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Pakistan Stratigraphy

Source provenance

Khan, M.H. (1968). The dating and correlation of the Nari and the Gaj Formations. Geological Bulletin of the Punjab University, 7, 57-65.

Peer-reviewed Full text read 1968

Cited by 3 units (3 published) · 0 field-level citations · 3 revision notes.

Larger-foraminiferal biozonation of the Upper Nari and Gaj formations near Karachi (Karachi Test Well No. 1, Pir Mangho). Two zones: a Spiroclypeus blanckenhorni ornata Zone (Aquitanian; Spiroclypeus spp., Eulepidina dilatata/formosa, Nephrolepidina, early Miogypsinoides) spanning the upper Upper Nari to basal Gaj, and an overlying Miogypsina globulina Zone (Late Aquitanian–Burdigalian) in the Gaj. Ages: Upper Nari = Rupelian–Early Aquitanian; Gaj = Late Aquitanian–Burdigalian. Also revises the Khirthar Formation as Lutetian–Rupelian (with a late-Auversian–Bartonian hiatus).

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