福建龙海牛头山新生代玄武岩橄榄岩包体的水

王蓉; 张保民

doi:10.3799/dqkx.2011.065

Volume 36 Issue 4

Jul. 2011

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WANG Rong, ZHANG Bao-min, 2011. Water in Peridotite Xenoliths from Niutoushan, Longhai, Fujian. Earth Science, 36(4): 635-642. doi: 10.3799/dqkx.2011.065

Citation:

WANG Rong, ZHANG Bao-min, 2011. Water in Peridotite Xenoliths from Niutoushan, Longhai, Fujian. Earth Science, 36(4): 635-642. doi: 10.3799/dqkx.2011.065

WANG Rong, ZHANG Bao-min, 2011. Water in Peridotite Xenoliths from Niutoushan, Longhai, Fujian. Earth Science, 36(4): 635-642. doi: 10.3799/dqkx.2011.065

Citation:

WANG Rong, ZHANG Bao-min, 2011. Water in Peridotite Xenoliths from Niutoushan, Longhai, Fujian. Earth Science, 36(4): 635-642. doi: 10.3799/dqkx.2011.065

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Water in Peridotite Xenoliths from Niutoushan, Longhai, Fujian

doi: 10.3799/dqkx.2011.065

WANG Rong^{1, 2
,},
ZHANG Bao-min²

1.
Faculty of Land Resource Engineering, Kuming University of Science and Technology, Kunming 650093, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2010-11-22
Publish Date: 2011-07-01

Abstract

Abstract

The analysis of infrared spectrum of pyroxene in lherzolite from peridotite xenoliths in Niutoushan, Longhai, Fujian, shows that there is water hosted in the pyroxene which exists by OH hydroxyl. The water content of clinopyroxene is (151－845)×10^-6, of orthopyroxene is (40－710)×10^-6, and of the whole rock (25－90)×10^-6 respectively. The water contents, both of pyroxene and of the whole rock, are higher than those in Nühan, Hannuoba and Subei basin, but are almost the same as those in Yangyuan. It demonstrates that pyroxene is the important reservoir in the upper mantle in Niutoushan. It may have experienced oceanic crust subduction and underplating in investigation locality.
- peridotite xenoliths,
- infrared spectroscopy,
- petrology

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References(57)

References

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Water in Peridotite Xenoliths from Niutoushan, Longhai, Fujian

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