Anatomy of an Early Archean gneiss complex: 3900 to 3600 Ma crustal evolution in southern West Greenland
Author:
Publisher
Geological Society of America
Subject
Geology
Cited by 114 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Convergent plate boundary environments for formation of ≥ 3800 Ma mafic-ultramafic assemblages (Isua area, Greenland): Implications for early global geodynamics;GEOSCI FRONT;2024
2. Convergent plate boundary environments for formation of ≥ 3800 Ma mafic–ultramafic assemblages (Isua area, Greenland): Implications for early global geodynamics;Geoscience Frontiers;2024-05
3. 3.7 billion year old detrital sediments in Greenland are consistent with active plate tectonics in the Eoarchean;Communications Earth & Environment;2024-04-15
4. Evaluating the multiple sulfur isotope signature of Eoarchean rocks from the Isua Supracrustal Belt (Southwest‐Greenland) by MC‐ICP‐MS: Volcanic nutrient sources for early life;Geobiology;2024-03
5. Zircon within chromitite requires revision of the tectonic history of the Eoarchean Itsaq Gneiss complex, Greenland;Geoscience Frontiers;2023-11
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