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High temperature rhyodacites of the 36 ka Hauparu pyroclastic eruption, Okataina Volcanic Centre, New Zealand: change in a si- licic magmatic system following caldera collapse. J. Volcanol. Geotherm. Res. 147, 357-376.Shane P, Smith VC, Nairn IA (2005b) High temperature rhyodacites of ...
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[M. Sohmiya, Y. Sugahara, M. Ogawa, J. Phys. Chem. B 111 (2007) 8836–8841] suggests that the pore size and the interactions between [Ru(bpy) 3] 2+ and the pore surface affects the efficiency; the larger pore size and the weaker interactions between [Ru(bpy) 3] 2+ and the ...
Shane P, Smith VC, Nairn IA (2005) High temperature rhyodacites of the 36 ka Hauparu pyroclastic eruption, Okataina Volcanic Centre, New Zealand: change in a silicic magmatic system following caldera collapse. J Volcanol Geoth Res 147:357-376. doi:10.1016/j.jvolgeores.2005.04.015...