@phdthesis{oai:tsukuba.repo.nii.ac.jp:00011122,
 author = {水野, 耕平 and Mizuno, Kohei},
 month = {},
 note = {Orthopyroxene-bearing pelitic hornfels (opx hornfels) is observed in the highest-grade contact metamorphic aureole of the Bushveld Complex in the northeastern Transvaal, South Africa. The environment and process of the metamorphism and its melting were examined on the basis of the newly calibrated orthopyroxene-biotite geothermometer and mineralogical and petrological evidences.

Opx hornfels consists mainly of orthopyroxene, biotite, cordierite, K-feldspar, and quartz. The hornfels is accompanied in places by leucocratic products which show melt textures consisting mainly of biotite, K-feldspar, plagioclase, and quartz. K-feldspar and quartz occationally contain tiny inclusions of orthopyroxene, biotite, and cordierite, which may have been refractory residues. According to the geological setting, ..., 1999, Includes bibliographical references},
 school = {筑波大学, University of Tsukuba},
 title = {Granulite metamorphism of pelitic rocks adjacent to the Bushveld complex contact in the Northeastern Transvaal area, South Africa},
 year = {2000}
}