Garnet peridotite xenoliths from kimberlites of Finland: nature of the lithospheric mantle at Archaean craton - Palaeoproterozoic mobile belt transition

Peltonen, P.; Huhma, H.; Tyni, M.; Shimizu, Nobumichi

doi:10.29173/ikc2844

International Kimberlite Conference Extended Abstracts: 1998

DOI: 10.29173/ikc2844

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Garnet peridotite xenoliths from kimberlites of Finland: nature of the lithospheric mantle at Archaean craton - Palaeoproterozoic mobile belt transition

P. Peltonen¹,

H. Huhma²,

M. Tyni³

et al.

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Mantle transect of the Karelian Craton from margin to core based on P-T data from garnet and clinopyroxene xenocrysts in kimberlites

Lehtonen¹,

O’Brien²

2009

Bull Geol Soc Finland

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Peridotitic garnet and clinopyroxene xenocrysts from the 1.2 Ga Lentiira-Kuhmo and the 760 Ma Kuusamo kimberlite fields, emplaced within the Central Karelian Craton, have been studied using major and trace element geochemistry to obtain information on the stratigraphy, compositional variability, and evolutionary history of the underlying lithospheric mantle. An earlier study on the 600 Ma Kaavi-Kuopio kimberlite field showed that near the SW margin of the craton the 230-km-thick subcontinental lithospheric mantle (SCLM) exhibits a well-developed 3-layer structure indicative of episodic construction.

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Mantle transect of the Karelian Craton from margin to core based on P-T data from garnet and clinopyroxene xenocrysts in kimberlites

Lehtonen¹,

O’Brien²

2009

Bull Geol Soc Finland

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show abstract

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Garnet peridotite xenoliths from kimberlites of Finland: nature of the lithospheric mantle at Archaean craton - Palaeoproterozoic mobile belt transition

Cited by 1 publication

References 1 publication

Mantle transect of the Karelian Craton from margin to core based on P-T data from garnet and clinopyroxene xenocrysts in kimberlites

Mantle transect of the Karelian Craton from margin to core based on P-T data from garnet and clinopyroxene xenocrysts in kimberlites

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