Georeferenced satellite mosaic of Iran with geometrical correction, there are two other mosaic in 1000k and 2500k scales.

   There large metamorphic terrains in Iran with various facies and grade. This map was prepared in 1986. Southwest (Zagros), northeast (Kopeh Daq) and north of Iran contains the least metamorphic rocks, which have most of hydrocarbon reserves of country. Classification of metamorphic rocks by type (regional, thermal and so) and tectonics events is of the map properties.

   This map displays temporal and spatial distribution of magmatic rocks in Iran with association of their feature, composition and environment. Also ophiolite belts show the old geosutures of Iran.

   It was prepared in 1964. Although the on-time knowledge regard the mineral zonation of Iran was very low, but the map was very successful in defining metallogenic provinces. First print of the paper map has been finished, however the new map is completed and revised with new information.

   In 1973, first tectonics map of Iran was prepared. With attention to crust, sedimentary environments, magmatism and metamorphism, Iran was subdivided to Sedimentological-structural zones that interpret geological history with consideration of rock units. The map was the start of systematic geology of Iran. Paper map was finished but detailed information has been remapped in 1000k scale and will be presented in the website.

   There are numerous hot springs in Iran, which are important in aspects of geotourism, medical usages and geothermal energy. At 1990, related map was prepared which in addition to classification of young deposits and structural pattern, it provide information of temperature, water discharge, chemical composition and application of springs.

   High seismicity of country caused the production of first seismotectonics map of Iran in 1976. The map consists of seismotectonical data overlaid on tectonics map. Distribution of historic and instrumental (20th Century) earthquake centers, their magnitude and focal depth and their relation to active faults were contributed on the map. Also the maps of Earthquake Risk, Maximum Ground Acceleration, Intensity Zonation of Historical Earthquakes and isoseismal are existed in 5000k scale. Second seismotectonics map of Iran was prepared in 1998 with the scale of 1000k.