دوره 26، شماره 4 - ( 10-1397 )                   جلد 26 شماره 4 صفحات 975-988 | برگشت به فهرست نسخه ها


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Ahmadi S, Tahmasbi Z, Ahmadi Khalaji A, Zal F. Mineral chemistry of tourmaline in Lale Zar granite mass (kerman province) . www.ijcm.ir. 2019; 26 (4) :975-988
URL: http://ijcm.ir/article-1-1204-fa.html
احمدی صدف، طهماسبی زهرا، احمدی خلجی احمد، زال فرهاد. بررسی شیمی کانی تورمالین در توده گرانیتی لاله‌زار (استان کرمان). مجله بلورشناسی و کانی شناسی ایران. 1397; 26 (4) :975-988

URL: http://ijcm.ir/article-1-1204-fa.html


دانشگاه لرستان
چکیده:   (75 مشاهده)
باتولیت گرانیتی لاله زار در جنوب شرق کمربند ماگمایی ارومیه –دختر و نوار دهچ-ساردوییه قرار دارد. این توده دارای تراکم پایینی از تورمالین با ریخت­های گرهکی، رگه­ای و خورشیدی است. رخداد کم تورمالین در این توده را می­توان به اشباع بودن توده از بور نسبت داد. تورمالین­های مورد بررسی در گستره سری شورل-دراویت و تورمالین­های قلیایی قرار می­گیرند. بیشتر جانشینی­های صورت گرفته در این تورمالین­ها از نوع جانشینی­های Ca + Mg(O) = Na + Mg(OH)، Ca = X - vac + Na،
Ca + Mg = (X – vac + Al) - 1 و جانشنی منیزیم به جای آهن هستند. وجود منطقه­بندی­های آشکار در تورمالین­ها، مقادیر بالای منیزیم و مقادیر FeO/FeO + MgO کمتر از 6/0 بیان کننده رشد تورمالین­ها در سیستم­های باز و یک خاستگاه ماگمایی-گرمابی تا گرمابی برای تورمالین­هاست. از طرفی مقدار بالای عناصر خاکی نادر در تورمالین­ها و غنی­شدگی چند برابری از عناصر خاکی نادر سبک (LREE) و غنی­شدگی کمتر از عناصر خاکی نادر سنگین ( (HREEنسبت به کندریت و سنگ میزبان و غنی­شدگی از عناصر دگرگونی مانندCr ،V ،Ni ،Cu ،Zn  و Zr بیان کننده خاستگاه گرمابی برای این تورمالین­هاست.    
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نوع مطالعه: پژوهشي | موضوع مقاله: تخصصي
دریافت: ۱۳۹۷/۱۰/۸ | پذیرش: ۱۳۹۷/۱۰/۸ | انتشار: ۱۳۹۷/۱۰/۸

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