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- W2386485344 abstract "During last three decades, the Wargal and Chhidru Formations in the Salt Range, Pakistan and their equivalents in the Himalayan region have been considered by many authors to be Middle Permian (Guadalupian) in age. Based on the correlation of the Guadalupian and Lopingian conodont zones of the Salt Range, Pakistan with those of South China, the Amb Formation and the lower part of the Wargal Formation in the Salt Range, Pakistan are Late Guadalupian in age. The Guadalupian/Lopingian boundary is in the lower part of the Wargal Formation, and the Wuchiapingian/Changhsingian boundary is in the lower part of the Chhidru Formation. The Permian/Triassic boundary is in the Kathwai Member of the Mianwali Formation. Thus, it can be inferred that the Selong Group in the southern Tibet is also Lopingian in age in view of its correlatable brachiopod faunas with those of the Kalabagh Member of the upper Wargal Formation and the Chhidru Formation and the conodont zones around the Permian/Triassic boundary in southern Tibet." @default.
- W2386485344 created "2016-06-24" @default.
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- W2386485344 date "2003-01-01" @default.
- W2386485344 modified "2023-10-03" @default.
- W2386485344 title "LATEST BIOSTRATIGRAPHICAL ADVANCES OF THE PERMIAN SYSTEM IN THE SALT RANGE, PAKISTAN" @default.
- W2386485344 hasPublicationYear "2003" @default.
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