New Uranium-lead (U-Pb) Zircon Geochronology of Sholayar Alkaline Syenite Complex, Kerala: Significance of Cryogenian Magmatism from the Southern Granulite Terrane of the Indian Shield

Author:

Chowdhury Moumita12,Ray Jyotisankar1234,Tomson J.K.56,Sarkar Debaleena12,Patel Suresh C.78,Kumar Rajeev9,Mukherjee Pratik12,Sahoo Soumili12,Koeberl Christian1011

Affiliation:

1. Department of Geology 1 , , 35, Ballygunge Circular Road, Kolkata - 700 019 India

2. University of Calcutta 1 , , 35, Ballygunge Circular Road, Kolkata - 700 019 India

3. Department of Geology 6 , , Mohali - 140 306 India

4. Amity University Punjab 6 , , Mohali - 140 306 India

5. Isotope Geochemistry Facility 2 , , Thiruvananthapuram - 695 001 India

6. National Centre for Earth Science Studies 2 , , Thiruvananthapuram - 695 001 India

7. Department of Earth Sciences 3 , , Powai, Mumbai - 400 076 India

8. Indian Institute of Technology 3 , , Powai, Mumbai - 400 076 India

9. Geological Survey of India 4 , Faridabad - 121 001 India

10. Department of Lithospheric Research 5 , , Althanstrasse 14, A-1090 13 Vienna Austria

11. University of Vienna 5 , , Althanstrasse 14, A-1090 13 Vienna Austria

Abstract

ABSTRACT U-Pb age data from the leuco-syenite from the Sholayar Alkaline Syenite Complex (SASC) (10°17′59.9″N: 076°47′26.3″E) is presented in this study. The present sample contains alkali feldspar (orthoclase), oligoclasic plagioclase, diopsidic pyroxene, biotite and opaque minerals (magnetite and ilmenite). The modal data of constituent minerals is plotted over the IUGS classification diagram and the data plots fall within the syenite field. Obtained age (mean age 706.7 ± 8.4 Ma) largely corresponds to the Cryogenian period. In chondrite-normalized diagrams, the syenite shows some affinity towards well-studied silica over-saturated syenites of the Southern Granulite Terrane (SGT). The Ti-in zircon thermometry indicates the crystallization temperature in the range of 613° to 755°C. The reported zircon U-Pb age suggests evidence for Cryogenian alkaline magmatism in the SGT associated either with asthenospheric upwelling in an extensional setting or subduction related continental rifting.

Publisher

Geological Society of India

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