1 Ocak 2020 Dergi makalesi Açık Erişim

Rizwan, Muhammad; Hanif, Muhammad; Ali, Nowrad; Rehman, Maqsood Ur

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    "creators": [
      {
        "affiliation": "Univ Peshawar, Natl Ctr Excellence Geol, Peshawar, Pakistan", 
        "name": "Rizwan, Muhammad"
      }, 
      {
        "affiliation": "Univ Peshawar, Natl Ctr Excellence Geol, Peshawar, Pakistan", 
        "name": "Hanif, Muhammad"
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      {
        "name": "Ali, Nowrad"
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      {
        "name": "Rehman, Maqsood Ur"
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    "description": "The Fort Munro Formation is 200-m-thick mixed carbonate-siliciclastic succession of Late Cretaceous (Campanian) age exposed at the Rakhi Nala Section, Sulaiman Range, Lower Indus Basin, Pakistan. The Fort Munro Formation is representing thin- to thick-bedded limestone with interbedded marls, shale and sandstone. Detailed microfacies analysis revealed the recognition of 15 microfacies types (11 carbonate and 4 sandstone). These facies were deposited on both inner and middle ramp platform. The inner ramp sediments are more widespread than the corresponding middle ramp including open-marine, skeletal shoals, semi-restricted, carbonate sand shoals and banks and lagoon depositional environments. The uppermost part of the Fort Munro Formation has received sufficient amount of siliciclasts, thereby producing a sandstone texture. These siliciclasts indicate the tectonic uplift, which thereby increases the source area rejuvenation. Therefore, a mixed carbonate-siliciclastic, moderately storm-dominated homoclinal ramp depositional environment is suggested for the Fort Munro Formation.", 
    "doi": "10.1007/s13146-020-00639-9", 
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    "journal": {
      "issue": "4", 
      "title": "CARBONATES AND EVAPORITES", 
      "volume": "35"
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    "publication_date": "2020-01-01", 
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      "title": "Dergi makalesi", 
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    "title": "Microfacies analysis and depositional environments of the Upper Cretaceous Fort Munro Formation in the Rakhi Nala Section, Sulaiman range, Pakistan"
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