نوع مقاله : علمی -پژوهشی

نویسندگان

• مریم معتمدالشریعتی ¹
• سید ناصر رئیس السادات ¹
• دکتر محمد وحیدی نیا ²
• معصومه موسی خوانی ¹

¹ گروه زمین‌شناسی، دانشکده علوم، دانشگاه بیرجند، بیرجند، ایران

² گروه زمین‌شناسی، دانشکده علوم، دانشگاه فردوسی مشهد، مشهد، ایران

چکیده

برش علی حاجی واقع در جنوب بیرجند با یک توالی کنگلومرایی که به صورت ناپیوستگی آذرین پی بر روی پریدوتیت های کرتاسه قرار گرفته آغاز می­شود. سپس سنگ آهک­های فسیل­دار با توالی از لایه­های مارنی و شیلی قرار می­گیرد. مطالعه و بررسی نمونه­های سخت و نرم، منجر به شناسایی 25 جنس و 39 گونه از مجموع روزن­داران کف­زی و پلانکتون گردید که 20 جنس و 30 گونه کف­زی و 5 جنس و 9 گونه روزن­داران پلانکتونیک می­باشد. با توجه به روزن­داران شناسایی شده 5 بایوزون معرفی و سن پالئوسن پسین- ائوسن پسین برای این توالی پیشنهاد شد. این برش قابل مقایسه با سایر برش­های اندازه­گیری شده در شمال بیرجند می­باشد. از سوی دیگر نهشته­ها با سن پالئوسن پسین بر روی مجموعه افیولیتی به فرم ناپیوسته قرار گرفته به نظر می­رسد بالا آمدن و جایگیری آنها در جنوب بیرجند قبل از پالئوسن پسین بوده است.

کلیدواژه‌ها

• بیرجند
• پالئوسن- ائوسن
• روزن‌داران
• زیست چینه‌نگاری

20.1001.1.20088299.1401.13.2.6.1

عنوان مقاله [English]

Biostratigraphy of Paleocene- Eocene deposits based on foraminifera in south of Birjand, Iran

نویسندگان [English]

• Maryam Motamedalshariati ¹
• Seyed Naser Raisossadat ¹
• Mohammad Vahidinia ²
• Masumeh Musakhani ¹

¹ Department of Geology, Faculty of Sciences, University of Birjand, Birjand, Iran

² Department of Geology, Faculty of Sciences, Ferdowsi University of Mashhad, Mashhad, Iran

چکیده [English]

The studied section is located in the eastern margin of Lut block, 38 kilometers south of Birjand (Iran) in the east of Ali Haji village. It is situated within the geological sheet map of Birjand (Ohanian and Tatevosian, 1978).The present study aimed to identify foraminifera assemblage in the measured section and present a biostratigraphic scheme. In addition, we evaluated the correlation of the studied section with other previously studied sections in the vicinity of Birjand.
Materials and Methods
This study was conducted on 10 rock samples and 29 soft shale and marl samples. The thin sections were photographed. After washing and separating the foraminifera from the sediments, imaging was performed using Scanning Electron Microscope (SEM).
Results and discussion
The section starts with a basal conglomerate, which is overly on the ophiolites (peridotite) unconformably. This conglomerate is composed of peridotite fragments, which are gradually converted into sandstone and calcareous sandstone. The succession continues with thick, cream-colored foraminifera limestone. The upper portion of the lower sequence and the middle segment mostly contain light-to-dark gray marl with thin layers of shale (colored gray-to-olive). The upper portion could be divided into two parts; the lower part contains most of the gray shale and sandstone with some trace fossils, and the upper parts mostly contain a grayish-green shale, which is formed between the layers of marl and gradually disappears, causing a reddish-brown shale to appear on top of the sequence. In addition, the biostratigraphic studies in Ali Haji section led to the identification of twenty genera and thirty species of benthic, as well as five genera and nine species of planktonic foraminifera. As a result, five biozones were introduced, including ; 1- Alveolina assemblage zone 2- Morozovella aragonensis interval zone 3- Turborotalia cf. possagnoensis taxon range zone4- Subbotina bolivariana taxon range zone 5- Uvigerina jacksonensis assemblage zone. Based on the introduced zones, the age of the studied section is suggested a late Paleocene to late Eocene. Furthermore, the comparison of the Ali Haji section in the south of Birjand showed correlations with the Ching Dar and Grong sections, the Dahan Rud section, and the Friznook section in the north of Birjand. The thickness of the detrital units at the base of the section during the Paleocene was observed to be more significant in the north of Birjand compared to the south, which could be attributed to the further subsidence of the basin due to the activity of synsedimentary faults, earlier transgression in the north, or higher altitudes in the south (paleo-high) in Paleocene.The limestone units in the southern part will be transformed into marl and marly limestone units. In the northern part, the thickness of limestone was considered significant in Ching Dar and Dahan Rud sections.In the Dahan Rud section, sandstone and conglomerate intercalations were thicker compared to the other sections. Although limestone and marl units were identified in the Friznook section, the detrital facies was thoroughly spread possibly due to flysch deposits with fossil trace diversity.
Conclusion
According to the results, the Ali Haji section in the south of Birjand with a thickness of 560 meters had conglomerates, limestone, nummulitic limestone, marly limestone, marl, shale, and sandy limestone. Due to the distribution and identification of foraminifera in the Ali Haji section, a late Paleocene to the late Eocene age is speculated. Given the disconformity boundary of ophiolites and Paleocene deposits, it could be concluded that the ophiolite placement occurred before the Late Paleocene.

کلیدواژه‌ها [English]

• Birjand
• Paleocene-Eocene
• Foraminifera
• Biostratigraphy