| Reference Type | Journal (article/letter/editorial) |
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| Title | Delhi Volcanics in Parts of Central Rajasthan and their Significance |
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| Journal | Journal Geological Society of India |
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| Authors | Gupta, P. | Author |
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| Mukhopadhyay, K. | Author |
| Bose, Utpal | Author |
| Year | 1988 (March 1) | Volume | 31 |
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| Page(s) | 314-327 | Issue | 3 |
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| Publisher | Geological Society of India | Place | Bangaluru, India |
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| URL | |
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| DOI | doi:10.17491/jgsi/1988/310304Search in ResearchGate |
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| Generate Citation Formats |
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| Classification | Not set | LoC | Not set |
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| Mindat Ref. ID | 17911184 | Long-form Identifier | mindat:1:5:17911184:6 |
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| GUID | 0 |
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| Full Reference | Gupta, P., Mukhopadhyay, K., Bose, Utpal (1988) Delhi Volcanics in Parts of Central Rajasthan and their Significance. Journal Geological Society of India, 31 (3). 314-327 doi:10.17491/jgsi/1988/310304 |
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| Plain Text | Gupta, P., Mukhopadhyay, K., Bose, Utpal (1988) Delhi Volcanics in Parts of Central Rajasthan and their Significance. Journal Geological Society of India, 31 (3). 314-327 doi:10.17491/jgsi/1988/310304 |
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| In | (1988, March) Journal of the Geological Society of India Vol. 31 (3). Geological Society of India |
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| Abstract/Notes | Abstract
The Proterozoic Delhi Supergroup of rocks along the Aravalli orographic axis in central Rajasthan encloses thick linear piles of syn-sedimentary volcanics. The volcanies are low-potassic oceanic tholeiites derived from mantle source. The repository basin was ensialic to start with and was partially rifted to facilitate magma upwelling concomitant with sedimentation. Structural stratigraphic and chemical characters of the volcanics militate against the possibility of its being allochthonous slices of an oceanic crust. |
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