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Thermochronological insights into the structural contact between the Tian Shan and Pamirs, Tajikistan. / Jepson, Gilby; Glorie, Stijn; Konopelko, Dmitry и др.

в: Terra Nova, Том 30, № 2, 01.04.2018, стр. 95-104.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Jepson, G, Glorie, S, Konopelko, D, Gillespie, J, Danišík, M, Evans, NJ, Mamadjanov, Y & Collins, AS 2018, 'Thermochronological insights into the structural contact between the Tian Shan and Pamirs, Tajikistan', Terra Nova, Том. 30, № 2, стр. 95-104. https://doi.org/10.1111/ter.12313

APA

Jepson, G., Glorie, S., Konopelko, D., Gillespie, J., Danišík, M., Evans, N. J., Mamadjanov, Y., & Collins, A. S. (2018). Thermochronological insights into the structural contact between the Tian Shan and Pamirs, Tajikistan. Terra Nova, 30(2), 95-104. https://doi.org/10.1111/ter.12313

Vancouver

Jepson G, Glorie S, Konopelko D, Gillespie J, Danišík M, Evans NJ и др. Thermochronological insights into the structural contact between the Tian Shan and Pamirs, Tajikistan. Terra Nova. 2018 апр. 1;30(2):95-104. doi: 10.1111/ter.12313

Author

Jepson, Gilby ; Glorie, Stijn ; Konopelko, Dmitry и др. / Thermochronological insights into the structural contact between the Tian Shan and Pamirs, Tajikistan. в: Terra Nova. 2018 ; Том 30, № 2. стр. 95-104.

BibTeX

@article{6e4009f632b54d8eac735676e605f10b,
title = "Thermochronological insights into the structural contact between the Tian Shan and Pamirs, Tajikistan",
abstract = "Multi-method thermochronology along the Vakhsh-Surkhob fault zone reveals the thermotectonic history of the South Tian Shan–Pamirs boundary. Apatite U/Pb analyses yield a consistent age of 251 ± 2 Ma, corresponding to cooling below ~550–350°C, related to the final closure of the Palaeo-Asian Ocean and contemporaneous magmatism in the South Tian Shan. Zircon (U–Th–Sm)/He ages constrain cooling below ~180°C to the end of the Triassic (~200 Ma), likely related either to deformation induced by the Qiangtang collision or to the closure of the Rushan Ocean. Apatite fission track thermochronology reveals two low-temperature (<120°C) thermal events at ~25 Ma and ~10 Ma, which may be correlated with tectonic activity at the distant southern Eurasian margin. The late Miocene cooling is confirmed by apatite (U–Th–Sm)/He data and marks the onset of mountain building within the South Tian Shan that is ongoing today.",
keywords = "FISSION-TRACK THERMOCHRONOLOGY, SOUTHERN TIEN-SHAN, (U-TH)/HE THERMOCHRONOMETRY, CENOZOIC DEFORMATION, TECTONIC EVOLUTION, EXHUMATION HISTORY, CENTRAL-ASIA, APATITE, ZIRCON, AGE",
author = "Gilby Jepson and Stijn Glorie and Dmitry Konopelko and Jack Gillespie and Martin Dani{\v s}{\'i}k and Evans, {Noreen J.} and Yunus Mamadjanov and Collins, {Alan S.}",
note = "Publisher Copyright: {\textcopyright} 2017 John Wiley & Sons Ltd",
year = "2018",
month = apr,
day = "1",
doi = "10.1111/ter.12313",
language = "English",
volume = "30",
pages = "95--104",
journal = "Terra Nova",
issn = "0954-4879",
publisher = "Wiley-Blackwell",
number = "2",

}

RIS

TY - JOUR

T1 - Thermochronological insights into the structural contact between the Tian Shan and Pamirs, Tajikistan

AU - Jepson, Gilby

AU - Glorie, Stijn

AU - Konopelko, Dmitry

AU - Gillespie, Jack

AU - Danišík, Martin

AU - Evans, Noreen J.

AU - Mamadjanov, Yunus

AU - Collins, Alan S.

N1 - Publisher Copyright: © 2017 John Wiley & Sons Ltd

PY - 2018/4/1

Y1 - 2018/4/1

N2 - Multi-method thermochronology along the Vakhsh-Surkhob fault zone reveals the thermotectonic history of the South Tian Shan–Pamirs boundary. Apatite U/Pb analyses yield a consistent age of 251 ± 2 Ma, corresponding to cooling below ~550–350°C, related to the final closure of the Palaeo-Asian Ocean and contemporaneous magmatism in the South Tian Shan. Zircon (U–Th–Sm)/He ages constrain cooling below ~180°C to the end of the Triassic (~200 Ma), likely related either to deformation induced by the Qiangtang collision or to the closure of the Rushan Ocean. Apatite fission track thermochronology reveals two low-temperature (<120°C) thermal events at ~25 Ma and ~10 Ma, which may be correlated with tectonic activity at the distant southern Eurasian margin. The late Miocene cooling is confirmed by apatite (U–Th–Sm)/He data and marks the onset of mountain building within the South Tian Shan that is ongoing today.

AB - Multi-method thermochronology along the Vakhsh-Surkhob fault zone reveals the thermotectonic history of the South Tian Shan–Pamirs boundary. Apatite U/Pb analyses yield a consistent age of 251 ± 2 Ma, corresponding to cooling below ~550–350°C, related to the final closure of the Palaeo-Asian Ocean and contemporaneous magmatism in the South Tian Shan. Zircon (U–Th–Sm)/He ages constrain cooling below ~180°C to the end of the Triassic (~200 Ma), likely related either to deformation induced by the Qiangtang collision or to the closure of the Rushan Ocean. Apatite fission track thermochronology reveals two low-temperature (<120°C) thermal events at ~25 Ma and ~10 Ma, which may be correlated with tectonic activity at the distant southern Eurasian margin. The late Miocene cooling is confirmed by apatite (U–Th–Sm)/He data and marks the onset of mountain building within the South Tian Shan that is ongoing today.

KW - FISSION-TRACK THERMOCHRONOLOGY

KW - SOUTHERN TIEN-SHAN

KW - (U-TH)/HE THERMOCHRONOMETRY

KW - CENOZOIC DEFORMATION

KW - TECTONIC EVOLUTION

KW - EXHUMATION HISTORY

KW - CENTRAL-ASIA

KW - APATITE

KW - ZIRCON

KW - AGE

UR - http://www.scopus.com/inward/record.url?scp=85043373696&partnerID=8YFLogxK

U2 - 10.1111/ter.12313

DO - 10.1111/ter.12313

M3 - Article

AN - SCOPUS:85043373696

VL - 30

SP - 95

EP - 104

JO - Terra Nova

JF - Terra Nova

SN - 0954-4879

IS - 2

ER -

ID: 12079089