1 Ocak 2020 Dergi makalesi Açık Erişim

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

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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Rizwan, Muhammad</dc:creator>
  <dc:creator>Hanif, Muhammad</dc:creator>
  <dc:creator>Ali, Nowrad</dc:creator>
  <dc:creator>Rehman, Maqsood Ur</dc:creator>
  <dc:date>2020-01-01</dc:date>
  <dc: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.</dc:description>
  <dc:identifier>https://aperta.ulakbim.gov.trrecord/110202</dc:identifier>
  <dc:identifier>oai:zenodo.org:110202</dc:identifier>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights>
  <dc:source>CARBONATES AND EVAPORITES 35(4)</dc:source>
  <dc:title>Microfacies analysis and depositional environments of the Upper Cretaceous Fort Munro Formation in the Rakhi Nala Section, Sulaiman range, Pakistan</dc:title>
  <dc:type>info:eu-repo/semantics/article</dc:type>
  <dc:type>publication-article</dc:type>
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