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Mundwara Alkali Igneous Complex, Rajasthan, India: Chronology and Sr Isotope Systematics


Affiliations
1 Geochemistry Division, KDMIPE, ONGC, Dehradun-248 195, India
2 Physical Research Laboratory, Ahmedabad - 380 009, India
3 Geology Department, M.L. Sukhadia University, Udaipur - 313 001, India
     

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Six whole rock samples have been dated by 40Ar/39Ar method to ascertain the emplacement time of the Mundwara Alkali Igneous Complex, Rajasthan, India. The dated samples include four from the Musala hill and one each from Mer and Toa hills of the complex. Out of these, only two syenite samples. viz. MR 86/4 and MR 86/7 from the Musala and Mer hills, respectively, have given plateaus at 64 Ma, while the remaining samples have exhibited saddle shaped spectra owing to the presence of excess argon. However, similar isochron ages of about 70 Ma obtained from a basalt (Musala hill) and a gabbro (Toa hill) by linear regression of all the data points might suggest initiation of igneolls activity at Mundwara around 70 Ma ago.

87Sr/86Sr ratios of this suite range from 0.70385 to 0.70551 indicating its derivation from a mantle source.


Keywords

Geochronology, Mundwara Alkali Igneous Complex, Rajasthan.
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  • Mundwara Alkali Igneous Complex, Rajasthan, India: Chronology and Sr Isotope Systematics

Abstract Views: 273  |  PDF Views: 4

Authors

S. S. Rathore
Geochemistry Division, KDMIPE, ONGC, Dehradun-248 195, India
T. R. Venkatesan
Physical Research Laboratory, Ahmedabad - 380 009, India
R. K. Srivastava
Geology Department, M.L. Sukhadia University, Udaipur - 313 001, India

Abstract


Six whole rock samples have been dated by 40Ar/39Ar method to ascertain the emplacement time of the Mundwara Alkali Igneous Complex, Rajasthan, India. The dated samples include four from the Musala hill and one each from Mer and Toa hills of the complex. Out of these, only two syenite samples. viz. MR 86/4 and MR 86/7 from the Musala and Mer hills, respectively, have given plateaus at 64 Ma, while the remaining samples have exhibited saddle shaped spectra owing to the presence of excess argon. However, similar isochron ages of about 70 Ma obtained from a basalt (Musala hill) and a gabbro (Toa hill) by linear regression of all the data points might suggest initiation of igneolls activity at Mundwara around 70 Ma ago.

87Sr/86Sr ratios of this suite range from 0.70385 to 0.70551 indicating its derivation from a mantle source.


Keywords


Geochronology, Mundwara Alkali Igneous Complex, Rajasthan.