ریزرخساره ها، محیط رسوبی و چینه نگاری سکانسی سازند قم در ناحیه مرق (جنوب غرب کاشان)
الموضوعات :
امراله صفری
1
(استادیار دانشگاه اصفهان )
حسین قنبرلو
2
(دانشگاه اصفهان)
ابراهیم محمدی
3
(دانشگاه تحصيلات تکميلي صنعتي و فناوري پيشرفته، کرمان)
الکلمات المفتاحية: سازند قم, ریز رخساره, سکانس های رسوبی, ناحیه مرق,
ملخص المقالة :
سازند قم در ناحیه مرق و در 20 کیلومتری جنوب غرب کاشان با ضخامت 216 متر از سنگ آهک و شیل تشکیل شده است که به صورت ناپیوسته بر روی سنگ آتشفشانی ائوسن و به طور ناپیوسته در زیر سازند قرمز بالایی قرار دارد. براساس آلوکم های اصلی و ویژگی های رسوبی نه ریز رخساره کربناته و یک رخساره آواری شناسایی گردید. این ریز رخساره ها ی کربناته و رخساره آوری در پلت فرمی از نوع شلف باز رسوب گذاری کرده اند. این پلت فرم را می توان به سه محیط شلف داخلی (لاگون محصور و نیمه محصور)، شلف میانی و شلف خارجی تقسیم کرد. براساس توزیع عمودی ریز رخساره ها سه سکانس رسوبی کامل درجه 3 و یک سکانس ناقص رسوبی تشخیص داده شد.
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