Takahito KAZAMA | Geodesy Laboratory, Kyoto University (kyoto-u.ac.jp)
[1] T. Kazama and S. Okubo (2009): Hydrological modeling of groundwater disturbances to observed gravity: Theory and application to Asama Volcano, Central Japan. J. Geophys. Res. (Solid Earth), 114 (B8), B08402, doi:10.1029/2009JB006391.
[2] T. Kazama, Y. Tamura, K. Asari, S. Manabe and S. Okubo (2012): Gravity changes associated with variations in local land water distributions: observations and hydrological modeling at Isawa Fan, northern Japan. Earth Planets Space, 64 (4), 309-331, doi:10.5047/eps.2011.11.003.
[3] T. Kazama, S. Okubo, T. Sugano, S. Matsumoto, W. Sun, Y. Tanaka, E. Koyama (2015): Absolute gravity change associated with magma mass movement in the conduit of Asama Volcano (Central Japan), revealed by physical modeling of hydrological gravity disturbances. J. Geophys. Res. (Solid Earth), 120 (2), 1263-1287, doi:10.1002/2014JB011563.
[4] T. Kazama, H. Hayakawa, T. Higashi, S. Ohsono, S. Iwanami, T. Hanyu, H. Ota, K. Doi, Y. Aoyama, Y. Fukuda, J. Nishijima, and K. Shibuya (2013): Gravity measurements with a portable absolute gravimeter A10 in Syowa Station and Langhovde, East Antarctica. Polar Science, 7 (3-4), 260-277, doi:10.1016/j.polar.2013.07.001.
[5] T. Kazama, H. Kawakatsu and N. Takeuchi (2008): Depth-dependent attenuation structure of the inner core inferred from short-period Hi-net data. Phys. Earth Planet. Int., 167 (3-4), 155-160, doi:10.1016/j.pepi.2008.03.001.