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Tonalite-Trondhjemite-Granodiorite

Encyclopedia of Astrobiology

Synonyms

TTG

Definition

Tonalite-trondhjemite-granodiorite (or TTG suite, a term coined by Jahn et al. 1981) is an association of rocks that compose a large part of Archean continental crust. It is widely accepted that this rock suite formed by melting of hydrous metabasalts at high pressure, yet the geodynamic setting in which this melting took place is discussed. Two main sources of melt are proposed: (1) basaltic material that was previously underplated beneath thickened crust (e.g., Smithies 2000) and (2) basaltic rocks in subducting oceanic slabs that melted in a hotter Archean mantle (e.g., Martin et al. 2005).

Overview

About 90 % of the juvenile continental crust generated between 4.0 and 2.5 Ga belongs to the “TTG suite” (tonalite, trondhjemite, granodiorite) (Jahn et al. 1981; Moyen and Martin 2012), although in some cratons (e.g., Yilgarn Craton, Australia; Champion and Sheraton 1997), high-K monzodioritic and syenogranitic rocks can also be abundant. Most of these rocks are...

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References and Further Reading

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Correspondence to Hervé Martin .

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Martin, H., Arndt, N. (2014). Tonalite-Trondhjemite-Granodiorite. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_1620-5

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  • DOI: https://doi.org/10.1007/978-3-642-27833-4_1620-5

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Chapter history

  1. Latest

    Tonalite-Trondhjemite-Granodiorite
    Published:
    25 May 2021

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1620-6

  2. Original

    Tonalite-Trondhjemite-Granodiorite
    Published:
    29 April 2015

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1620-5