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卡姆巴尔达硫化镍矿床产于北北西向,由超镁铁、镁铁和长英质火山岩和沉积岩构成的太古宙绿岩带里,这个绿岩带由卡尔古利向南延伸达120公里。在卡姆巴尔达地区绿岩带宽达7—8公里,并以主要断层为界,西部以含年轻沉积岩的绿岩带与断层并列,而东侧与沉积岩—长英质火山岩以断层相隔。绿岩带以北北西向的紧密褶皱为特征。见有例转褶皱和高角度走向断层,有些地区有交错褶皱,在卡姆巴尔达的局部地方,
The KalmBalda sulphide nickel deposit is produced in north-west-west, Archean greenstone belts of ultramafic, mafic and long-magmatic volcanic and sedimentary rocks extending south from Kalgoorlie to 120 km . The greenstone in the Karbabal region is 7-8 km wide and is dominated by major faults. The greenstone belt containing young sedimentary rocks in the west is parallel to the fault and the east side is separated from the sedimentary rocks by the faulted quartz volcanic rocks. Greenstone belts are characterized by tight north-northwest fold. See examples of the fold and high-angle faulting, in some areas are staggered folds, in parts of the area of Kambaldah,