| Micro faunal assemblages in the Ordovician – Silurian successions from the Pin Valley of Tethys Himalaya, India |
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| 引用本文：S. K. PARCHA,Shivani PANDEY.2009.Micro faunal assemblages in the Ordovician – Silurian successions from the Pin Valley of Tethys Himalaya, India[J].地球学报,30(S1):49. |
| DOI：10.3975/cagsb.2009.s1.26 |
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| 中文摘要: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. |
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| Micro faunal assemblages in the Ordovician – Silurian successions from the Pin Valley of Tethys Himalaya, India |
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| Abstract: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. |
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