Source provenance
Gardezi, A.H. (1968). Note on the geology of area around Nathiagali, District Hazara, West Pakistan. Geological Bulletin of the Punjab University, 7, 71-78.
Peer-reviewed Full text read 1968
Cited by 1 unit (1 published) · 0 field-level citations · 1 revision note.
Field note on the Hazara Slate Formation around Nathiagali: flysch-type geosynclinal turbidites (argillites, silty shales, siltstones, subgreywackes) >10,000 ft thick with a thick psammite forming Miranjani Peak; describes the Langrial and Miranjani algal (oncolitic/stromatolitic) limestone bands within the slates, overlain with apparent paraconformity by the Toarcian Maira Formation (Bouleiceras cf. nitescens). SE-directed imbricate thrusting within the syntaxial loop.
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Units citing this source
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- Lithology: Around Nathiagali the Hazara Slate Formation is flysch-type geosynclinal turbidite (argillites, silty shales, siltstones and subgreywackes) exceeding 10,000 ft, with graded bedding, flute casts and slump structures and a thick psammite (>500 ft) forming Miranjani Peak; it contains the Langrial and Miranjani algal (oncolitic/stromatolitic) limestone bands and is overlain with apparent paraconformity by the Toarcian Maira Formation (Bouleiceras cf. nitescens) (Gardezi, 1968).