To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.
龙岗地块与北
之间
接触
上,发育了一条晚太古宙-古元古宙时期
线性

。
To date, komatiites with spinifex textures have not been found in the supracrustal rocks, but rock sequences similar to greenstones metamorphosed up to upper amphibolite facies are often observed.
龙岗地块与北
之间
接触
上,发育了一条晚太古宙-古元古宙时期
线性

。
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