Skip Nav Destination
Omphacite paradox in mantle peridotites
Russ. Geol. Geophys. (2015) 56 (11): 1568–1577.
This article has been cited by the following articles in journals that are participating in CrossRef Cited-by Linking.
Origin of V. Grib pipe eclogites (Arkhangelsk region, NW Russia): geochemistry, Sm-Nd and Rb-Sr isotopes and relation to regional Precambrian tectonics
- Elena V. Shchukina
- Aleksey M. Agashev
- Natalia G. Soloshenko
- Mariya V. Streletskaya
- Dmitry A. Zedgenizov
Mineralogy and Petrology (2019) 113 (5): 593.
Three types of element fluxes from metabasite into peridotite in analogue experiments: Insights into subduction-zone processes
- A.L. Perchuk
- V.O. Yapaskurt
- W.L. Griffin
- M.Yu. Shur
- S.E.M. Gain
Lithos (2018) 302-303: 203.
Indicator reactions of K and Na activities in the upper mantle: Natural mineral assemblages, experimental data, and thermodynamic modeling
- O. G. Safonov
- V. G. Butvina
Geochemistry International (2016) 54 (10): 858.