Later ordovician age of camptonite dike of agardak complex. South-Eastern Tuva as evidence of the presence plume magmatism at collisional orogeny

A. E. Izokh; G. V. Polyakov; V. G. Mal'kovets; R. A. Shelepaev; A. V. Travin; Yu K. Litasov; A. A. Gibsher

Later ordovician age of camptonite dike of agardak complex. South-Eastern Tuva as evidence of the presence plume magmatism at collisional orogeny

A. E. Izokh, G. V. Polyakov, V. G. Mal'kovets, R. A. Shelepaev, A. V. Travin, Yu K. Litasov, A. A. Gibsher

Research output: Contribution to journal › Article

Original language	English
Pages (from-to)	794-798
Number of pages	5
Journal	Doklady Akademii Nauk
Volume	378
Issue number	6
Publication status	Published - Dec 1 2001

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Izokh, A. E., Polyakov, G. V., Mal'kovets, V. G., Shelepaev, R. A., Travin, A. V., Litasov, Y. K., & Gibsher, A. A. (2001). Later ordovician age of camptonite dike of agardak complex. South-Eastern Tuva as evidence of the presence plume magmatism at collisional orogeny. Doklady Akademii Nauk, 378(6), 794-798.

Later ordovician age of camptonite dike of agardak complex. South-Eastern Tuva as evidence of the presence plume magmatism at collisional orogeny. / Izokh, A. E.; Polyakov, G. V.; Mal'kovets, V. G.; Shelepaev, R. A.; Travin, A. V.; Litasov, Yu K.; Gibsher, A. A.

In: Doklady Akademii Nauk, Vol. 378, No. 6, 01.12.2001, p. 794-798.

Research output: Contribution to journal › Article

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