Abstract
The Konthainhundi suite represents a syn to post orogenic calc-alkalic to alkalicalcic series. The rocks were a result of the collapse of a shallow level magma chamber aided by caldera subsidence.
This is a preview of subscription content, log in via an institution to check access.
Similar content being viewed by others
References
Bhattacharji S 1967J. Geol. 75 101
Buddington A F 1936 Gravity stratification as a criterion in the interpretation of structure of certain intrusives of the northwestern adirandacks; 16th Int. Geol. Congr. Rep. Washington, 1933, p. 347
Carmichael I S E, Turner F J and Verhoogan J 1974Igneous Petrol. (New York: McGraw Hill)
Jayaram S 1907Rec. Mysore Geology Dept. Vol. 8, Part 2, p. 73
Jayaram S 1913Rec. Mysore Geology Dept. Vol. 13, Part 2, p. 45
Johansen A 1937A descriptive petrology of igneous rocks (Chicago: University Press) Vols 1 and 2, p. 360
Peacock M A 1931J. Geol. 39 54
Ramakrishnan M and Mallikarjuna C 1976J. Geol. Soc. India 17 207
Wager L R and Brown G M 1968Layered igneous rocks (London: Oliver and Boyd) p. 588
Wager L R, Brown G M and Wadsworth W J 1960J. Petrol. 1 73
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Karkare, S.G., Ojha, R.K. & Srivastava, R.C. A note on the petrochemistry of the Konthainhundi pluton, District Mysore, Karnataka. Proc. Indian Acad. Sci. (Earth Planet Sci.) 93, 71–77 (1984). https://doi.org/10.1007/BF02863385
Received:
Revised:
Issue Date:
DOI: https://doi.org/10.1007/BF02863385