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    • Volume 7, Issue 1
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    •   صفحهٔ اصلی
    • نشریات انگلیسی
    • Geopersia
    • Volume 7, Issue 1
    • مشاهده مورد
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    Palynofacies analysis and paleoenvironmental interpretation of the Dalichai Formation, northeast of Semnan

    (ندگان)پدیدآور
    zarei, elahe
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    اندازه فایل: 
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    نوع مدرک
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    Research Paper
    زبان مدرک
    English
    نمایش کامل رکورد
    چکیده
    Palynological 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.
    کلید واژگان
    Palynofacies
    Depositional environment
    Dalichai Formation
    Central Alborz

    شماره نشریه
    1
    تاریخ نشر
    2017-01-01
    1395-10-12
    ناشر
    Tehran, University of Tehran Press
    سازمان پدید آورنده
    *Assistant Professor, Department of Geology, Faculty of Geology, Damghan University,

    شاپا
    2228-7817
    2228-7825
    URI
    https://dx.doi.org/10.22059/geope.2017.224223.648291
    https://geopersia.ut.ac.ir/article_61096.html
    https://iranjournals.nlai.ir/handle/123456789/369735

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