Восточный (Китайский) сегмент Южного Тянь-Шаня: коллизионная структура и главные палеозойские события

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Восточный (Китайский) сегмент Южного Тянь-Шаня: коллизионная структура и главные палеозойские события. / Biske, Y. S.

In: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Vol. 7, No. 3, 01.12.1998, p. 3-13.

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

BibTeX

@article{4bcf013e502f487cbafc60cd2f57a310,

title = "Восточный (Китайский) сегмент Южного Тянь-Шаня: коллизионная структура и главные палеозойские события",

abstract = "Structural design of Southern (Variscian) Tien Shan in the Eastern segment consists, south to north, of: 1) broken border of Tarim paleocontinent; 2) upper Paleozoic frontal basin; 3) volcanics and sediments of Turkestan ocean with ophiolites and some signs of nappe tectonics on initial stages of collision; 4) island arc unite (terraine) of Erben-Kumyshtala; 5) collisional suture on southern limit of Jili microcontinent, as a part of Paleokazakhstan. Collision of Erben-Kumyshtala with Paleokazakhstan border happened about Devonian/Carboniferous limit, but did not close Turkestan ocean. This event took place only at Late Carboniferous all along northern border of Tarim paleocontinent.",

author = "Biske, {Y. S.}",

year = "1998",

month = dec,

day = "1",

language = "русский",

volume = "7",

pages = "3--13",

journal = "Вестник Санкт-Петербургского университета. Науки о Земле",

issn = "2541-9668",

publisher = "Издательство Санкт-Петербургского университета",

number = "3",

}

RIS

TY - JOUR

T1 - Восточный (Китайский) сегмент Южного Тянь-Шаня: коллизионная структура и главные палеозойские события

AU - Biske, Y. S.

PY - 1998/12/1

Y1 - 1998/12/1

N2 - Structural design of Southern (Variscian) Tien Shan in the Eastern segment consists, south to north, of: 1) broken border of Tarim paleocontinent; 2) upper Paleozoic frontal basin; 3) volcanics and sediments of Turkestan ocean with ophiolites and some signs of nappe tectonics on initial stages of collision; 4) island arc unite (terraine) of Erben-Kumyshtala; 5) collisional suture on southern limit of Jili microcontinent, as a part of Paleokazakhstan. Collision of Erben-Kumyshtala with Paleokazakhstan border happened about Devonian/Carboniferous limit, but did not close Turkestan ocean. This event took place only at Late Carboniferous all along northern border of Tarim paleocontinent.

AB - Structural design of Southern (Variscian) Tien Shan in the Eastern segment consists, south to north, of: 1) broken border of Tarim paleocontinent; 2) upper Paleozoic frontal basin; 3) volcanics and sediments of Turkestan ocean with ophiolites and some signs of nappe tectonics on initial stages of collision; 4) island arc unite (terraine) of Erben-Kumyshtala; 5) collisional suture on southern limit of Jili microcontinent, as a part of Paleokazakhstan. Collision of Erben-Kumyshtala with Paleokazakhstan border happened about Devonian/Carboniferous limit, but did not close Turkestan ocean. This event took place only at Late Carboniferous all along northern border of Tarim paleocontinent.

UR - http://www.scopus.com/inward/record.url?scp=0032458650&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0032458650

VL - 7

SP - 3

EP - 13

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 2541-9668

IS - 3

ER -

ID: 49957171