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在东皮尔巴拉地块中,在该太古宙绿岩岩系的上部沉积层中,通过对相模型和原始流向的确定,认识了两种很易分别的同时代的台地(冲积)至海槽(浊流岩)的沉积物。在这两个地区,除了浅海陆棚岩相外,浅水到深水的过渡带是突然的。在戈尔格(Gorge)溪绿岩带中,过渡带出现在其北部和东北到西南部;而在布贾(Budjan)溪-莫斯基托溪绿岩带,则出现在北部到南部及东南部。虽然不能断然说,这两个带的沉
In the eastern Pilbara massif, in the upper sedimentary layer of this Archean greenstone series, two distinctly contemporary contemporaneous plateaus (alluvial) are known to the sea, through the determination of facies model and original flow direction Silt (turbidite) sediments. In both regions, except for the shallow-shelf continental facies, the transition from shallow to deep water is abrupt. In the Gorge Brooks, transitional zones occur in the north and northeast to southwest; in the Budjan - Mosquito Brook greenstone zones occur in the north to south and southeast unit. Although it can not be categorically said that the two belt Shen