Results 61 to 70 of about 388 (174)
Neoproterozoic Samalpatti and Cretaceous-Paleogene Amba Dongar massifs are considered to evaluate the change of sources of carbonatite magmatism in evolving tectonosphere of India. The inherited character of Ba and Sr distribution components is traced in
S. V. Rasskazov +4 more
doaj +1 more source
Origin of carbonatites-liquid immiscibility caught in the act. [PDF]
Berndt J, Klemme S.
europepmc +1 more source
Mass balance of complementary metasomatic processes using isocon analysis. [PDF]
Kozlov EN, Fomina EN.
europepmc +1 more source
A statistical regression analysis was performed of a summary of borrowed literary iso- topic data on 176 carbonatite occurrences worldwide (a total of 1829 paired δ18О-δ13С values in primary carbonatites).
Bolonin A. V.
doaj +1 more source
Calcium isotope compositions as a means to trace carbonate recycling. [PDF]
Huang S, Jacobsen SB.
europepmc +1 more source
Petrogenesis of juvenile pelletal lapilli in ultramafic lamprophyres. [PDF]
Prokopyev I +5 more
europepmc +1 more source
Linking deep CO2 outgassing to cratonic destruction. [PDF]
Wang ZX, Liu SA, Li S, Liu D, Liu J.
europepmc +1 more source
Carbonatites in skarn objects of the Urals
The temperature range of the formation of skarns suggests the melting of limestones in the heat-and-mass transfer columns of the Earth’s crust. The ontogenic analysis of structures of the carbonate rocks in some Ural skarn objects indicates the presence ...
V. A. Popov
doaj
Partitioning of REE between calcite and carbonatitic melt containing P, S, Si at 650-900 °C and 100 MPa. [PDF]
Chebotarev DA +2 more
europepmc +1 more source

