1 Ocak 2020 Dergi makalesi Açık Erişim

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

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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/110202</identifier>
  <creators>
    <creator>
      <creatorName>Rizwan, Muhammad</creatorName>
      <givenName>Muhammad</givenName>
      <familyName>Rizwan</familyName>
      <affiliation>Univ Peshawar, Natl Ctr Excellence Geol, Peshawar, Pakistan</affiliation>
    </creator>
    <creator>
      <creatorName>Hanif, Muhammad</creatorName>
      <givenName>Muhammad</givenName>
      <familyName>Hanif</familyName>
      <affiliation>Univ Peshawar, Natl Ctr Excellence Geol, Peshawar, Pakistan</affiliation>
    </creator>
    <creator>
      <creatorName>Ali, Nowrad</creatorName>
      <givenName>Nowrad</givenName>
      <familyName>Ali</familyName>
    </creator>
    <creator>
      <creatorName>Rehman, Maqsood Ur</creatorName>
      <givenName>Maqsood Ur</givenName>
      <familyName>Rehman</familyName>
    </creator>
  </creators>
  <titles>
    <title>Microfacies Analysis And Depositional Environments Of The Upper Cretaceous Fort Munro Formation In The Rakhi Nala Section, Sulaiman Range, Pakistan</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2020</publicationYear>
  <dates>
    <date dateType="Issued">2020-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/110202</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1007/s13146-020-00639-9</relatedIdentifier>
  </relatedIdentifiers>
  <rightsList>
    <rights rightsURI="http://www.opendefinition.org/licenses/cc-by">Creative Commons Attribution</rights>
    <rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
  </rightsList>
  <descriptions>
    <description descriptionType="Abstract">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.</description>
  </descriptions>
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