Browsing by Author "Takahashi E."
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Browsing by Author "Takahashi E."
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Tuff J.; Gibson S.A.; Takahashi E. (2005)The anhydrous phase relations of an uncontaminated (primitive), ferropicrite lava from the base of the Early Cretaceous Paraná-Etendeka continental flood basalt province have been determined between 1 atm and 7 GPa. The ...
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Iwamori H.; McKenzie D.; Takahashi E. (1995)The primary effects of melt segregation processes on isentropic melting paths are studied using a one-dimensional steady-state model. A parameterization of X(T',P) to 9 GPa shows that X, the degree of melting, depends on ...
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Kogiso T.; Hirose K.; Takahashi E. (1998)Melting experiments on synthesized homogeneous mixtures of a pyrolitic peridotite (KLB-1) and average mid-oceanic ridge basalt (MORB) were carried out at pressures between 1.5 and 3.0 GPa and temperatures between 1300° and ...
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Nishihara Y.; Takahashi E. (2001)Knowledge of the mineralogical constituents of the Earth's mantle depends heavily on high-P experiments of pyrolite composition. In order to understand the planetary interior better, phase relations and mineral physics ...
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Miyazaki A.; Hiyagon H.; Sugiura N.; Hirose K.; Takahashi E. (2004)Solubility experiments for nitrogen and noble gases (Ar and Ne) in silicate melts were conducted using two experimental configurations: one was conducted at 1 atmospheric pressure, T =1300°C and oxygen fugacity (fO2) of ...
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Shibata T.; Takahashi E.; Matsuda J.I. (1998)We determined solubility of Ne, Ar, Kr, and Xe in binary silicate melts (Na2O-SiO2 and MgO-SiO2) and ternary silicate melts (Na2O-CaO-SiO2 and CaO-MgO-SiO2) at total pressures of 1.10-1.99 kbars and temperatures of ...
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Nishihara Yu.; Takahashi E.; Matsukage K.; Kikegawa T. (2003)In-situ synchrotron X-ray diffraction experiments were conducted using the MAX-III multianvil press of KEK on an omphacite (Di63JD37), for which Di = Ca(Mg,Fe)Si206 and Jd = NaAlSi206 Pressure-volume-temperature data were ...
Now showing items 1-7 of 7