The Mannapra syenite, Central Kerala, India: Geochemistry, petrogenesis and bearing on anorogenic magmatism

Details The Mannapra syenite, Central Kerala, India: Geochemistry, petrogenesis and bearing on anorogenic magmatism The Mannapra syenite, Central Kerala, India: Geochemistry, petrogenesis and bearing on anorogenic magmatism

Mar 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985ineps..94...43s&link_type=abstract

Proceedings of the Indian Academy of Sciences - Earth and Planetary Sciences, Volume 94, Issue 1, pp.43-56

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Syenite, Mineralogy, Geochemistry, Petrogenesis, Subsolidus Reequilibration, Anorogenic Magmatism

Scientific paper

Occurrence of a syenite body near Mannapra, Trichur district, Kerala, is reported. The syenite, emplaced within charnockitic country rocks along the Idamalayar faultlineament, is exposed over an area of 8 km2. The rock, classified as quartz alkali feldspar syenite based on Q-A-P proportions, has alkali feldspar as the dominant mineral constituent which shows variation in perthitic texture from crypto- to micro- and patch-perthites. Both ortho- and clino-pyroxenes are present, with the former showing blebs of plagioclase suggesting Al-unmixing. Clinopyroxene shows subsolidus reequilibration with greenish pleochroic grain margins and local conversion to alkali amphibole. The petrochemical characters indicate that the syenite crystallized from a partial melt which equilibrated from K-rich, Rb-depleted source in the upper mantle, in response to crustal distension and mantle degassing prior to the rifting of the continent. Reaction between early formed minerals and the late peralkaline liquid towards the residual phase resulted in subsolidus reequilibration textures. The syenite is envisaged to be yet another example of the manifestation of anorogenic magmatism in this part of the Indian shield.

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