Xenolith evidence for lithospheric melting above anomalously hot mantle under the northern Canadian Cordillera
Article Abstract:
The harzburgite xenoliths of seven mantle xenolith suites in the northern Canadian Cordillera formed by partial melting of the lower lithosphere in response to the rise of fluids and heat from anomalously hot asthenospheric mantle below. This was gleaned from a study of both major and trace element data from the seven suites. Findings show that there are two types of xenolith suites in the area, namely, unimodal suites comprised mainly of fertile lherzolite xenoliths and bimodal suites with both fertile lherzolites and refractory harzburgites.
Publication Name: Contributions to Mineralogy and Petrology
Subject: Earth sciences
ISSN: 0010-7999
Year: 1998
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Crustal contamination in early Basin-and-Range hawaiites of the Los Encinos Volcanic Field, central Mexico
Article Abstract:
A study of the mineral content in the Los Encinos Volcanic Field hawaiites in central Mexico reveals the existence of large quantities of megacrysts and xenocrysts and minimal amounts of rare granulite xenoliths in these hawaiites, which undergo elemental impacts of crustal contamination. However, unlike in other volcanic locations, lower crustal contamination in these hawaiites does not lead to barium accumulation, suggesting the possible extraction of elements such as thorium and uranium toward the volcanic surface by ascending magmas.
Publication Name: Contributions to Mineralogy and Petrology
Subject: Earth sciences
ISSN: 0010-7999
Year: 1995
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The relationship between the hawaiites and basalts of the Itcha Volcanic Complex, central British Columbia
Article Abstract:
Fractional crystallization from parental magmas is responsible for formation of the hawaiites and the Fe-rich alkali olivine basalt (AOB) lavas of the Itcha Volcanic Complex, central British Columbia. The process involves high-pressure fractionation of a clinopyroxene-dominated wehrlite assemblage. The presence of high Sr/Zr ratios in these rock types shows this. The Sr/Zr ratios are low in Fe-poor AOB lavas, evolving from AOB parental magmas at comparatively low pressures.
Publication Name: Contributions to Mineralogy and Petrology
Subject: Earth sciences
ISSN: 0010-7999
Year: 1995
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