1 |
Baranov, V., 1957, A New Method for interpretation of aeromagnetic maps: PSEUDO-GRAVIMENTRIC Anomalies: Geophysics, 22, 359–383. doi: 10.1190/1.1438369
DOI
|
2 |
Baranov, V., 1957, A New Method for interpretation of aeromagnetic maps: PSEUDO-GRAVIMENTRIC Anomalies: Geophysics, 22, 359–383. doi: 10.1190/1.1438369
DOI
|
3 |
Isezaki, N., 1986, Anew shipboard three component magnetometer: Geophysics, 51, 1992–1998. doi: 10.1190/1.1442054
DOI
ScienceOn
|
4 |
Lourenco, J. S., and Morrison, H. F., 1973, Vector Magnetic anomalies derived from measurements of a single component of the field: Geophysics, 38, 359–368. doi: 10.1190/1.1440346
DOI
|
5 |
Takada, A., Oshima, O., Aramaki, S., Ono, K., Yoshida, T., and Kajima, K.,1992, Geology of Aogashima Volcano, Izu Islands: Bulletin of the Volcanological Society of Japan, 37, 233–250
|
6 |
Ueda, Y., Kumagaya, K., Koyama, K., 2008, Air borne magnetic surveys andtheir significaces for the monitoring of volcanic activities: Japan Geoscience Union Meeting, O220–004
|
7 |
Yamamoto, M., Seama, N., and Isezaki, N., 2005, Geomagnetic paleointensity over 1.2 Ma from deep-tow vector magnetic data across the East Pacific Rise: Earth, Planets, and Space, 57, 465–470
DOI
|
8 |
Tokyo Disaster Prevention Council, 1990, The reports for the property of volcanic eruption at Izu Island Arc (Aogashima): the booklet of earth science, 233–250
|
9 |
Nabighian, M. N., 1972, The analytic signal of two-dimensional magnetic bodies with polygonnal cross-section, its properties and use for automated anomaly interpretation: Geophysics, 37, 507–517. doi: 10.1190/ 1.1440276
|
10 |
Okuma, S., Makino, M., and Nakatsuka, T., 1989, Two-layer Model Inversion of Magnetic Anomalies using Pseudogravity and Reduction to the Pole: An application to the analysis of aeromagnetic anomalies over Izu-Oshima:: Geophysical Exploration (Buturi-Tansa), 42, 82–96
|
11 |
Makino, M., Nakatsuka, T., Okuma, S., and Kaneko, T., 1988, Aeromagnetic Anomalies over the Izu-Oshima Volcano: Bulletin of the Volcanological Society of Japan, Second Series, 33, 217–223
|
12 |
International Association of Geomagnetism and Aeronomy (IAGA), Division V, Working Group VMOD: Geomagnetic Field Modeling, 2005, The -Generation InternationalGeomagnetic Reference Field: Geophysical Journal International, 161, 561–565. doi: 10.1111/j.1365-246X.2005. 02641.x
DOI
ScienceOn
|
13 |
Blakely, R. J., 1995, Potential theory in Gravity and Magnetic Applications: Cambridge University Press, 441p
|
14 |
Kato, H., Isezaki, N., Park, C. H., Kim, C. H., and Nakanishi, M., 2007, Characteristics of crustal magnetic structure in the Tsushima (Ulleung) and Japan Basins from vector magnetic anomalies: Earth, Planets, and Space, 59, 887–895
DOI
|
15 |
Pelto, C. R., Elkin, T. A., and Boyd, H. A., 1968, Automatic contouring of irregularly spaced data: Geophysics, 34, 424–430
DOI
|
16 |
Hughes, D. S., and Pondrom, W. L., 1947, Computation of vertical magneticanomalies from total magnetic field measurements: Transactions – American Geophysical Union, 28, 193–197
DOI
|
17 |
Okuma, S., Makino, M., and Nakatsuka, T., 1994, Magnetization intensitymapping in and around Izu-Oshima volcano:: Japan Journal of Geomagnetism and Geoelectricity, 46, 541–556
DOI
|