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• W2114840823 abstract "Mafic S-type granites of the Lachlan Fold Belt always contain a INTRODUCTION distinctive suite of enclaves, dominated by schists and gneisses of high Maas et al. (1997) have proposed complex models of metamorphic grade, generally with lesser numbers of microgranular crustal melting and magma mixing to account for the enclaves. Maas et al. (1997, Journal of Petrology 38, chemical and isotopic features of several kinds of enclaves 815–841) recently described enclaves from the S-type Deddick in the S-type Deddick Granodiorite of the Lachlan Fold Granodiorite. They concluded that the metasedimentary enclaves Belt (LFB), exposed at McKillops Bridge. That grancould be either source lithologies or accidental xenoliths, and that odiorite is a member of the Bullenbalong Suite (area the most common microgranular enclaves formed as globules of ~3100 km; White & Chappell, 1988), itself part of the hybrid magma that mingled with the host magma. All features of very extensive and slightly more diverse Bullenbalong the metasedimentary enclaves are consistent with an origin as lithic Supersuite (total area ~8750 km plus ~4000 km of restite fragments from the source, and their ubiquity in the mafic Svolcanic rocks); it occurs near the southern extremity of type granites and their rarity in both felsic varieties and in I-type those granites. These are the rocks that have been used granites conform with such an origin. The argument that these as primary examples of restite and of the restite model enclaves are not in chemical equilibrium with the host granite in S-type granites (Hine et al., 1976; White & Chappell, because they do not complement its composition is not valid, as they 1977; Chappell et al., 1987; Chappell, 1996b), and the represent less fertile parts of the source that did not melt to the point enclosed enclaves have been regarded by us as lithic of disaggregation. Unaltered cores of microgranular enclaves in the restite (White & Chappell, 1988; Chen et al., 1989; S-type granites have compositions that do not match those of any Chappell & White, 1991; White et al., 1991; Wyborn known igneous rock and an origin by metamorphism of a calcareous et al., 1991). sediment is probable. Partial melting during that metamorphism Maas et al. (1997) mostly reject the presence of restite accounts for the pseudo-igneous textures seen in these enclaves. enclaves in the Deddick Granodiorite. However, the" @default.
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• W2114840823 date "1999-03-01" @default.
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• W2114840823 title "Application of the Restite Model to the Deddick Granodiorite and its Enclaves --a Reinterpretation of the Observations and Data of Maas et al. (1997)" @default.
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• W2114840823 doi "https://doi.org/10.1093/petroj/40.3.413" @default.
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