سامانه مدیریت نشریات علمی دانشگاه دامغان

شرافت, شهزاد, ترک‌زاده, زهرا, مکی‌زاده, محمدعلی. (1404). رخداد سپیولیت در فرامافیک‌های شمال نائین. مجله زمین شیمی ایران, 26(1), 219-228. doi: 10.29252/ijcm.26.1.219
شهزاد شرافت; زهرا ترک‌زاده; محمدعلی مکی‌زاده. "رخداد سپیولیت در فرامافیک‌های شمال نائین". مجله زمین شیمی ایران, 26, 1, 1404, 219-228. doi: 10.29252/ijcm.26.1.219
شرافت, شهزاد, ترک‌زاده, زهرا, مکی‌زاده, محمدعلی. (1404). 'رخداد سپیولیت در فرامافیک‌های شمال نائین', مجله زمین شیمی ایران, 26(1), pp. 219-228. doi: 10.29252/ijcm.26.1.219
شرافت, شهزاد, ترک‌زاده, زهرا, مکی‌زاده, محمدعلی. رخداد سپیولیت در فرامافیک‌های شمال نائین. مجله زمین شیمی ایران, 1404; 26(1): 219-228. doi: 10.29252/ijcm.26.1.219

رخداد سپیولیت در فرامافیک‌های شمال نائین

مجله بلورشناسی و کانی شناسی ایران
مقاله 17، دوره 26، شماره 1 - شماره پیاپی 69، فروردین 1397، صفحه 219-228    اصل مقاله (5.22 M)
شناسه دیجیتال (DOI): 10.29252/ijcm.26.1.219
نویسندگان
شهزاد شرافت* 1؛ زهرا ترک‌زاده1؛ محمدعلی مکی‌زاده2
1دانشگاه پیام‌نور
2دانشگاه اصفهان
چکیده
در این پژوهش، رخداد کانی سپیولیت برای نخستین بار از سنگ­های فرامافیک توالی افیولیتی شمال نائین گزارش می­شود. سپیولیت کانی رسی آبدار با ساختار الیافی است که به­واسطه ویژگی­های منحصر به فرد خود در صنایع مختلف کاربرد دارد. تشکیل سپیولیت، پیامد واکنش­های متعددی است که در سنگ­های فرامافیک توالی افیولیتی شمال نائین رخ داده است. این فرایند طی سه مرحله اصلی انجام شده است. ابتدا سیالات گرمابی با تاثیر بر سنگ­های فرامافیک، آنها را به سرپانتینیت تبدیل کرده­اند. هجوم سیالات دارای CO2-H2O در امتداد سطوح ضعف سرپانتینیت­های برشی و خرد شده، باعث انحلال سرپانتینیت و کربناته شدن آن شده­اند. طی کربناته شدن سرپانتینیت­ها، واکنش بین سنگ­های فرابازی با محلول­های گرمابی سبب تشکیل محلولی غنی از Mg  و/یا  Si در دمای پائین شده و سرانجام، کانی سپیولیت در نتیجه فعالیت سیالات گرمابی غنی از CO2،H2O و SiO2 شکل گرفته است.     
کلیدواژه‌ها
سپیولیت؛ سنگ‌های فرامافیک؛ لیستونیت؛ سیالات گرمابی؛ افیولیت نائین؛ ایران مرکزی
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