Provenance analysis of the Mesozoic Hoh-Xil-Songpan-Ganzi turbidites in northern Tibet: Implications for the tectonic evolution of the eastern Paleo-Tethys Ocean

L. Ding, D. Yang, F. L. Cai, A. Pullen, Paul A Kapp, George E Gehrels, L. Y. Zhang, Q. H. Zhang, Q. Z. Lai, Y. H. Yue, R. D. Shi

Research output: Contribution to journalArticle

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Abstract

[1] Mesozoic strata of the Hoh-Xil-Songpan-Ganzi complex in northern Tibet are exposed in a vast (> 370,000 km2) triangle-shaped orogenic belt bound by the Longmen Shan thrust belt in the east, the Kunlun terrane and North China block in the north, and the Qiangtang terrane and Yidun arc in the south. These strata consist of Middle-Upper Triassic submarine fan and deep marine facies rocks that were deposited in the Paleo-Tethys Ocean. Late Triassic-Early Jurassic contractional deformation in the eastern Hoh-Xil-Songpan- Ganzi complex marks the demise of the Paleo-Tethys Ocean basin and the accretion of the Gondwana-derived Qiangtang terrane to Eurasia. We conducted geological mapping, regional stratigraphic analyses, and U-Pb geochronology of detrital zircons (n = 4128) on the Mesozoic sequences exposed in the Hoh-Xil-Songpan-Ganzi complex, Kunlun terrane, and Qiangtang terrane. We identify for the first time marine silciclastic sandstone and shale of Jurassic age in the northwestern Hoh-Xil-Songpan-Ganzi complex that unconformably overlie Upper Triassic turbidites. Zircon age data indicate that the Middle-Upper Triassic marine gravity-flow deposits of the Hoh-Xil-Songpan-Ganzi complex were shed from the North and South China blocks, and Middle-Late Triassic ultrahigh-pressure Qinling- Dabie orogenic belt, as well as the Kunlun and Qiangtang terranes. In addition, the detrital zircon results suggest vast sediment source to sink distances (>1500 km) for the Middle- Upper Triassic Hoh-Xil-Songpan-Ganzi strata, which is consistent with tectonic models for the Paleo-Tethys Ocean basin that incorporate significant components of horizontal tectonic transport like opening of large back-arc basins in response to oceanic slab rollback.

Original languageEnglish (US)
Pages (from-to)34-48
Number of pages15
JournalTectonics
Volume32
Issue number1
DOIs
StatePublished - 2013

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Tethys
Tibet
strata
Tectonics
tectonic evolution
provenance
terrane
tectonics
oceans
Triassic
China
ocean
arcs
Geochronology
geochronology
zircon
sandstones
ocean basin
Shale
Sandstone

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

Provenance analysis of the Mesozoic Hoh-Xil-Songpan-Ganzi turbidites in northern Tibet : Implications for the tectonic evolution of the eastern Paleo-Tethys Ocean. / Ding, L.; Yang, D.; Cai, F. L.; Pullen, A.; Kapp, Paul A; Gehrels, George E; Zhang, L. Y.; Zhang, Q. H.; Lai, Q. Z.; Yue, Y. H.; Shi, R. D.

In: Tectonics, Vol. 32, No. 1, 2013, p. 34-48.

Research output: Contribution to journalArticle

Ding, L. ; Yang, D. ; Cai, F. L. ; Pullen, A. ; Kapp, Paul A ; Gehrels, George E ; Zhang, L. Y. ; Zhang, Q. H. ; Lai, Q. Z. ; Yue, Y. H. ; Shi, R. D. / Provenance analysis of the Mesozoic Hoh-Xil-Songpan-Ganzi turbidites in northern Tibet : Implications for the tectonic evolution of the eastern Paleo-Tethys Ocean. In: Tectonics. 2013 ; Vol. 32, No. 1. pp. 34-48.
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abstract = "[1] Mesozoic strata of the Hoh-Xil-Songpan-Ganzi complex in northern Tibet are exposed in a vast (> 370,000 km2) triangle-shaped orogenic belt bound by the Longmen Shan thrust belt in the east, the Kunlun terrane and North China block in the north, and the Qiangtang terrane and Yidun arc in the south. These strata consist of Middle-Upper Triassic submarine fan and deep marine facies rocks that were deposited in the Paleo-Tethys Ocean. Late Triassic-Early Jurassic contractional deformation in the eastern Hoh-Xil-Songpan- Ganzi complex marks the demise of the Paleo-Tethys Ocean basin and the accretion of the Gondwana-derived Qiangtang terrane to Eurasia. We conducted geological mapping, regional stratigraphic analyses, and U-Pb geochronology of detrital zircons (n = 4128) on the Mesozoic sequences exposed in the Hoh-Xil-Songpan-Ganzi complex, Kunlun terrane, and Qiangtang terrane. We identify for the first time marine silciclastic sandstone and shale of Jurassic age in the northwestern Hoh-Xil-Songpan-Ganzi complex that unconformably overlie Upper Triassic turbidites. Zircon age data indicate that the Middle-Upper Triassic marine gravity-flow deposits of the Hoh-Xil-Songpan-Ganzi complex were shed from the North and South China blocks, and Middle-Late Triassic ultrahigh-pressure Qinling- Dabie orogenic belt, as well as the Kunlun and Qiangtang terranes. In addition, the detrital zircon results suggest vast sediment source to sink distances (>1500 km) for the Middle- Upper Triassic Hoh-Xil-Songpan-Ganzi strata, which is consistent with tectonic models for the Paleo-Tethys Ocean basin that incorporate significant components of horizontal tectonic transport like opening of large back-arc basins in response to oceanic slab rollback.",
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T2 - Implications for the tectonic evolution of the eastern Paleo-Tethys Ocean

AU - Ding, L.

AU - Yang, D.

AU - Cai, F. L.

AU - Pullen, A.

AU - Kapp, Paul A

AU - Gehrels, George E

AU - Zhang, L. Y.

AU - Zhang, Q. H.

AU - Lai, Q. Z.

AU - Yue, Y. H.

AU - Shi, R. D.

PY - 2013

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N2 - [1] Mesozoic strata of the Hoh-Xil-Songpan-Ganzi complex in northern Tibet are exposed in a vast (> 370,000 km2) triangle-shaped orogenic belt bound by the Longmen Shan thrust belt in the east, the Kunlun terrane and North China block in the north, and the Qiangtang terrane and Yidun arc in the south. These strata consist of Middle-Upper Triassic submarine fan and deep marine facies rocks that were deposited in the Paleo-Tethys Ocean. Late Triassic-Early Jurassic contractional deformation in the eastern Hoh-Xil-Songpan- Ganzi complex marks the demise of the Paleo-Tethys Ocean basin and the accretion of the Gondwana-derived Qiangtang terrane to Eurasia. We conducted geological mapping, regional stratigraphic analyses, and U-Pb geochronology of detrital zircons (n = 4128) on the Mesozoic sequences exposed in the Hoh-Xil-Songpan-Ganzi complex, Kunlun terrane, and Qiangtang terrane. We identify for the first time marine silciclastic sandstone and shale of Jurassic age in the northwestern Hoh-Xil-Songpan-Ganzi complex that unconformably overlie Upper Triassic turbidites. Zircon age data indicate that the Middle-Upper Triassic marine gravity-flow deposits of the Hoh-Xil-Songpan-Ganzi complex were shed from the North and South China blocks, and Middle-Late Triassic ultrahigh-pressure Qinling- Dabie orogenic belt, as well as the Kunlun and Qiangtang terranes. In addition, the detrital zircon results suggest vast sediment source to sink distances (>1500 km) for the Middle- Upper Triassic Hoh-Xil-Songpan-Ganzi strata, which is consistent with tectonic models for the Paleo-Tethys Ocean basin that incorporate significant components of horizontal tectonic transport like opening of large back-arc basins in response to oceanic slab rollback.

AB - [1] Mesozoic strata of the Hoh-Xil-Songpan-Ganzi complex in northern Tibet are exposed in a vast (> 370,000 km2) triangle-shaped orogenic belt bound by the Longmen Shan thrust belt in the east, the Kunlun terrane and North China block in the north, and the Qiangtang terrane and Yidun arc in the south. These strata consist of Middle-Upper Triassic submarine fan and deep marine facies rocks that were deposited in the Paleo-Tethys Ocean. Late Triassic-Early Jurassic contractional deformation in the eastern Hoh-Xil-Songpan- Ganzi complex marks the demise of the Paleo-Tethys Ocean basin and the accretion of the Gondwana-derived Qiangtang terrane to Eurasia. We conducted geological mapping, regional stratigraphic analyses, and U-Pb geochronology of detrital zircons (n = 4128) on the Mesozoic sequences exposed in the Hoh-Xil-Songpan-Ganzi complex, Kunlun terrane, and Qiangtang terrane. We identify for the first time marine silciclastic sandstone and shale of Jurassic age in the northwestern Hoh-Xil-Songpan-Ganzi complex that unconformably overlie Upper Triassic turbidites. Zircon age data indicate that the Middle-Upper Triassic marine gravity-flow deposits of the Hoh-Xil-Songpan-Ganzi complex were shed from the North and South China blocks, and Middle-Late Triassic ultrahigh-pressure Qinling- Dabie orogenic belt, as well as the Kunlun and Qiangtang terranes. In addition, the detrital zircon results suggest vast sediment source to sink distances (>1500 km) for the Middle- Upper Triassic Hoh-Xil-Songpan-Ganzi strata, which is consistent with tectonic models for the Paleo-Tethys Ocean basin that incorporate significant components of horizontal tectonic transport like opening of large back-arc basins in response to oceanic slab rollback.

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