The Late Cretaceous Chagai arc outcrops in western Pakistan,southern Afghanistan and eastern Iran.It is in the Tethyan convergence zone,formed by northward subduction of the Arabian oceanic plate beneath the Afghan block.The oldest unit of the Chagai arc is the Late Cretaceous Sinjrani Volcanic Group.This is composed of porphyritic lava flows and volcaniclastic rocks,and subordinate shale,sandstone,limestone and chert.The flows are fractionated low-K tholeiitic basalts,basalticandesites,and andesites.Relative enrichment in their LILE and depletion in HFSE,and negative Nb and Ta and positive K,Ba and Sr anomalies point to a subduction-related origin.Compared to MORB,the least fractionated Chagai basalts have low Na_2O,Fe_2O_3~T,CaO,Ti,Zr,Y and ~(87)Sr/~(86)Sr.Rather than an Andean setting,these results suggest derivation from a highly depleted mantle in an intraoceanic arc formed by Late Cretaceous convergence in the Ceno-Tethys.The segmented subduction zone formed between Gondwana and a collage of small continental blocks(Iran,Afghan,Karakoram,Lhasa and Burma) was accompanied by a chain of oceanic island arcs and suprasubduction ophiolites including Semail,Zagros,Chagai-Raskoh,Kandahar,Muslim Bagh,Waziristan and Kohistan-Ladakh,Nidar,Nagaland and Manipur.These complexes accreted to the southern margin of Eurasia in the Late Cretaceous. The Late Cretaceous Chagai arc outcrops in western Pakistan, southern Afghanistan and eastern Iran. It is in the Tethyan convergence zone, formed by northward subduction of the Arabian oceanic plate beneath the Afghan block. Oldest means of the Chagai arc is the Late Cretaceous Sinjrani Volcanic Group. This is composed of porphyritic lava flows and volcaniclastic rocks, and subordinate shale, sandstone, limestone and chert.The flows are fractionated low-K tholeiitic basalts, basalticandesites, anddesites.Relative enrichment in their LILE and depletion in HFSE, and negative Nb and Ta and positive K, Ba and Sr anomalies point to a subduction-related origin. Compared to MORB, the least fractionated Chagai basalts have low Na 2 O, Fe 2 O 3 ~ T, CaO, Ti, Zr, Y and ~ 87 Sr / ~ (86) Sr. Rather than an Andean setting, these results suggest derivation from a highly depleted mantle in an intraoceanic arc formed by Late Cretaceous convergence in the Ceno-Tethys. The segmented subduction zone formed between Gondwana and a collage of small continental blocks (Iran, Afghan, Karakoram, Lhasa and Burma) was accompanied by a chain of oceanic island arcs and suprasubduction ophiolites including Semail, Zagros, Chagai-Raskoh, Kandahar, Muslim Bagh, Waziristan and Kohistan-Ladakh, Nidar , Nagaland and Manipur.These complexes accreted to the southern margin of Eurasia in the Late Cretaceous.