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Browsing by Author Lepvrier, C.

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  • Tectonophysics Volume 393 issue 1-4 2004 [doi 10.1016%2Fj.tecto.2004.07.030] C. Lepvrier; H. Maluski; Vu Van Tich; A. Leyreloup; Phan Truong -- The Early Triassic Indosinian orogeny in Vietnam (Truong.pdf.jpg
  • Article

  • The Early Triassic Indosinian orogeny in Vietnam (Truong Son Belt and Kontum Massif); implications for the geodynamic evolution of Indochina

    • Authors: Lepvrier, C.; Maluski, H.; Vu, Van Tich; Leyreloup, A.; Phan, Truong Thi; Nguyen, Van Vuong (2004)

  • New structural field data at various scale and 40Ar–39Ar geochronological results, from the basement rocks in the Truong Son belt and Kontum Massif of Vietnam, confirm that ductile deformation and high-temperature metamorphism were caused by the Early Triassic event of the Indosinian Orogeny in the range of 250–240 Ma. A compilation of isotopic data obtained in other countries along the Sibumasu–Indochina boundary broadly indicates same interval of ages. This tectonothermal event is interpreted as the result of a synchronous oblique collision of Indochina with both Sibumasu and South China, inducing dextral and sinistral shearing along E–W to NW–SE and N–S fault zones, respectively. T...

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Browsing by Author Lepvrier, C.

Jump to: 0-9 A B C D E F G H I J K L M N O P Q R S T U V W X Y Z
or enter first few letters:  
Showing results 1 to 1 of 1
  • Tectonophysics Volume 393 issue 1-4 2004 [doi 10.1016%2Fj.tecto.2004.07.030] C. Lepvrier; H. Maluski; Vu Van Tich; A. Leyreloup; Phan Truong -- The Early Triassic Indosinian orogeny in Vietnam (Truong.pdf.jpg
  • Article

  • The Early Triassic Indosinian orogeny in Vietnam (Truong Son Belt and Kontum Massif); implications for the geodynamic evolution of Indochina

    • Authors: Lepvrier, C.; Maluski, H.; Vu, Van Tich; Leyreloup, A.; Phan, Truong Thi; Nguyen, Van Vuong (2004)

  • New structural field data at various scale and 40Ar–39Ar geochronological results, from the basement rocks in the Truong Son belt and Kontum Massif of Vietnam, confirm that ductile deformation and high-temperature metamorphism were caused by the Early Triassic event of the Indosinian Orogeny in the range of 250–240 Ma. A compilation of isotopic data obtained in other countries along the Sibumasu–Indochina boundary broadly indicates same interval of ages. This tectonothermal event is interpreted as the result of a synchronous oblique collision of Indochina with both Sibumasu and South China, inducing dextral and sinistral shearing along E–W to NW–SE and N–S fault zones, respectively. T...