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Micro faunal assemblages in the Ordovician – Silurian successions from the Pin Valley of Tethys Himalaya, India
  
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S. K. PARCHA Wadia institute of Himalayan Geology, General Mahadeo Singh Road, Dehra Dun, 248 001, India parchask@gmail.com; parchask@wihg.res.in. 
Shivani PANDEY Wadia institute of Himalayan Geology, General Mahadeo Singh Road, Dehra Dun, 248 001, India  
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摘要:
Micro faunal assemblages in the Ordovician – Silurian successions from the Pin Valley of Tethys Himalaya, India
      The Spiti basin together with the Zanskar basin forms the largest basin among the Tethyan Himalayan successions and forms one of the best-developed sec-tions in the Tethyan Tibetan belt. The basin is one of the classical areas, which depicts a continuous fos-siliferous Palaeozoic - Mesozoic successions. The present studies are focused on the Ordovician and Si-lurian successions of the Pin valley of the Spiti basin. Pin valley exposes richly fossiliferous lithological successions from Neoproterozoic to Cretaceous; therefore, it is an ideal section for the detail paleobi-ological and geological studies.
S. K. PARCHA,Shivani PANDEY.2009.Micro faunal assemblages in the Ordovician – Silurian successions from the Pin Valley of Tethys Himalaya, India[J].Acta Geoscientica Sinica,30(S1):49.
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