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Eoarchean contrasting ultra-high-pressure to low-pressure metamorphisms (<250 to >1000 °C/GPa) explained by tectonic plate convergence in deep time

Precambrian research, 2020-07, Vol.344, p.105770, Article 105770

2020

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New 1:20,000 scale geological maps, synthesis and history of investigation of the Isua supracrustal belt and adjacent orthogneisses, southern West Greenland: A glimpse of Eoarchaean crust formation and orogeny

Precambrian research, 2009-08, Vol.172 (3-4), p.189-211

2009

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Multistage late Neoarchaean crustal evolution of the North China Craton, eastern Hebei

Precambrian research, 2011-08, Vol.189 (1), p.43-65

2011

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Cross-examining Earth’s oldest stromatolites: Seeing through the effects of heterogeneous deformation, metamorphism and metasomatism affecting Isua (Greenland) ∼3700 Ma sedimentary rocks

Precambrian research, 2019-09, Vol.331, p.105347, Article 105347

2019

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Convergent plate boundary environments for formation of ≥ 3800 Ma mafic–ultramafic assemblages (Isua area, Greenland): Implications for early global geodynamics

Di xue qian yuan., 2024-05, Vol.15 (3), p.101794, Article 101794

2024

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Mesoarchaean collision of Kapisilik terrane 3070Ma juvenile arc rocks and >3600Ma Isukasia terrane continental crust (Greenland)

Precambrian research, 2015-03, Vol.258, p.146-160

2015

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Seeing through the magnetite: Reassessing Eoarchean atmosphere composition from Isua (Greenland) >=3.7 Ga banded iron formations

Di xue qian yuan., 2017-11, Vol.8 (6), p.1233-1240

2017

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3806Ma Isua rhyolites and dacites affected by low temperature Eoarchaean surficial alteration: Earth's earliest weathering

Precambrian research, 2015-10, Vol.268, p.323-338

2015

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3700Ma pre-metamorphic dolomite formed by microbial mediation in the Isua supracrustal belt (W. Greenland): Simple evidence for early life?

Precambrian research, 2010-12, Vol.183 (4), p.725-737

2010

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Inventory and assessment of Palaeoarchaean gneiss terrains and detrital zircons in southern West Greenland

Precambrian research, 2004-12, Vol.135 (4), p.281-314

2004

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Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures

Nature (London), 2016-09, Vol.537 (7621), p.535-538

2016

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The early Archaean Itsaq Gneiss Complex of southern West Greenland: the importance of field observations in interpreting age and isotopic constraints for early terrestrial evolution

Geochimica et cosmochimica acta, 2000-09, Vol.64 (17), p.3035-3060

2000

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Fifty years of the Eoarchean and the case for evolving uniformitarianism

Precambrian research, 2021-12, Vol.367, p.106442, Article 106442

2021

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Evolution of the Palaeozoic mafic-ultramafic Lizard Complex (SW England) from zircon and baddeleyite U-Pb-Hf isotopic constraints: New thoughts on the convergence of Avalonia and Armorica

Lithos, 2023-09, Vol.452-453, p.107227, Article 107227

2023

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The Itsaq Gneiss Complex of southern West Greenland; the world's most extensive record of early crustal evolution (3900-3600 Ma)

Precambrian research, 1996-05, Vol.78 (1), p.1-39

1996

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3710 and ⪖ 3790 Ma volcanic sequences in the Isua (Greenland) supracrustal belt; structural and Nd isotope implications

Chemical geology, 1997-09, Vol.141 (3), p.271-287

1997

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Review of the Isua supracrustal belt area (Greenland) Eoarchean geology from integrated 1:20,000 scale maps, field observations and laboratory data: Constraints on early geodynamics

Precambrian research, 2022-09, Vol.379, p.106785, Article 106785

2022

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Comparison of three cannulas for hysterosalpingography: a prospective, randomized study

Fertility and sterility, 2010, Vol.94 (4), p.S211-S211

2010

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The emergence of the Eoarchaean proto-arc: evolution of a c. 3700 Ma convergent plate boundary at Isua, southern West Greenland

Geological Society special publication, 2015-01, Vol.389 (1), p.113-133

2015

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In support of rare relict ∼3700 Ma stromatolites from Isua (Greenland)

Earth and planetary science letters, 2021-05, Vol.562, p.116850, Article 116850

2021

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Isua (Greenland) ~3700 Ma meta-serpentinite olivine Mg# and δ18O signatures show connection between the early mantle and hydrosphere: Geodynamic implications

Precambrian research, 2021-08, Vol.361, p.106249, Article 106249

2021

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3850 Ma BIF and mafic inclusions in the early Archaean Itsaq Gneiss Complex around Akilia, southern West Greenland? The difficulties of precise dating of zircon-free protoliths in migmatites

Precambrian research, 2002-08, Vol.117 (3), p.185-224

2002

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Adjacent terranes with ca. 2715 and 2650 Ma high-pressure metamorphic assemblages in the Nuuk region of the North Atlantic Craton, southern West Greenland: Complexities of Neoarchaean collisional orogeny

Precambrian research, 2007-06, Vol.155 (3), p.159-203

2007

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The Eoarchean legacy of Isua (Greenland) worth preserving for future generations

Earth-science reviews, 2019-11, Vol.198, p.102923, Article 102923

2019

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Earth's oldest mantle fabrics indicate Eoarchaean subduction

Nature communications, 2016-02, Vol.7 (1), p.10665-10665, Article 10665

2016

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Eoarchean contrasting ultra-high-pressure to low-pressure metamorphisms (<250 to >1000 °C/GPa) explained by tectonic plate convergence in deep time

New 1:20,000 scale geological maps, synthesis and history of investigation of the Isua supracrustal belt and adjacent orthogneisses, southern West Greenland: A glimpse of Eoarchaean crust formation and orogeny

Multistage late Neoarchaean crustal evolution of the North China Craton, eastern Hebei

Cross-examining Earth’s oldest stromatolites: Seeing through the effects of heterogeneous deformation, metamorphism and metasomatism affecting Isua (Greenland) ∼3700 Ma sedimentary rocks

Convergent plate boundary environments for formation of ≥ 3800 Ma mafic–ultramafic assemblages (Isua area, Greenland): Implications for early global geodynamics

Mesoarchaean collision of Kapisilik terrane 3070Ma juvenile arc rocks and >3600Ma Isukasia terrane continental crust (Greenland)

Seeing through the magnetite: Reassessing Eoarchean atmosphere composition from Isua (Greenland) >=3.7 Ga banded iron formations

3806Ma Isua rhyolites and dacites affected by low temperature Eoarchaean surficial alteration: Earth's earliest weathering

3700Ma pre-metamorphic dolomite formed by microbial mediation in the Isua supracrustal belt (W. Greenland): Simple evidence for early life?

Inventory and assessment of Palaeoarchaean gneiss terrains and detrital zircons in southern West Greenland

Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures

The early Archaean Itsaq Gneiss Complex of southern West Greenland: the importance of field observations in interpreting age and isotopic constraints for early terrestrial evolution

Fifty years of the Eoarchean and the case for evolving uniformitarianism

Evolution of the Palaeozoic mafic-ultramafic Lizard Complex (SW England) from zircon and baddeleyite U-Pb-Hf isotopic constraints: New thoughts on the convergence of Avalonia and Armorica

The Itsaq Gneiss Complex of southern West Greenland; the world's most extensive record of early crustal evolution (3900-3600 Ma)

3710 and ⪖ 3790 Ma volcanic sequences in the Isua (Greenland) supracrustal belt; structural and Nd isotope implications

Review of the Isua supracrustal belt area (Greenland) Eoarchean geology from integrated 1:20,000 scale maps, field observations and laboratory data: Constraints on early geodynamics

Comparison of three cannulas for hysterosalpingography: a prospective, randomized study

The emergence of the Eoarchaean proto-arc: evolution of a c. 3700 Ma convergent plate boundary at Isua, southern West Greenland

In support of rare relict ∼3700 Ma stromatolites from Isua (Greenland)

Isua (Greenland) ~3700 Ma meta-serpentinite olivine Mg# and δ18O signatures show connection between the early mantle and hydrosphere: Geodynamic implications

3850 Ma BIF and mafic inclusions in the early Archaean Itsaq Gneiss Complex around Akilia, southern West Greenland? The difficulties of precise dating of zircon-free protoliths in migmatites

Adjacent terranes with ca. 2715 and 2650 Ma high-pressure metamorphic assemblages in the Nuuk region of the North Atlantic Craton, southern West Greenland: Complexities of Neoarchaean collisional orogeny

The Eoarchean legacy of Isua (Greenland) worth preserving for future generations

Earth's oldest mantle fabrics indicate Eoarchaean subduction

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