محیط رسوبی و برخاستگاه ماسه سنگهای سازند شوریجه (نئوکومین) در برش آبگرم، شرق حوضه کپه داغ

رخساره‌های رسوبی

مقاله 4، دوره 7، شماره 1، شهریور 1393، صفحه 125-149   

نوع مقاله: مقالات پژوهشی

شناسه دیجیتال (DOI): 10.22067/sed.facies.v7i1.25699

نویسندگان

محمد خانه باد^* ؛ طیبه گل افشانی؛ سید رضا موسوی حرمی؛ اسداله محبوبی

دانشگاه فردوسی مشهد

چکیده

در این مطالعه به بررسی محیط رسوبی و برخاستگاه ماسه سنگهای سازند شوریجه به سن کرتاسه پیشین در برش آبگرم واقع در حوضه رسوبی کپه داغ پرداخته شده است. تجزیه و تحلیل رخساره های رسوبی در این برش حاکی از وجود دو مجموعه رخساره ای آواری شامل رخساره های قاره ای و دشت ساحلی و نیز دو رخساره کربناته مرتبط با دشت ساحلی است. نتایج حاصل از تجزیه مدال و داده های ژئوشیمیایی به برخاستگاه زمین ساختی کوه زایی چرخه مجدد و سنگ مادر رسوبی کوارتزی (حاصل از چرخه مجدد رسوبی) اشاره دارد. همچنین استفاده از نمودارهای تفکیکی، جایگاه زمین ساختی حاشیه غیرفعال قاره ای را برای ماسه سنگهای سازند شوریجه نشان می دهد. شاخص شیمیایی دگرسانی آلتراسیون (CIA) محاسبه شده، میزان هوازدگی در منطقه منشأ را متوسط تا بالا معرفی می کند. این امر با نتایج پتروگرافی ماسه سنگها و رخساره ای مبنی بر وجود شرایط آب و هوای نیمه مرطوب تا نیمه خشک همخوانی دارد.

کلیدواژه‌ها

برخاستگاه؛ ژئوشیمی؛ سازند شوریجه؛ کپه داغ؛ محیط رسوبی

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