Before the early Archaean (>3 000Ma), the chemically heterogeneous original crust had been developed.

  • 早太古代以前(大于3000Ma),本区已发育了成分不均匀的原始地壳,后期表壳岩系沉积在这种地壳的裂谷当中并发生了麻粒岩相变质作用;
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