The petrogenesis of ultramafic rocks in the >3.7 Ga Isua supracrustal belt, southern West Greenland: geochemical evidence for two distinct magmatic cumulate trends
Dyk ned i forskningsemnerne om 'The petrogenesis of ultramafic rocks in the >3.7 Ga Isua supracrustal belt, southern West Greenland: geochemical evidence for two distinct magmatic cumulate trends'. Sammen danner de et unikt fingeraftryk.