Journal
LITHOS
Volume 208, Issue -, Pages 378-392Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.lithos.2014.08.023
Keywords
Garnet; Aplite; Pegmatite; LA-ICP-MS; IRMS; Iran
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Funding
- Science and Research Branch
- University of Texas at Austin
- University of Cape Town
- NRF (South Africa)
- Institute for Research on Earth Evolution (Yokosuka, Japan)
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Triassic monzogranites and granodiorites of the Khajeh Morad region in northeastern Iran are cut by two types of garnet-bearing intrusive veins: (1) aplite and (2) granitic pegmatite. The former is composed of quartz, feldspar, muscovite, with minor garnet, biotite, and ilmenite. The latter contains quartz, plagioclase (+/- quartz and muscovite inclusions), alkali feldspar, and muscovite, with minor amounts of garnet, tourmaline, beryl, columbite, and ilmenite. Garnet in both rock types has MnO > 12 wt.% and CaO
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