The vast majority of garnet-bearing granites is s-type and was probably derived from partial melting of predominantly metasedimentary crustal rocks (
Answers
Answered by
29
Answer:
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).
Similar questions
Physics,
5 months ago
Environmental Sciences,
10 months ago
English,
10 months ago
Biology,
1 year ago
Math,
1 year ago