GSJ Open-file Report no.534
Hijiori volcano (N38 36'35'', E140 9'20'') is a small caldera with approximately 2 km in diameter erupted at about 12 ky (Miyagi, 2004) on the place where no volcanic body had existed before. To understand how a new felsic volcano commences the activity, the magma process of Hijiori volcano is studied (and reported elsewhere). Here I report some useful petrological parameters for bulk rock composition of the essential ejecta (Table 1).
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Sample ID | Hj_j-Q |
Loc. N | 38 39'24.8'' |
Loc. E | 140 12'19.3'' |
SiO2 | 60.71 |
TiO2 | 0.71 |
Al2O3 | 15.85 |
tFeO | 6.6 |
MnO | 0.11 |
MgO | 3.9 |
CaO | 6.62 |
Na2O | 3.03 |
K2O | 1.28 |
P2O5 | 0.12 |
Total | 98.93 |
The parameters include the amount and chemical compositions of minerals and melt in equilibrium at some P, T, fO2, and H2O concentrations. These parameters were obtained using the MELTS program (Asimow and Ghiorso, 1998; Ghiorso and Sack, 1995) over the range of pressure from 1 atmosphere to 16 k bar with 0.1 k bar step, temperature from 700 to 1400 deg-C with 1 deg-C step, oxygen fugacity FMQ, FMQ+1, FMQ+2 log unit, and water concentration 0.1, 0.5, 1.0, 1.5, 2.0, 2.5, 3.0, 3.5, 4.0 4.5, 5.0, 6.0, 8.0, and 10 wt.% H2O. Since the MELTS program outputs huge quantities of numerical values (combination of P, T, H2O, and fO2 is about 4.7 million), I summarized them into a suite of contour maps on pressure-temperature plane using the GMT program (Wessel and Smith, 1998), and htmlized them cross-linked to develop a convenient tool.
This research project has been conducted under the research contract with Nuclear and Industrial Safety Agency (NISA).
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