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在印度达瓦尔克拉通认出了三个连续而类型不同的绿岩带。最下部的绿岩带,主要是由镁铁-超镁铁火山岩和化学沉积物组成。中和上群是由火山岩、火山碎屑-岩屑和化学沉积物组成。但在绿岩带中,化学沉积物的类型和丰度有很大差异。最下部群,是以霍伦纳拉西普尔-努吉哈利(Holenarasipur-Nuggihalli)片岩带为代表,含有铬云母石英岩和磁铁石英岩。在一个地区,也见到了薄夹层状重晶石层与产在具鬣剌结构的橄榄
Three consecutive and different types of greenstone belts have been identified in India’s Walvalton. The lowermost greenstone belt is composed mainly of mafic-ultramafic volcanic rocks and chemical deposits. The middle and upper herds consist of volcanic rocks, pyroclastic debris and chemical deposits. However, the types and abundances of chemical deposits are quite different in the greenstone belt. The lowermost member, represented by the Holenarasipur-Nuggihalli schist belt, contains chrome micaceous quartzite and magnetite quartzite. In one area, thin layers of barite have also been found, with olive grown in a mane