Panjal Traps
The Panjal Traps or the Tethyan Plume is a large igneous province (LIP) that erupted during the Early–Middle Permian in what is now north-western India. The Panjal Traps are associated with the opening of the Neo-Tethys Ocean, which resulted in the dispersal of the Cimmerian continental blocks from the north-eastern margin of Gondwana and possibly the break-up of this old and large continent.In the Zanskar-Spliti-Lahaul area (in the north-western Himalayas and south-east Ladakh) the 30–150 m (98–492 ft)-thick basalts of the Panjal Traps are mostly exposed as massive (terrestrial) lava flows, but also as (marine) pillow lavas and hyaloclastites.
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Panjal Traps
The Panjal Traps or the Tethyan Plume is a large igneous province (LIP) that erupted during the Early–Middle Permian in what is now north-western India. The Panjal Traps are associated with the opening of the Neo-Tethys Ocean, which resulted in the dispersal of the Cimmerian continental blocks from the north-eastern margin of Gondwana and possibly the break-up of this old and large continent.In the Zanskar-Spliti-Lahaul area (in the north-western Himalayas and south-east Ladakh) the 30–150 m (98–492 ft)-thick basalts of the Panjal Traps are mostly exposed as massive (terrestrial) lava flows, but also as (marine) pillow lavas and hyaloclastites.
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The Panjal Traps or the Tethya ...... perly dated to 289 Ma in 2011.
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The Panjal Traps or the Tethya ...... llow lavas and hyaloclastites.
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Panjal Traps
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