2012
DOI: 10.5647/jsoee.21.3_64
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Availability of Mantle Carbon as an Educational Resource for Environmental Education

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Cited by 1 publication
(2 citation statements)
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“…The P-T conditions recorded in the fluid inclusions are consistent with those for a boundary between plagioclase and spinel lherzolite (0.7 ± 0.1 GPa and 900 °C, Borghini et al 2010). Yamamoto et al (2012) has also estimated the depths of Ichinomegata mantle xenoliths using fluid inclusions and reports that the depths of origin for the Ichinomegata mantle xenoliths are 27.4-36.5 km.…”
Section: Properties Recorded In Fluid Inclusionsmentioning
confidence: 51%
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“…The P-T conditions recorded in the fluid inclusions are consistent with those for a boundary between plagioclase and spinel lherzolite (0.7 ± 0.1 GPa and 900 °C, Borghini et al 2010). Yamamoto et al (2012) has also estimated the depths of Ichinomegata mantle xenoliths using fluid inclusions and reports that the depths of origin for the Ichinomegata mantle xenoliths are 27.4-36.5 km.…”
Section: Properties Recorded In Fluid Inclusionsmentioning
confidence: 51%
“…The petrology of Ichinomegata peridotite xenoliths has been studied by several researchers (Kuno 1967;Aoki 1971;Takahashi 1978Takahashi , 1980Takahashi , 1986Abe et al 1992Abe et al , 1998. While a short reports exist on the CO 2 /H 2 O ratios of the fluid inclusions (Trial et al 1984;Yamamoto et al 2012), the chemical composition and origin of the fluids remain to be fully investigated.…”
Section: Introductionmentioning
confidence: 98%