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Rizwan, Muhammad; Hanif, Muhammad; Ali, Nowrad; Rehman, Maqsood Ur
<?xml version='1.0' encoding='utf-8'?> <resource xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://datacite.org/schema/kernel-4" xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4.1/metadata.xsd"> <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> </resource>
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