Source provenance
Robertson, A.H.F. & Collins, A.S. (2002). Shyok Suture Zone, N Pakistan: late Mesozoic-Tertiary evolution of a critical suture separating the oceanic Ladakh Arc from the Asian continental margin. Journal of Asian Earth Sciences, 20(3), 309-351.
Cited by 1 unit (1 published) · 0 field-level citations · 1 revision note.
Structural/stratigraphic anatomy of the Shyok Suture Zone (Skardu-Khaplu-Hushe-Thalle), separating the oceanic Ladakh Arc from the south-Asian (Karakoram) margin. Defines the Burje-La Formation, Askore Amphibolite, Pakora Formation (~7 km Early Cretaceous volcaniclastics), Saltoro Formation and the structurally highest Bauma-Harel Group (Ordovician + Carboniferous-Permian-Triassic carbonate/siliciclastic south-Asian-margin sediments). NOTE: the paper's 'Thalle' is the Thalle Valley (volcaniclastics correlated with the Pakora Formation), NOT the Ordovician Thalle Limestone of the dataset; and it does not treat the Plio-Pleistocene Bunthang Sequence.
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Units citing this source
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- Age: Robertson & Collins (2002), in their structural anatomy of the Shyok Suture Zone, describe the Bauma-Harel Group as the structurally highest unit — a several-km-thick succession of Ordovician and Carboniferous-to-Permian-Triassic low-grade mixed carbonate/siliciclastic rocks deposited on the south-Asian continental margin. This Palaeozoic-Triassic assignment diverges from the tentative Cretaceous-Eocene age recorded here (after GSP/Kazmi & Abbasi 2008); flagged as an unresolved divergence pending reconciliation, with the primary suture-zone study favouring a Palaeozoic-Triassic age.