نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشجوی دکترا، بخش زمین شناسی، دانشکده علوم، دانشگاه هرمزگان، بندرعباس، ایران

2 گروه زمین شناسی، دانشکده علوم، دانشگاه هرمزگان، بندرعباس، ایران

3 گروه زمین شناسی ، دانشگاه شهید باهنر، کرمان ، ایران

4 گروه زمین شناسی - دانشکده علوم پایه - دانشگاه هرمزگان - بندرعباس

چکیده

باتولیت الیگوسن ساردوییه، با روند شمال ­باختر- جنوب­ خاور، در استان کرمان و در بخش جنوب خاوری کمان ماگمایی ارومیه- ­دختر قرار دارد و به درون واحدهای آتشفشانی ائوسن متشکل از آندزیت، آندزیت- بازالت و مقدار کمی بازالت همراه با آذرآواری­ها تزریق شده است. این باتولیت از سنگ­های اسیدی و حدواسط مانند دیوریت، تونالیت، گرانودیوریت و مونزوگرانیت تشکیل شده است. بررسی­های شیمی دو کانی پلاژیوکلاز و آمفیبول نشان می­دهد که ترکیب پلاژیوکلازها با An 24-43از الیگوکلاز تا آندزین متغیر بوده و آمفیبول با ترکیب مگنزیوهورنبلند از نوع کلسیک است. مطالعات صحرایی، سنگ‎شناسی و ژئوشیمیایی نشان می­دهند که ماگمای سازنده این توده از نوع I، متاآلومین تا کمی پرآلومین است و در سری کالک­آلکالن جای می‏گیرد. در الگوی عنکبوتی نرمالیز شده به گوشته اولیه، نمونه‎های مورد مطالعه غنی‎شدگی از عناصر با شعاع یونی بزرگ (LILE) مانند U، K، Pb، Sr و تهی‎شدگی از عناصر با قدرت یونی زیاد (HFSE) مانند Nb، Ta، Ti دارند که از ویژگی شاخص ماگماهای موقعیت زمین­ساختی کمان آتشفشانی در حاشیه فعال قاره­ای است. بر اساس مطالعات ژئوشیمیایی باتولیت ساردوییه به نظر می­رسد که در اثر ذوب بخشی سنگ­های متابازیک پوسته زیرین ایجاد شده‎اند.

کلیدواژه‌ها

موضوعات

کتابنگاری
صدیقیان، س.، درگاهی، س.، آروین، م.، 1395- سنگ­نگاری، منشأ و تحولات ماگمایی کمپلکس نفوذی خونرنگ، شمال باختر جیرفت، استان کرمان، فصل نامه علوم زمین، شماره 102، صص. 207 تا 220.
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