The Kohistan Sequences: Crust and Mantle of an Obducted Island Arc
Abstract
The Kohistan sequence outcrops in the western part of the western Himalayan syntaxis. It is a thick pile (3040 km) of metamorphosed magmatic, volcanic and sedimentary rocks. It is composed of six main units i.e. from bottom to top:
- the southern amphibolitlc belt with basal ultramafics,
- the "pyroxene granulite" belt (10-15 km thick),
- the northern amphibolitic belt, intruded by various dioritic bodies,
- a metasedimentary oceanic series (Kalam series), - a volcanic calc-alkaline series (Utror Volcanics), up to 6-8 km thick,
- an upper detrital series (Yasin group, Lower Cretaceous).
This sequence is interpreted as a complete cross-section of a mature island arc formed by subduction during Mesozoic in the southern part of the Neotethys and obducted onto the Indian plate in Upper Cretaceous times.
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