Geology and geochemistry of metabasalts of Shimoga schist belt, Dharwar Craton: implications for the late Archean basin development

Author:

Boraiaha Chandan-KumarORCID,Ugarkar Annappa Ganpatrao,Kerr Andrew C.,Chandan Rashmi,Manuvachari Trivikram,Rajanna Shivaprasad

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference60 articles.

1. Balakrishnan S, Rajamani V, Hanson GN (1999) U–Pb ages for zircon and titanite from the Ramagiri area, southern India: evidence for accretionary origin of eastern Dharwar Craton during late Archean. J Geol 107:69–86

2. Bhaskar Rao YJ, Drury SA (1982) Incompatible trace element geochemistry of Archaean metavolcanic rocks from the Bababudan volcanic-sedimentary belt. Karnataka Geol Soc India 23:1–12

3. Chadwick B, Ramakrishnam M, Viswanatha MN (1981) Structural and metamor-phic relations between Sargur and Dharwar supracrustal rocks and Peninsular Gneiss in Central Karnataka. J Geol Soc India 22:557–569

4. Chadwick B, Vasudev VN, Jayaram S (1988) Stratigraphy and structure of late Archaean Dharwar volcanic and sedimentary rocks and their basement in a part of the Shimoga basin, east of Bhadravathi. Karnataka J Geol Soc India 32:1–19

5. Chadwick B, Vasudev VN, Krishna Rao B, Hegde GV (1991) The stratigraphy and structure of the Dharwar Supergroup adjacent to the Honnali dome: implications for late Archean basin development and regional structure in the western part of Karnataka. J Geol Soc India 38:457–484

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