نمایش مختصر رکورد

dc.contributor.authorzarei, elaheen_US
dc.date.accessioned1399-07-09T09:50:30Zfa_IR
dc.date.accessioned2020-09-30T09:50:30Z
dc.date.available1399-07-09T09:50:30Zfa_IR
dc.date.available2020-09-30T09:50:30Z
dc.date.issued2017-01-01en_US
dc.date.issued1395-10-12fa_IR
dc.date.submitted2017-01-04en_US
dc.date.submitted1395-10-15fa_IR
dc.identifier.citationzarei, elahe. (2017). Palynofacies analysis and paleoenvironmental interpretation of the Dalichai Formation, northeast of Semnan. Geopersia, 7(1), 27-34. doi: 10.22059/geope.2017.224223.648291en_US
dc.identifier.issn2228-7817
dc.identifier.issn2228-7825
dc.identifier.urihttps://dx.doi.org/10.22059/geope.2017.224223.648291
dc.identifier.urihttps://geopersia.ut.ac.ir/article_61096.html
dc.identifier.urihttps://iranjournals.nlai.ir/handle/123456789/369735
dc.description.abstractPalynological and Palynofacies analysis combined with sedimentological studies have been performed on Dalichai Formation, northeast of Semnan, in order to define its paleoenviromental interpretation. Based on petrographic studies of organic matter, three palynofacies types were recognized as PF-1, PF-2, and PF-3. PF-1 is a characteristic of proximal shelf settings or basin. This palynofacies in the lower part of Dalichai Formation represents the shallowest environment because it is comprised almost exclusively of large black phytoclast while PF-1 in limestone successions in the upper part of Dalichai Formation was deposited in distal setting under suboxic environment. This interpretation is supported by sedimentological and paleontological data. PF-2 represents the lower and middle parts of the formation with high contents of brown wood and sporomorphs. In addition, it shows the presence of fluorescent amorphous organic matter and proximate dinocysts deposited in the open marine lagoon (the anoxic-suboxic environment) in agreement with general sedimentological observations. PF-3 has a high diversity of dinocysts, combined with the terrestrial material. A diverse dinocyst assemblage is common in shelf environments, leading us to interpret a possible inner to middle shelf close enough to land to allow accumulation of terrestrially derived organic material.en_US
dc.format.extent613
dc.format.mimetypeapplication/pdf
dc.languageEnglish
dc.language.isoen_US
dc.publisherTehran, University of Tehran Pressen_US
dc.relation.ispartofGeopersiaen_US
dc.relation.ispartofGeopersiafa_IR
dc.relation.isversionofhttps://dx.doi.org/10.22059/geope.2017.224223.648291
dc.subjectPalynofaciesen_US
dc.subjectDepositional environmenten_US
dc.subjectDalichai Formationen_US
dc.subjectCentral Alborzen_US
dc.titlePalynofacies analysis and paleoenvironmental interpretation of the Dalichai Formation, northeast of Semnanen_US
dc.typeTexten_US
dc.typeResearch Paperen_US
dc.contributor.department*Assistant Professor, Department of Geology, Faculty of Geology, Damghan University,en_US
dc.citation.volume7
dc.citation.issue1
dc.citation.spage27
dc.citation.epage34


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