Petrology of peridotite xenoliths in lamprophyre from Shingu, Southwestern Japan: Implications for origin of Fe-rich mantle peridotites-Reference-Cited by-同舟云学术

Petrology of peridotite xenoliths in lamprophyre from Shingu, Southwestern Japan: Implications for origin of Fe-rich mantle peridotites

Published:1987-10 Issue:2 Volume:37 Page:137-155
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Mineralogy and Petrology

Author:

Goto Kiyoshi,Arai Shoji

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF01164188.pdf

Reference33 articles.

1. Aoki K, Prinz M (1974) Chromian spinels in lherzolite inclusions from Itinome-gata, Japan. Contrib Mineral Petrol 46: 249?256

2. Arai S (1984) Pressure-temperature dependent compositional variation of phlogopitic micas in upper mantle peridotites. Contrib Mineral Petrol 87: 260?264

3. ?? (1986): K/Na variation in phlogopite and amphibole of upper mantle peridotites due to fractionation of the metasomatizing fluids. J Geol 94: 436?444

4. ?? (1987): An estimation of the least depeleted spinel peridotite on the basis of olivinespinel mantle array. N Jb Miner Mh H 8: 347?354

5. ??Hirai H (1983) Petrographical notes on deep-seated and related rocks (1) Mantle peridotites from Kurose and Noyamadake alkali basalts, southwestern Japan. Ann Rep Inst Geosci Univ Tsukuba 9:65?67

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