Lamprophyres from the Harohalli dyke swarm in the Halaguru and Mysore areas, Southern India: Implications for backarc basin magmatism

Author:

Lanjewar Shubhangi,Randive Kirtikumar

Funder

National Centre for Antarctic and Ocean Research

Ministry of Earth Sciences, Goa

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference67 articles.

1. U-Pb ages for zircon and titanite from the Ramagiri area, southern India: Evidence for accretionary origin of the Eastern Dharwar Craton during the late Archean;Balakrishnan;J. Geol.,1999

2. Petrological. Geochemical and isotopic characteristics of potassic and ultrapotassic magmatism in Central- southern Italy: inference on its genesis and on the nature of mantle sources;Conticelli;Period. di Mineral.,2004

3. A procedure for geochemical interpretation of terrestrial rare- earth abundance patterns;Coryell;J. Geophys. Res.,1963

4. Devaraju, T.C., Laajoki, K., Makkonen, H., Khandali, S.D., Ugarkar, A.G., Jamkhindi, M.S.R., 1995a. Neo-proterozoic Dyke swarms of Southern Karnataka. Part I: Field characters, petrography and Mineralogy. In: Memoir Geological Society of India No. 33, pp. 209–265.

5. Neo-proterozoic Dyke swarms of Southern Karnataka. Part II: geochemistry, oxygen isotope composition, Rb-Sr age and petrogenesis;Devaraju;Mem. Geol. Soc. India,1995

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