierite and biotite; and garnet and biotite. All assembles have quartz, K-feldspar and plagioclase.
Publication Name: Contributions to Mineralogy and Petrology
Subject: Earth sciences
ISSN: 0010-7999
Year: 1998
User Contributions:
Comment about this article or add new information about this topic:
An SEM study of porosity and grain boundary microstructure in quartz mylonites, Simplon Fault Zone, Central Alps
Article Abstract:
The grain boundary microstructure in quartz mylonites developed in effectively monomineralic veins from the Simplon Fault Zone of the Central Alps is characterized by three features. On two-grain boundaries are scattered fine pores of almost constant size and shape and all samples have large, irregularly shaped 'vug'-like porosity. Interconnected ridge structures on three- and four-grain junctions and vein-like or branch-like branching structures are also developed on two-grain boundaries and intragranular fractures.
Publication Name: Contributions to Mineralogy and Petrology
Subject: Earth sciences
ISSN: 0010-7999
Year: 1998
User Contributions:
Comment about this article or add new information about this topic:
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