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- W2365626383 abstract "This contribution reviews on the chemical compositions of the mantle sources of carbonatites, mantle metasomatism, mechanisms of Partial melting in asthenospheric mantle and the evolution models for carbenatite magmas based on the occurrences, petrologic characteristics and Nd-Sr-Pb isotope and trace element data of the known carbonatites in the world and experiment Petrologic data. Carbonatite could not only be produced in extentional tectonic setting in lithosphere, such as continental rift, but also be formed in locally derivative spreading setting on a compressive tectonic background. The former is chalacterized by association with peralkaline rocks forming ring complexes and mainly is derived from the asthenospheric mantle as a nephelinitic ultrabasic-basic magmas and then through liquid immiciblity, but the later is characterized by its occurrence as a single lens and banded carbonatitic intrusion and/or extrusion along extentional lithospheric fractures resulted from continental collision and in such case carbenatite could directly be preduced by very small partial melting of the lithospheric mantle." @default.
- W2365626383 created "2016-06-24" @default.
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- W2365626383 date "1998-01-01" @default.
- W2365626383 modified "2023-09-25" @default.
- W2365626383 title "CARBONATITE: A PROBE ROCK FOR THE TECTONIC SETTINGS OF CONTINENTAL LITHOSPHERE AND MANTLE METASOMATISM" @default.
- W2365626383 hasPublicationYear "1998" @default.
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