Naha, K. ; Majumdar, A. (1971) Reinterpretation of the Aravalli basal conglomerate at Morchana, Udaipur district, Rajasthan, western India Geological Magazine, 108 (2). pp. 111-114. ISSN 0016-7568
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Official URL: http://journals.cambridge.org/action/displayAbstra...
Related URL: http://dx.doi.org/10.1017/S0016756800051128
Abstract
The supposed Aravalli basal conglomerate near Morchana, considered to mark an erosional unconformity above the older Precambrian Banded Gneissic Complex in central Rajasthan, is a tectonic mélange in a terrain involved in superposed deformations. The supposed pebbles represent tectonic inclusions of various shapes, formed by isoclinal folding, stretching and disruption of concordant, pre- or early-kinematic vein quartz and rare pegmatite sheets in the Aravalli mica schist during the first folding.
| Item Type: | Article |
|---|---|
| Source: | Copyright of this article belongs to Cambridge University Press. |
| ID Code: | 31146 |
| Deposited On: | 05 Mar 2011 04:51 |
| Last Modified: | 09 Jun 2011 10:07 |
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