Subrahmanyam, N. P., Leelanandam, C. (1991) Geochemistry and Petrology of the Cumulophyric Layered Suite of Rocks from the Toa Pluton of the Mundwara Alkali Igneous Complex, Rajasthan. Journal Geological Society of India, 38 (4). 397-411 doi:10.17491/jgsi/1991/380405
Reference Type | Journal (article/letter/editorial) | ||
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Title | Geochemistry and Petrology of the Cumulophyric Layered Suite of Rocks from the Toa Pluton of the Mundwara Alkali Igneous Complex, Rajasthan | ||
Journal | Journal Geological Society of India | ||
Authors | Subrahmanyam, N. P. | Author | |
Leelanandam, C. | Author | ||
Year | 1991 (October 1) | Volume | 38 |
Page(s) | 397-411 | Issue | 4 |
Publisher | Geological Society of India | Place | Bangaluru, India |
URL | |||
DOI | doi:10.17491/jgsi/1991/380405Search in ResearchGate | ||
Generate Citation Formats | |||
Classification | Not set | LoC | Not set |
Mindat Ref. ID | 18218468 | Long-form Identifier | mindat:1:5:18218468:4 |
GUID | 0 | ||
Full Reference | Subrahmanyam, N. P., Leelanandam, C. (1991) Geochemistry and Petrology of the Cumulophyric Layered Suite of Rocks from the Toa Pluton of the Mundwara Alkali Igneous Complex, Rajasthan. Journal Geological Society of India, 38 (4). 397-411 doi:10.17491/jgsi/1991/380405 | ||
Plain Text | Subrahmanyam, N. P., Leelanandam, C. (1991) Geochemistry and Petrology of the Cumulophyric Layered Suite of Rocks from the Toa Pluton of the Mundwara Alkali Igneous Complex, Rajasthan. Journal Geological Society of India, 38 (4). 397-411 doi:10.17491/jgsi/1991/380405 | ||
In | (1991, October) Journal of the Geological Society of India Vol. 38 (4). Geological Society of India | ||
Abstract/Notes | Abstract The Toa layered suite ranges from feldspalhic peridotites to gabbros and gabbroic anorthosites. This suite differs from the Mer and MusaIa plutons in having coarse-grained cumulophyric rocks (with ubiquitous olivine) and scanty feldspathoidal dikes. Observed features are traceable to the high H2O content and high H2O/CO2 ratio of the parental liquid. High H2O content has reduced the viscosity of the magma by many orders of magnitude and facilitated rapid crystallization and settling of crystals leading to the formation of coarse-grained cumulophyric suite of rocks. With its selective reactivity to Si-O-Si bridges, H2O has depressed the activities of the saturated components (ab, or and qz) in the magma and led to the crystallization of considerable amounts of olivine from the silica-undersaturated components and consequently of feldspars (instead of feldspathoids). The depression of the liquidus of albite has facilitated the crystallization of more calcic feldspars leading to the formation of gabbroic anorthosites. A model of pulsed emplacement of magma is proposed to account (1) for the differing H2O and CO2 contents of the parental liquids of the Musala, Mer and Toa plutons, and (2) for the three different trends of differentiation in the three plutons which gave rise to an amazing variety of rock types in the Mundwara Complex. |
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