A map is a plot of radiation intensity as a function of position of the object in the sky. One of the coordinate systems, equatorial coordinate system, elliptical coordinate system and galactic coordinate system, is used to note the position of the object regardless of your position on the earth. A universally accepted coordinate system, the equatorial coordinate system (right ascension and declination) is normally used in radio astronomy.
From a map, the astronomer gets the information of the position of the emitting source and the structural details of the source. The structural details of the source in a map depends on the resolution of the radio telescope. (see section 1.2.1).