Retrograde isochemical phase transformations of majoritic garnets included in 
diamonds: A case study of subcalcic Cr-rich majoritic pyrope from a Snap Lake 
diamond, Canada

Sobolev, N. V.; Wirth, R.; Logvinova, A. M.; Yelisseyev, A. P.; Kuzmin, D. V.

doi:10.1016/j.lithos.2016.07.030

Item

ITEM ACTIONSEXPORT

Add to Basket

Local TagsRelease HistoryDetailsSummary

Released

Journal Article

Retrograde isochemical phase transformations of majoritic garnets included in diamonds: A case study of subcalcic Cr-rich majoritic pyrope from a Snap Lake diamond, Canada

Authors

Sobolev, N. V.
External Organizations;

/persons/resource/wirth

Wirth, R.
4.3 Chemistry and Physics of Earth Materials, 4.0 Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Logvinova, A. M.
External Organizations;

Yelisseyev, A. P.
External Organizations;

Kuzmin, D. V.
External Organizations;

External Ressource

No external resources are shared

Fulltext (public)

There are no public fulltexts stored in GFZpublic

Supplementary Material (public)

There is no public supplementary material available

Citation

Sobolev, N. V., Wirth, R., Logvinova, A. M., Yelisseyev, A. P., Kuzmin, D. V. (2016): Retrograde isochemical phase transformations of majoritic garnets included in diamonds: A case study of subcalcic Cr-rich majoritic pyrope from a Snap Lake diamond, Canada. - Lithos, 265, 267-277.
https://doi.org/10.1016/j.lithos.2016.07.030

Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_1856890

Abstract

There is no abstract available