Monazite and xenotime U–Th–Pb $$_{\mathrm{total}}$$ total ages from basement rocks of the (central) Shillong–Meghalaya Gneissic Complex, Northeast India

Author:

Borah Pritom,Hazarika Pranjit,Mazumdar Amulya Chandra,Rabha Mridul

Funder

University Grants Commission

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference87 articles.

1. Bardoloi A, Mazumdar A C and Chowdhary P K 1994 Polyphase deformation and fold geometry study of the Precambrian Gneissic Complex around Nalanga hill, Goalpara district, Assam; Indian J. Earth Sci. 21 236–246.

2. Barooah B C and Goswami I D 1972 Precambrian stratigraphy of the Assam plateau; J. Mines Metals Fuels. 20 368–373.

3. Bea R 1996 Residence of REE, Y, Th and U in granites and crustal protoliths; Implications for the chemistry of crustal melts; J. Petrol. 37(3) 521–552.

4. Bhattacharjee C C and Baruah N C 1973 The study of joints in relation to the folding episodes in the Pre-Cambrian rocks of the Hahim area; J. Assam Sci. Soc. 16 54–62.

5. Bhattacharya A, Mazumdar A C and Sen S K 1988 Fe–Mg mixing in cordierite: Constraints from natural data and implications for cordierite–garnet thermometry in granulites; Am. Mineral. 73 338–344.

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