The vast majority of garnet-bearing granites is s-type and was probably derived from partial melting of predominantly metasedimentary crustal rocks (
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The vast majority of garnet-bearing granites are S-type and were probably derived from partial melting of predominantly metasedimentary crustal rocks (Chappell and White, 1974; Clemens, 2003) although a few authors have questioned the whole concept of S-type granites (e.g. Kemp et al., 2007).
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