High- and Low-Temperature I-type Granites
نویسندگان
چکیده
منابع مشابه
Amphibole Chemistry in Low–temperature I–type Granites from Kashmar Area, Northeastern Central Iran Plate (CIP)
The Kashmar granitoid (43.5–42.4 Ma) forms an extensive part of iron–oxide type magmatic belt in northern side of the Doruneh Fault. It includes plutons of tonalite, granodiorite, granite and alkali feldspar granite which are metaluminous (ASI ≤ 1) in nature. They contain dominantly felsic minerals, representing I–type granites with low–temperature and low–pressure characteristics. According to...
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ژورنال
عنوان ژورنال: Resource Geology
سال: 1998
ISSN: 1344-1698,1751-3928
DOI: 10.1111/j.1751-3928.1998.tb00020.x