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Rama Rao, B.
- The "Champion Gneiss" in the Archaean Complex of Mysore, Southern India - A Review
Authors
1 Former Director of Geology in Mysore, Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 2, No 0 (1961), Pagination: 31-38Abstract
Smeeth's classification of the granites and granitic gneisses comprising the major portion of the Archaean Complex of Mysore, into 4 separate epochs of plutonic intrusions starting with the" Champion Gneiss" as the earliest granitic intrusion into the Dharwar System, and his views that each of those intrusions comprise several types resulting from magmatic differentiation and crystallisation need some modifications as the author has already previously pointed out. This paper specially deals with the" Champion Gneiss"; and its position as an independent epoch of granitic intrusion is briefly reviewed and discussed.
Attention is drawn to the fact that the indiscriminate extension of the term "Champion Gneiss"-(the name originally given by Smeeth to a fine grained, opalescent quartz bearing micaceous gneiss, which he believed to be the highly crushed phase of the earliest granitic intrusion into the Dharwar System) to include several other types of schistose acidic and basic rocks which contain such opalescent quartz,:and even to some granites and other rock types which do not contain it, has led to much confusion in the classification, correlation, and correct interpretation of the origin of those types. Describing briefly the chief characteristics of the various types of rocks which have been included under the comprehensive term "Champion Gneiss", the author has now defined the term "Champion Gneiss". discarding from the group several types which cannot by any means be considered as granitic variants. The name is to be restricted only to the island-like exposures of granitic rocks within the schist belts, with their finer-grained marginal types and their undoubted crushed and altered phases.
The granites of this series are considered to have come up or intruded throwing aside their covers and crystallised directly from molten material (magma); the regions where we may expect to find the basement rocks of the Dharwar System, are also indicated.
- The Archaean Provinces of India and their Comparison with those of Other Continental Shields
Authors
1 Bangalore, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 5 (1964), Pagination: 55-71Abstract
Doubts still exist in regard to the precise correlation of the Archaean formations in the different regions of the Indian Shield, either with one another or with those of other continental shield areas. In this paper the information available at present on the composition, classification and correlation of the Archaean formations in the several pre-Cambrian shields of the world is briefly reviewed, and a broad generalised correlation based on their absolute ages is given. The rock formations older than the Cambrians, which range in their absolute ages from about 600 to 3,500 million years as shown by radiometric determinations, have been classified broadly into 8 age groups and standard names have been suggested for each of the groups.- Development of an Integrated Pest Management Module for Cotton in Andhra Pradesh
Authors
1 Regional Agricultural Research Station, Lam Farm, Guntur-522 034, Andhra Pradesh, IN