Thermobarometry of Ca-amphibole in a Typical Low–temperature I-type Granite from Kashmar, Iran
The Kashmar granitoid (42.5 Ma) occurs in NE Central Iran Plate (CIP). It mainly includes felsic metaluminous (ASI ≤ 1) I–type granite and granodiorite plutons. Microprobe analyses show that the Kashmar amphiboles are low in Ti and (Na+K)A contents (all < 0.5 apfu), indicating magnesio–hornblende...
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| Format: | Article |
| Language: | fas |
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Shahid Rajaee Teacher Training University (SRTTU)
2007-03-01
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| Series: | Fanāvarī-i āmūzish |
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| Online Access: | https://jte.sru.ac.ir/article_1252_f9e8afa965ee2c5fdb3a198de99a8ef1.pdf |