Reply is made to several critical discussions published since the publication of the original paper in 1964 (for reference, see this Bibliography Vol. 29, Mookherjee 1; see also Vol. 29, Mookherjee 2; Vol. 30, Poddar 2; Vol. 31, No. 4, 02 E67-02447; Vol. 32, No. 1, 02 E68-00608). The deposit is regarded as a product of ascending hydrothermal solutions. Textural and geothermometric considerations militate against an origin by tectonic remobilization of wall-rock constituents. Differences of opinion on various aspects of structural and regional geology are discussed.

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