Ti-rich hornblende in successively zoned amphibole from thermally metamorphosed basaltic rock in the Shionomisaki igneous complex
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- Makino Kuniaki
- Department of Geology, Faculty of Science, Shinshu University
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- Yanagida Takeshi
- Department of Geology, Faculty of Science, Shinshu University
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- Yamaguchi Yoshiaki
- Department of Geology, Faculty of Science, Shinshu University
Bibliographic Information
- Other Title
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- 潮岬火成複合岩体の熱変成玄武岩産累帯角閃石のTiに富むホルンブレンド
- Ti-rich hornblende in successively zone
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Abstract
Amphibole from thermally metamorphosed basalt in the Shionomisaki igneous complex, southwest Japan is successively zoned from edenite to Ti-rich hornblende through actinolite. The amphibole compositions show large compositional range of AlIV, which is strongly positively correlated with ΣA and Ti contents. Fe3+ content of the Ti-rich hornblende is estimated to be very low, based on routine amphibole structural constraints. Ti rich amphibole (kaersutite) from the upper-mantle is generally deficient in H+ of the O3 site, and is regarded as Ti replacing Al balanced by O2- for OH-. Infrared absorbance analyses indicate, however, that substitution of OH- by O2- in the O3 site is negligible in the Ti rich hornblende from thermally metamorphosed basaltic rock. Strong correlation between Ti and AlIV suggests that the conventional Ti-tschermakite substitution, R2++2Si Ti+2AlIV (R2+=Fe2++Mn+Mg), caused the Ti-incorporation, without the oxy substitution (OH- O2-) in the O3 site. The relationship between ΣA and AlIV implies that the edenite substitution is also dominant along the amphibole zoning.
Journal
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- Earth Science (Chikyu Kagaku)
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Earth Science (Chikyu Kagaku) 51 (3), 223-227, 1997
The Association for the Geological Collaboration in Japan
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Details 詳細情報について
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- CRID
- 1390001204266840576
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- NII Article ID
- 110004862342
- 10002219588
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- NII Book ID
- AN00141269
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- ISSN
- 21897212
- 03666611
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- NDL BIB ID
- 4215068
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- Text Lang
- en
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- Data Source
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- JaLC
- NDL
- CiNii Articles
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- Abstract License Flag
- Disallowed