آمونیت های سازند کژدمی در کوه سیوند، برش شول، شمال شیراز در حوضه زاگرس، کاربرد دیرینه بوم شناسی
الموضوعات :ناصر رئیس السادات 1 , مهناز پروانه نژاد شیرازی 2
1 - دانشگاه بیرجند
2 - دانشگاه پیام نور
الکلمات المفتاحية: آمونیت, آلبین, سازند کژدمی, دیرینه بوم شناسی, حوضه زاگرس,
ملخص المقالة :
سازند کژدمی در حوضه زاگرس گسترش داشته و دارای دو رخساره کم عمق و عمیق می باشد. برش مورد مطالعه در
شمال شیراز در کوه سیوند در نزدیکی روستا شول قرار داد. برش مورد مطالعه با ضخامت 210 متر شامل سنگ آهک،
سنگ آهک مارنی و سنگ آهک های لایه نازک می باشد. چهار گونه Knemiceras persicum Collignon, 1981, Knemiceras aff. persicum Collignon, 1981, Knemiceras aff. iraniense Collignon, 1981, Knemiceras dubertreti Basse, 1940, مورد شناسایی قرار گرفتند و توصیف شدند.
بررسی آمونیت های سازند کژدمی نشان می دهد، گروههای شکلی متفاوت در این سازند پراکنده هستند.. به طوریکه در
غرب حوضه و فروافتادگی دزفول آمونیت های اسفروکونیک با تزئینات کم پراکندگی بیشتر دارد که نشانه دهنده عمق
بیشتر اس ت، در حالیکه در نواحی استان فارس و بوشهر آمونیت های با تزئینات بیشتر که نشانه دهنده عمق کمتر حوضه
است، گسترش دارند.در برش شول نیز مجموعه آمونیتی نیز عمق کم را پیشنهاد می کند که این امر با حضور فرامینیفرهای
بنتیک پشتیبانی می شود.
المصادر:
منابع
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ALAVI, M., 2004, Regional stratigraphi of Zagros fold-and-thrust belt of Iran and its proforeland evolution. American Journal of Science, 304, 1-20.
ARTHUR, M.A., JENKYNS, H.C., BRUMSACK, H.J., SCHLANGER, S.O., 1990, Stratigraphy, geochemistry and paleoceanography of organic carbon-rich Cretaceous sequences. In: Ginsburg, R.N., Beaudoin, B. (Eds), Cretaceous Resources, Events, and Rhythms. Kluwer, Dordrecht, 75-119.
ALY, M.F. and Abdel-Gawad G.I. 2001, Early Cretaceous ammonites of Gebel Lagama, North Sinai, Egypt. Palaeontographica, A262, 25-52.
ALY M.F., SMADI A. and ABU-AZZAM A. 2008, LateCenomanian-Early Turonian ammonites of
Jordan. Revue de Paléobiologie, Genève, 27, 43-71.
ASADI, A., MAJIDI FARD, M.R., VAZIRII, S. H. and YOUSEFI RAD H. M., 2016, Albian ammonites of the Kazhdumi Formation in the Nar section, east of Bushehr (Zagros zone). Scientific quarterly Journal of Geoscience, 25,199-212.
BASSE, É., 1937-1940, Les Céphalopodes crétacés des massifs côtiers syriens. Part 1-2. Notes et Mémoires sur le Moyen-Orient, Paris, 2, 165-200; 3, 411-473.
BATT, R. J., 1989, Ammonite Shell Morphotype Distributions in the Western Interior Greenhorn Sea and SomePaleoecological ImplicationsAuthor(s). PALAIOS, 4, 32-42.
BATT, R. J., 1991, Sutural amplitude of ammonite shells as paleoenvironment a1 indicator, Sutural amplitude of ammonite shells as a paleoenvironmental indicator. Lethaia, 24, 219-225.
BATT, R. J., 1993, Ammonite morphotypes as indicators of oxygenation in a Cretaceous epicontinental sea. Lethaia, 26, 49-63.
BAUDIN, F., 2005, A late Hauterivian short-lived anoxic event in the Mediterranean Tethys: the “Faraoni event”. Comptes Rendus Geosciences, 337, 1532-1540.
BÖHM, J. 1898, Ueber Ammonites Pedernalis v. Buch.-Zeitschrift der Deutschen Geologischen Gesellschaft, Hannover, Band 50, 183-201.
BORDENAVE, M.L., and BURWOOD, R., 1995, The Albian Kazhdumi Formation of the Dezful Embayment, Iran, one of the most efficient petroleum generating systems. In: Katz, B. (Ed.) Petroleum Source Rocks Series, CaseBook in Earth Sciences. Springer, Berlin, 183–207.
BORDENAVE, M.L., and HEGRE, J.A., 2005, The influence of tectonics on the entrapment of oil in the Dezful embayment, Zagros fold belt, Iran. Journal of Petroleum Geology, 28, 339–368.
BORDENAVE, M., HEGRE, J. 2010, Current Distribution of Oil and Gas Fields in the Zagros Fold Belt of Iran and Contiguous Offshore as the Result of the Petroleum Systems. Geological Society, London, Special Publications 291-353.
BUCH, L. von 1850, ber Ceratiten. Physikalische Mathematische Abhandlungen der Koeniglichen Akademie der Wissenschaften zu Berlin, v. 1 (1848), p. 1–33.
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