بازسازی شرایط محیط رسوبی سازند تاربور براساس تجزیه و تحلیل میکروفاسیس ها در ناحیه مورک (جنوب سمیرم)
الموضوعات :حسین قنبرلو 1 , امراله صفری 2 , حسین وزیری مقدم 3
1 - دانشگاه اصفهان
2 - دانشگاه اصفهان
3 - دانشگاهاصفهان
الکلمات المفتاحية: رودیست, سازند تاربور, میکروتافوفاسیس, میکروفاسیس, امواج طوفانی, ماستریشتین,
ملخص المقالة :
به منظور بازسازی شرایط محیط رسوبی رسوبات ماستریشتین میانی-بالایی (سازند تاربور) در ناحیه مورک (جنوب سمیرم) از مطالعات میکروفاسیس و میکروتافوفاسیس استفاده گردید. سازند تاربور در ناحیه مورک با ضخامت 239 متر از آهک و شیل تشکیل شده است. این سازند بر روی سازند گورپی و زیر رسوبات کنگلومرای پالئوسن قرار دارد. هفت میکروفاسیس براساس توزیع آلوکم های اصلی و ویژگی های رسوبی تشخیص داده شد. علاوه براین رسوبات سازند تاربور در یک پلت فرم کربناته از نوع رمپ هموکلینال تشکیل شده است. براساس نوع آلوکم های اصلی و ویژگی های تافونومیکی پنج میکروتافوفاسیس در ناحیه مورد مطالعه شناسایی و براساس تفسیر و توزیع عمودی میکروفاسیس ها و میکروتافوفاسیس ها بیشتر رسوبات در ناحیه مورد مطالعه در یک محیط تحت تاثیر امواج طوفانی ته نشین شده اند و به همین دلیل باعث عدم تشکیل تجمعات رودیستی و فراوانی جلبک های سبز دازی کلاداسه آ در ناحیه مورد مطالعه گردیده است. همچنین به علت ورود مواد آواری و افزایش مواد غذایی، قشرسازی بیشتر توسط بریوزئر ها صورت پذیرفته است.
المصادر:
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[1] آقانباتي، ع.، 1385، زمين شناسي ايران: سازمان زمين شناسي و اکتشافات معدني کشور، 586 ص.
[2] بختیاری، س.، 1392 ، اطلس راه های ایران: موسسه جغرافیایی و کارتوگرافی گیتاشناسی، 1:1000000
[3] صداقت، م. ا.، قریب، ف. و شاوردی، ط. ، 1377 ، نقشه زمین شناسی چهارگوش سمیرم: انتشارات سازمان زمین شناسی کشور، مقیاس 1:1000000.
[4] صفري، ا.، وزيري مقدم، ح. و لاسمي ی.، ۱۳۸۵، ميكروفاسيس ها و محيط رسوبي سازند تاربور در ناحيه خرامه (جنوب شرق شيراز)، دو فصلنامه مجله پژوهشي علوم پايه دانشگاه اصفهان، جلد، ۲۳، شماره ۱، ۱۲۳-۱۳۶.
[5] عزيزي، ر.، صفري، ا. و وزيري مقدم، ح.، 1394، ریزرخساره ها، محیط رسوبی و چینه نگاری سکانسی سازند تاربور در ناحیه سمیرم (جنوب غرب اصفهان)، دو فصلنامه رخساره های رسوبی مشهد، جلد 8، شماره 2، 198-215.
[6] مغفوري مقدم، ا.، ۱۳۸۴، ديرينه شناسي و محيط ديرينه سازند تاربور در اطراف خرم آباد،فصلنامه علوم زمين، جلد ۱۵، شماره ۵۸، ۳۸-۴۵.
[7] ABDEL-GAWAD, G.I., SABER, S.G., EL SHAZLY, S.H., and SALAMA, Y.F., 2011, Turonian rudist facies from Abu Roash area, north western desert, Egypt: Journal of African Earth Sciences, 59(4-5), 359–372.
[8] ACCORDI, G., CARBONE, F., and PIGNATTI, J.O., 1998, Depositional history of a Paleogene carbonate ramp (western Cephalonia, Ionian Islands, Greece): Geologica Romana, 34, 131–205.
[9] AFZAL, J., WILLIAMS, M., LENG, M.J., and ALDRIDGE, R. J., 2011, Dynamic response of the shallow marine benthic ecosystem to regional and pan-Tethyan environmental change at the Paleocene–Eocene boundary. Palaeogeography, Palaeoclimatology, Palaeoecology, 309, 141–160.
[10 AGHAEI, A., MAHBOUBI, A., MOUSSAVI-HARAMI, R., HEUBECK, C., and NADJAFI, M., 2013, Facies analysis and sequence stratigraphy of an Upper Jurassic carbonate ramp in the Eastern Alborz range and Binalud Mountains, NE Iran: Facies, 59(4), 863–889.
[11] ALAVI, M., 2007, Structures of the Zagros fold-thrust belt in Iran: American Journal of science, 307(9), 1064–1095.
[12] AL-HAJ, M.A., 2020, Sedimentological Study of the Hartha Formation in Selected Oilfields, Northern Iraq: Iranian Journal of Science and Technology Transaction A-Science, 44(2), 389–400.
[13] AMIRI BAKHTIAR, H., TAHERI, A., and VAZIRI-MOGHADDAM, H., 2011, Maastrichtian facies succession and sea-level history of the Hossein-Abad, Neyriz area, Zagros Basin: Historical Biology, 23(02-03), 145–153.
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