scholarly article | Q13442814 |
P356 | DOI | 10.1038/NGEO2170 |
P2093 | author name string | Richard A. Stern | |
Larry M. Heaman | |||
Thomas Chacko | |||
Jesse R. Reimink | |||
P2860 | cites work | The composite Archaean grey gneisses: Petrological significance, and evidence for a non-unique tectonic setting for Archaean crustal growth | Q59664232 |
Formation of Paleoarchean continental crust through infracrustal melting of enriched basalt | Q59664239 | ||
High-precision oxygen isotope analysis of picogram samples reveals 2 m gradients and slow diffusion in zircon | Q60123596 | ||
Middle Archean continent formation by crustal delamination | Q67207842 | ||
Zircon megacrysts from kimberlite: oxygen isotope variability among mantle melts | Q69670310 | ||
Petrogenesis of Andesites | Q101012067 | ||
Partial melting of amphibolite/eclogite and the origin of Archean trondhjemites and tonalites | Q106232078 | ||
The oxidation state of Hadean magmas and implications for early Earth's atmosphere | Q34237087 | ||
Priscoan (4.00-4.03 Ga) orthogneisses from northwestern Canada | Q54007905 | ||
The Petrology of Thingmuli, a Tertiary Volcano in Eastern Iceland | Q55888371 | ||
Geology and zircon geochronology of the Acasta Gneiss Complex, northwestern Canada: New constraints on its tectonothermal history | Q55918503 | ||
4.2 Ga zircon xenocryst in an Acasta gneiss from northwestern Canada: Evidence for early continental crust | Q56609570 | ||
Silicic magma petrogenesis in Iceland by remelting of hydrothermally altered crust based on oxygen isotope diversity and disequilibria between zircon and magma with implications for MORB | Q57637935 | ||
Geochemical and Isotopic Evidence for Crustal Assimilation Beneath Krafla, Iceland | Q57846786 | ||
3.96 Ga gneisses from the Slave province, Northwest Territories, Canada | Q57877993 | ||
Role of oceanic plateaus in the initiation of subduction and origin of continental crust | Q58211322 | ||
Generation of trondhjemitic-tonalitic liquids and Archean bimodal trondhjemite-basalt suites | Q59263057 | ||
Effect of steeper Archean geothermal gradient on geochemistry of subduction-zone magmas | Q59609517 | ||
Forty years of TTG research | Q59664229 | ||
P433 | issue | 7 | |
P407 | language of work or name | English | Q1860 |
P921 | main subject | Iceland | Q189 |
P304 | page(s) | 529-533 | |
P577 | publication date | 2014-05-25 | |
P1433 | published in | Nature Geoscience | Q1337483 |
P1476 | title | Earth’s earliest evolved crust generated in an Iceland-like setting | |
P478 | volume | 7 |
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Q55029860 | Evidence of Enriched, Hadean Mantle Reservoir from 4.2-4.0 Ga zircon xenocrysts from Paleoarchean TTGs of the Singhbhum Craton, Eastern India. |
Q56610940 | Formation of Hadean granites by melting of igneous crust |
Q59926119 | In situ evidence for continental crust on early Mars |
Q59062859 | Low-temperature crystallization of granites and the implications for crustal magmatism |
Q57874987 | No evidence for Hadean continental crust within Earth’s oldest evolved rock unit |
Q64904758 | Record of low-temperature aqueous alteration of Martian zircon during the late Amazonian. |
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