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

ARC Centre of Excellence for Core to Crust Fluid Systems (incorporation ARC National Key Centre for Geochemical evolution and Metallogeny of Continents (GEMOC))

Research output: Contribution to journal › Article › peer-review

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

Cite this

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title = "Later Ordovician age of camptonite dike of agardak complex. South-Eastern Tuva as evidence of the presence plume magmatism at collisional orogeny",

author = "Izokh, \{A. E.\} and Polyakov, \{G. V.\} and Mal'kovets, \{V. G.\} and Shelepaev, \{R. A.\} and Travin, \{A. V.\} and Litasov, \{Yu K.\} and Gibsher, \{A. A.\}",

year = "2001",

language = "Russian",

volume = "378",

pages = "794--798",

journal = "Doklady Akademii Nauk",

issn = "0869-5652",

publisher = "National Academy of Sciences",

number = "6",

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TY - JOUR

T1 - Later Ordovician age of camptonite dike of agardak complex. South-Eastern Tuva as evidence of the presence plume magmatism at collisional orogeny

AU - Izokh, A. E.

AU - Polyakov, G. V.

AU - Mal'kovets, V. G.

AU - Shelepaev, R. A.

AU - Travin, A. V.

AU - Litasov, Yu K.

AU - Gibsher, A. A.

PY - 2001

Y1 - 2001

UR - https://www.scopus.com/pages/publications/0345095362

M3 - Article

AN - SCOPUS:0345095362

SN - 0869-5652

VL - 378

SP - 794

EP - 798

JO - Doklady Akademii Nauk

JF - Doklady Akademii Nauk

IS - 6

ER -

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

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