دوره 32، شماره 1 - ( 1-1403 )                   جلد 32 شماره 1 صفحات 160-145 | برگشت به فهرست نسخه ها


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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
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

URL: http://ijcm.ir/article-1-1845-fa.html


1- گروه زمین‌شناسی، دانشکده علوم زمین، دانشگاه شهید بهشتی، تهران، ایران
2- گروه زمین‌شناسی، دانشکده علوم زمین، دانشگاه خوارزمی، تهران، ایران
چکیده:   (230 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.     
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نوع مقاله: پژوهشي | موضوع مقاله: تخصصي

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