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

In: Terra Nova, Vol. 30, No. 2, 01.04.2018, p. 95-104.

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

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, vol. 30, no. 2, pp. 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 et al. Thermochronological insights into the structural contact between the Tian Shan and Pamirs, Tajikistan. Terra Nova. 2018 Apr 1;30(2):95-104. doi: 10.1111/ter.12313

Author

Jepson, Gilby ; Glorie, Stijn ; Konopelko, Dmitry et al. / Thermochronological insights into the structural contact between the Tian Shan and Pamirs, Tajikistan. In: Terra Nova. 2018 ; Vol. 30, No. 2. pp. 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