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فیزیک زمین و فضا
سال:2023 - دوره:48 - شماره:4
3d surface heat flow, low-temperature basins and curie point depth of the iranian plateau: hydrocarbon reservoirs and iron deposits
- صفحه:137-150
airborne geophysical data interpretation of nkalagu and abakaliki regions of the lower benue trough, nigeria: implication for mineral potentiality
- صفحه:21-32
calibration of iaspei standard broad-band magnitude mb for iranian plateau earthquakes
- صفحه:125-135
effect of nonextensive perturbation on ion acoustic solitons
- صفحه:221-229
geophysical surveys for saltwater intrusion assessment using electrical resistivity tomography and electromagnetic induction methods
- صفحه:1-20
internet application for interactive visualization of geophysical and space data: approach, architecture, technologies
- صفحه:151-160
long-short rupture boundary of coseismic displacement estimation based on 30-seconds gnss observation
- صفحه:67-76
magnetotelluric evidence for electrical anisotropy in the sabalan geothermal reservoir, northwestern iran
- صفحه:55-65
markov chain monte carlo non-linear geophysical inversion with an improved proposal distribution: application to geo-electrical data
- صفحه:107-124
modelling thermal convection of earth mantle with aspect code
- صفحه:99-106
prediction of water saturation by fsvm using well logs in a gas field
- صفحه:77-86
source fault analyses from insar data and aftershocks for the fin doublet earthquakes on 14 november 2021 in hormozgan province, south iran
- صفحه:87-97
spatial analysis of pm2.5 concentration over iraq during 2003-2020
- صفحه:173-182
spatial and temporal variation of seismic ambient noise in tehran region for frequency range 1-30 hz
- صفحه:33-45
the comparison of modis land surface temperature with meteorological stations measurements in iran
- صفحه:161-172
the effect of dust aerosols on some meteorological parameters in two dry and humid areas
- صفحه:183-195
the effect of variations of eej on the ionospheric tec at different longitudinal sectors using ground-based observation
- صفحه:197-220
the magnitude threshold for detecting recorded earthquakes in tehran’s accelerometer networks
- صفحه:47-54
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