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جلد 32 شماره 1 صفحات 160-145 |
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Dehghani Dashtabi S, mahmoody S, Rahgoshay M. Physicochemical conditions of granitoids amphibole crystallization in Hararan (part of Lalehzar granitoid complex in Baft city, Kerman Province). www.ijcm.ir 2024; 32 (1) :145-160
URL: http://ijcm.ir/article-1-1845-fa.html
URL: http://ijcm.ir/article-1-1845-fa.html
دهقانی دشتابی سلیمه، محمودی شهریار، رهگشای محمد. شرایط فیزیکوشیمیایی تبلور کانی آمفیبول گرانیتوئید هراران (بخشی از توده گرانیتوئیدی لالهزار در شهرستان بافت استان کرمان). مجله بلورشناسی و کانی شناسی ایران. 1403; 32 (1) :145-160
1- گروه زمین‌شناسی، دانشکده علوم زمین، دانشگاه شهید بهشتی، تهران، ایران
2- گروه زمین‌شناسی، دانشکده علوم زمین، دانشگاه خوارزمی، تهران، ایران
2- گروه زمین‌شناسی، دانشکده علوم زمین، دانشگاه خوارزمی، تهران، ایران
چکیده: (177 مشاهده)
توده گرانیتوئیدی لالهزار از مهمترین فازهای ماگمایی کمربند ارومیه-دختر بوده و در جنوبشرق این کمربند در استان کرمان واقع است. بخشی از این توده گسترده در بخش جنوبی منطقه هراران رخنمون دارد که بر اساس بررسیهای سنگنگاری، این سنگهای آذرین از جنس گرانودیوریت و دیوریت و دارای کانیهای کوارتز، پلاژیوکلاز، آمفیبول، بیوتیت، پیروکسن و کانیهای کدر هستند. جایابی نمونههای آمفیبول این توده گرانیتوئیدی بر نمودارهای ردهبندی نشان میدهد که آمفیبولها کلسیمی و از نوع هورنبلند هستند. این آمفیبولها، آذرین و مربوط به سری ماگمایی آهکی قلیایی و از نوع آمفیبولهای فرورانش (S) هستند که در محیط فرورانش تشکیل شدهاند. محاسبه فشار و دمای تشکیل این آمفیبولها با روشهای مختلف نشان داد که این آمفیبولها در دمای 650 تا 798 درجه سانتیگراد و فشار 9/0 تا 3/2 کیلوبار تشکیل شدهاند. همچنین گریزندگی اکسیژن ماگما در زمان تشکیل آمفیبول بالا بوده و این کانی در اعماق 5 تا 7 کیلومتری زمین ایجاد شده است. بر اساس روابط بین برخی از عناصر اصلی این آمفیبولها، جانشینیهای چرماکیتی (جانشینی Al بهجای Si, Fe و Mg) و جانشینی ادنیتیک (جانشینی Si بهجای AlIV، Na یا K) در این آمفیبولها رخ داده اما جانشینی نوع گلوکوفان، ریبکیت و ریشتریت در آنها انجام نشده است.
واژه‌های کلیدی: هراران، جانشینی، گریزندگی اکسیژن.
فهرست منابع
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