The South Ladakh ophiolites (NW Himalaya, India): an intra-oceanic tholeiitic arc origin with implication for the closure of the Neo-Tethys

In the Ladakh–Zanskar area, two groups of ophiolites document closure of the Neo-Tethys Ocean during India–Asia convergence. They are localized north of the Indus Suture Zone and in South Ladakh, respectively. The South Ladakh group includes the Spontang ophiolite, with both crustal and mantle units...

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Veröffentlicht in:Chemical geology 2004-02, Vol.203 (3), p.273-303
Hauptverfasser: Mahéo, Gweltaz, Bertrand, Hervé, Guillot, Stéphane, Villa, Igor M., Keller, Francine, Capiez, Paul
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Sprache:eng
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