Cited by 247Geological and Geochemical AnalysisGeochemistry and Elemental AnalysisAstro and Planetary Science

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The mechanisms of petrogenesis of the Archaean continental crust—Comparison with modern processes

Martin, Hervé·1993·Lithos

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Crossref · 10.1016/0024-4937(93)90046-f

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References 119 · Cited by 247

Research works printed but not linked: 13

  1. Allègre, 1985, The evolving Earth system, Terra Cognita, 5, 5
  2. Evans, 1992, Most late Archaean tonalites, trondhjemites and granodiorites (TTG) in the SW Superior Province were derived from mantle melts, not by melting of basalts, AGU abstract V22D-3, 330
  3. Jégouzo, 1991, Thrusting, crustal thickening and granite formation in the Archaean of eastern Finland, Terra Abstracts, 3, 33
  4. Martin, 1986, Effect of steeper Archaean geothermal gradient on geochemistry of subduction-zone magmas, Geology, 14, 753, 10.1130/0091-7613(1986)14<753:EOSAGG>2.0.CO;2 · DOI
  5. Martin, 1991, Unsegment de croûte continentale d'âge archéen ancien, (3,4 milliards d'années. Le massif de Sete-Voltas (Bahia, Brésil), C. R. Acad. Sci. Paris, 313, 531
  6. Mc Culloch, 1992, Partial melting versus dehydration of subducted slabs and the Pb paradox, Abstracts of the 29th I.G.C. Kyoto, 1638, 181
  7. Mueller, 1983, Incompatible element rich andesitic amphibolites from the Archaean of Montana and Wyoming: evidence for mantle metasomatism, Geology, 11, 203, 10.1130/0091-7613(1983)11<203:IAAFTA>2.0.CO;2 · DOI
  8. Mueller, 1988, Evidence for Archaean subduction and crustal recycling, Wyoming province, Geology, 16, 871, 10.1130/0091-7613(1988)016<0871:EFASAC>2.3.CO;2 · DOI · Paper page
  9. Nisbet, 1983, Model for Archaean plate tectonics, Geology, 11, 376, 10.1130/0091-7613(1983)11<376:MFAPT>2.0.CO;2 · DOI
  10. Ronov, 1976, A new model for the chemical structure of the Earth's crust, Geochim. Int., 13, 89
  11. Stern, 1982, An Andean andesite derived directly from subducted MORB or from LIL depleted subcontinental mantle, Trans. Am. Geophys. Union, 63, 1148
  12. Taylor, 1988, Light rare-earth enrichment of supra subduction-zone mantle: evidence from the Troodos ophiolite, Cyprus, Geology, 16, 448, 10.1130/0091-7613(1988)016<0448:LREEOS>2.3.CO;2 · DOI · Paper page
  13. Wolf, 1989, The formation of tonalitic liquids during vapour-absent partial melting of amphibolite at 10 kb (abstract), Eos Trans. AGU, 70, 506

Metadata

Authors
Martin, H.
Affiliations
Centre National de la Recherche Scientifique (FR)
Corresponding author
Martin, Hervé
Venue
Lithos
Publisher
Elsevier BV
Published
1993-09
Volume
30
Issue
3-4
Pages
373-388
ISSN
0024-4937 (ISSN-L)
OpenAlex
W1969870923
Cited by
247
References
119
Citations by year
2026: 5 · 2025: 4 · 2024: 4 · 2023: 7 · 2022: 10 · 2021: 9 · 2020: 15 · 2019: 8 · 2018: 10 · 2017: 8 · 2016: 6 · 2015: 7 · 2014: 5 · 2013: 8 · 2012: 12
FWCI
6.41
Type
journal article
Language
en
Open access
closed
Locations
Lithos (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
Keywords
petrogenesis, komatiite, rare earth elements, ytterbium, garnet, hornblende, partial melting, subduction zone, mantle wedge partial melting, slab dehydration, geothermal gradient, Benioff zone, continental crustal growth

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