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    • Keywords


      India-Asia collision; 40Ar-39Ar thermochronology; deformation; trans-Himalaya

    • Abstract


      New40Ar-39Ar thermochronological results from the Ladakh region in the India-Asia collision zone provide a tectono-thermal evolutionary scenario. The characteristic granodiorite of the Ladakh batholith near Leh yielded a plateau age of 46.3 ± 0.6 Ma (2σ). Biotite from the same rock yielded a plateau age of 44.6 ± 0.3 Ma (2σ). The youngest phase of the Ladakh batholith, the leucogranite near Himya, yielded a cooling pattern with a plateau-like age of ∼ 36 Ma. The plateau age of muscovite from the same rock is 29.8 ±0.2 Ma (2σ). These ages indicate post-collision tectono-thermal activity, which may have been responsible for partial melting within the Ladakh batholith. Two basalt samples from Sumdo Nala have also recorded the post-collision tectono-thermal event, which lasted at least for 8 MY in the suture zone since the collision, whereas in the western part of the Indus Suture, pillow lava of Chiktan showed no effect of this event and yielded an age of emplacement of 128.2 ±2.6 Ma (2σ). The available data indicate that post-collision deformation led to the crustal thickening causing an increase in temperature, which may have caused partial melting at the base of the thickened crust. The high thermal regime propagated away from the suture with time.

    • Author Affiliations


      Rajneesh Bhutani1 Kanchan Pande2 T R Venkatesan3

      1. Department of Earth Sciences, Pondicherry University, Pondicherry - 605 014, India
      2. Department of Earth Sciences, Indian Institute of Technology, Powai, Mumbai - 400 076, India
      3. A2, Anand flats, 40, 2nd main road, Gandhinagar, Adyar, Chennai - 600 020, India
    • Dates

  • Journal of Earth System Science | News

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      Posted on July 25, 2019

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