Greenstone belts are not intracontinental rifts. What then are they?

Hundreds of intracontinental rifts with ages between 3.0 and 0 Ga were recognized on Earth. Compressional features are either absent or insignificant in the vast majority of these rifts. Intense compression is the rule in greenstone belts and preservation of regional extensional structures is rare. A common fate of intracontinental rifts is to develop into oceans which are likely to close. Mountain belts mark places where oceans have closed. In contrast to intracontinental rifts both mountain belts and greenstone belts are dominated by compressional structures. It is suggested that greenstone belts are mountain belts marking the places where oceans have closed. The complicated process of ocean closing and the regional complexities recorded in greenstone belts are compared.