Abstract
Detrital zircons as old as nearly 4.4 Ga offer insights into the earliest moments of Earth history. Results of geochemical investigations of these grains have been interpreted to indicate their formation in near-H2O saturated meta- and peraluminous magmas under a relatively low (15–30 °C/km) geotherm. A key feature in pursuing a petrotectonic model that explains the full spectrum of these observations is their seeming contrast to most Phanerozoic magmatic zircons, specifically their low Ti-in-zircon crystallization temperatures and inclusion assemblages. The ~22 Ma Arunachal leucogranites of the eastern Himalaya appear, however, to be a rare exception to this generality. They show large-ion lithophile covariance trends indicative of wet basement melting together with a normal distribution of magmatic crystallization temperatures about an average of 660 °C. In the same fashion as Hadean zircons, Arunachal leucogranite and host gneiss zircons are dominated by muscovite + quartz inclusions that yield formation pressures of 5–15 kbars. We suggest that the Arunachal leucogranites originated in the hanging wall of a megathrust that carried H2O-rich foreland sediments to depths of >20 km whereupon de-watering reactions released fluids that fluxed hanging wall anatexis. Modeling suggests the thermal structure of this continental collision environment may have been broadly similar to a Hadean ocean-continent subduction zone. The similarity of these two environments, separated by over 4 Ga may explain seemingly common features of the Hadean and Arunachal leucogranite zircons. Their key difference is the absence of metaluminous magmas in the continental collision environment, which is shielded from juvenile additions.
Special collection papers can be found online at http://www.minsocam.org/MSA/AmMin/special-collections.html.
Acknowledgments
The ion microprobe facility at UCLA is partly supported by a grant from the Instrumentation and Facilities Program, Division of Earth Sciences, National Science Foundation. This research was conducted with support from grants to T.M.H. from NSF-EAR’s Petrology/Geochemistry and Continental Dynamics Programs. We thank Frederic Herman, Michelle Hopkins-Wielicki, and Oscar Lovera for advice and technical assistance and Nigel Harris and Amos Aikman for critical readings.
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- Invited Centennial Article
- On the nature and significance of rarity in mineralogy
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- Special collection: advances in ultrahigh-pressure metamorphism
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- Special collection: perspectives on origins and evolution of crustal magmas
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- From the Hadean to the Himalaya: 4.4 Ga of felsic terrestrial magmatism
- Spinels renaissance: the past, present, and future of those ubiquitous minerals and materials
- Compositional effects on the solubility of minor and trace elements in oxide spinel minerals: insights from crystal-crystal partition coefficients in chromite exsolution
- Spinels renaissance: the past, present, and future of those ubiquitous minerals and materials
- An X-ray magnetic circular dichroism (XMCD) study of Fe ordering in a synthetic MgAl2O4-Fe3O4 (spinel-magnetite) solid-solution series: Implications for magnetic properties and cation site ordering
- Research Article
- High concentrations of manganese and sulfur in deposits on Murray Ridge, Endeavour Crater, Mars
- Research Article
- A Cr3+ luminescence study of spodumene at high pressures: effects of site geometry, a phase transition, and a level-crossing
- Research Article
- Phase transitions between high- and low-temperature orthopyroxene in the Mg2Si2O6-Fe2Si2O6 system
- Research Article
- High-temperature and high-pressure behavior of carbonates in the ternary diagram CaCO3-MgCO3-FeCO3
- Research Article
- Natural Mg-Fe clinochlores: enthalpies of formation and dehydroxylation derived from calorimetric study
- Research Article
- Trace element thermometry of garnet-clinopyroxene pairs
- Research Article
- Constraints on the solid solubility of Hg, Tl, and Cd in arsenian pyrite
- Research Article
- Ni-phyllosilicates (garnierites) from the Falcondo Ni-laterite deposit (Dominican Republic): mineralogy, nanotextures, and formation mechanisms by HRTEM and AEM
- Research Article
- Cu diffusion in a basaltic melt
- Research Article
- High-pressure behavior of the polymorphs of FeOOH
- New Mineral Names
- New Mineral Names
Articles in the same Issue
- Invited Centennial Article
- On the nature and significance of rarity in mineralogy
- Special collection: mechanisms, rates, and timescales of geochemical transport processes in the crust and mantle
- Zircon saturation and Zr diffusion in rhyolitic melts, and zircon growth geospeedometer
- Review
- On silica-rich granitoids and their eruptive equivalents
- Special collection: advances in ultrahigh-pressure metamorphism
- Discovery of in situ super-reducing, ultrahigh-pressure phases in the Luobusa ophiolitic chromitites, Tibet: new insights into the deep upper mantle and mantle transition zone
- Special collection: from magmas to ore deposits
- Uraninite from the Olympic Dam IOCG-U-Ag deposit: linking textural and compositional variation to temporal evolution
- Special collection: from magmas to ore deposits
- A story of olivine from the McIvor Hill complex (Tasmania, Australia): Clues to the origin of the Avebury metasomatic Ni sulfide deposit
- Special collection: perspectives on origins and evolution of crustal magmas
- The origin of extensive Neoarchean high-silica batholiths and the nature of intrusive complements to silicic ignimbrites: Insights from the Wyoming batholith, U.S.A.
- Special collection: perspectives on origins and evolution of crustal magmas
- From the Hadean to the Himalaya: 4.4 Ga of felsic terrestrial magmatism
- Spinels renaissance: the past, present, and future of those ubiquitous minerals and materials
- Compositional effects on the solubility of minor and trace elements in oxide spinel minerals: insights from crystal-crystal partition coefficients in chromite exsolution
- Spinels renaissance: the past, present, and future of those ubiquitous minerals and materials
- An X-ray magnetic circular dichroism (XMCD) study of Fe ordering in a synthetic MgAl2O4-Fe3O4 (spinel-magnetite) solid-solution series: Implications for magnetic properties and cation site ordering
- Research Article
- High concentrations of manganese and sulfur in deposits on Murray Ridge, Endeavour Crater, Mars
- Research Article
- A Cr3+ luminescence study of spodumene at high pressures: effects of site geometry, a phase transition, and a level-crossing
- Research Article
- Phase transitions between high- and low-temperature orthopyroxene in the Mg2Si2O6-Fe2Si2O6 system
- Research Article
- High-temperature and high-pressure behavior of carbonates in the ternary diagram CaCO3-MgCO3-FeCO3
- Research Article
- Natural Mg-Fe clinochlores: enthalpies of formation and dehydroxylation derived from calorimetric study
- Research Article
- Trace element thermometry of garnet-clinopyroxene pairs
- Research Article
- Constraints on the solid solubility of Hg, Tl, and Cd in arsenian pyrite
- Research Article
- Ni-phyllosilicates (garnierites) from the Falcondo Ni-laterite deposit (Dominican Republic): mineralogy, nanotextures, and formation mechanisms by HRTEM and AEM
- Research Article
- Cu diffusion in a basaltic melt
- Research Article
- High-pressure behavior of the polymorphs of FeOOH
- New Mineral Names
- New Mineral Names