スポンサーリンク
公益社団法人 日本地震学会、地球電磁気・地球惑星圏学会 、特定非営利活動法人 日本火山学会、日本測地学会、日本惑星科学会 | 論文
- Spatial variation of coda wave amplitude in media with a localized heterogeneous region
- The BGS magnetic field candidate models for the 10th generation IGRF
- Meteoroid orbital element distributions at 1 AU deduced from the Harvard Radio Meteor Project observations
- Longitudinal effects in geomagnetic disturbances at mid-latitudes
- A hybridized mixed finite element domain decomposed method for two dimensional magnetotelluric modelling
- Can we estimate total magnetization directions from aeromagnetic data using Helbig's integrals?
- Hypocenter distribution of plate boundary zone off Fukushima, Japan, derived from ocean bottom seismometer data
- Treatment of horizontal and vertical tidal signals in GPS data: A case study on a floating ice shelf
- Utility of aeromagnetic studies for mapping of potentially active faults in two forearc basins: Puget Sound, Washington, and Cook Inlet, Alaska
- Mafic-felsic magma interaction at Satsuma-Iwojima volcano, Japan: Evidence from mafic inclusions in rhyolites
- Static shift levelling using geomagnetic transfer functions
- Helium observation in the Martian ionosphere by an X-ray ultraviolet scanner on Mars orbiter NOZOMI.
- Westward drift in secular variation of the main geomagnetic field inferred from IGRF
- Sq and sfe currents at equatorial stations along the western and eastern African sectors
- A simulation analysis to optimize orbits for a tropical GPS radio occultation mission
- Ground uplift detected by precise leveling in the Ontake earthquake swarm area, central Japan in 2002-2004
- Advance short-term prediction of the large Tokachi-oki earthquake, September 25, 2003, M = 8.1 A case history
- Observation of large-scale traveling ionospheric disturbances of auroral origin by global GPS networks
- Fault model of the 2005 Fukuoka-ken Seiho-oki earthquake estimated from coseismic deformation observed by GPS and InSAR
- In situ observations of low-density regions inside the plasmasphere
スポンサーリンク