О происхождении контрастной вулканической серии девона Атбаши-Кокшаальского района (Южный Тянь-Шань)

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О происхождении контрастной вулканической серии девона Атбаши-Кокшаальского района (Южный Тянь-Шань). / Biske, Yu S.; Tabuns, E. V.

In: Doklady. Earth science sections, Vol. 321 A, No. 9, 01.01.1994, p. 68-73.

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

BibTeX

@article{226ebeac95a44159bed1574a943834f6,

title = "О происхождении контрастной вулканической серии девона Атбаши-Кокшаальского района (Южный Тянь-Шань)",

abstract = "The opening of the Turkesttan ocean basin, on whose margins the folded-sheet structures of the Tyan-Shan were built up, occurred in the early Paleozoic. Much later, in Devonian time, volcanic eruptions occurred in the same area.",

author = "Biske, {Yu S.} and Tabuns, {E. V.}",

year = "1994",

month = jan,

day = "1",

language = "русский",

volume = "321 A",

pages = "68--73",

journal = "Doklady Earth Sciences",

issn = "1028-334X",

publisher = "МАИК {"}Наука/Интерпериодика{"}",

number = "9",

}

RIS

TY - JOUR

T1 - О происхождении контрастной вулканической серии девона Атбаши-Кокшаальского района (Южный Тянь-Шань)

AU - Biske, Yu S.

AU - Tabuns, E. V.

PY - 1994/1/1

Y1 - 1994/1/1

N2 - The opening of the Turkesttan ocean basin, on whose margins the folded-sheet structures of the Tyan-Shan were built up, occurred in the early Paleozoic. Much later, in Devonian time, volcanic eruptions occurred in the same area.

AB - The opening of the Turkesttan ocean basin, on whose margins the folded-sheet structures of the Tyan-Shan were built up, occurred in the early Paleozoic. Much later, in Devonian time, volcanic eruptions occurred in the same area.

UR - http://www.scopus.com/inward/record.url?scp=0028194409&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0028194409

VL - 321 A

SP - 68

EP - 73

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 9

ER -

ID: 49959475