سامانه مدیریت نشریات علمی دانشگاه دامغان

الماسی, علیرضا, ارجمندزاده, رضا, فرانسیسکو سانتوز, ژوزه, کریم‌پور, محمدحسن. (1404). شیمی سنگ و ایزوتوپ‌های Sr-Nd توده‌های نیمه‌عمیق مافیک- حدواسط کاشمر، شاهدی بر فرورانش حوضه پشت کمان سبزوار به زیر بلوک لوت. مجله زمین شیمی ایران, 25(4), 711-726. doi: 10.29252/ijcm.25.4.711
علیرضا الماسی; رضا ارجمندزاده; ژوزه فرانسیسکو سانتوز; محمدحسن کریم‌پور. "شیمی سنگ و ایزوتوپ‌های Sr-Nd توده‌های نیمه‌عمیق مافیک- حدواسط کاشمر، شاهدی بر فرورانش حوضه پشت کمان سبزوار به زیر بلوک لوت". مجله زمین شیمی ایران, 25, 4, 1404, 711-726. doi: 10.29252/ijcm.25.4.711
الماسی, علیرضا, ارجمندزاده, رضا, فرانسیسکو سانتوز, ژوزه, کریم‌پور, محمدحسن. (1404). 'شیمی سنگ و ایزوتوپ‌های Sr-Nd توده‌های نیمه‌عمیق مافیک- حدواسط کاشمر، شاهدی بر فرورانش حوضه پشت کمان سبزوار به زیر بلوک لوت', مجله زمین شیمی ایران, 25(4), pp. 711-726. doi: 10.29252/ijcm.25.4.711
الماسی, علیرضا, ارجمندزاده, رضا, فرانسیسکو سانتوز, ژوزه, کریم‌پور, محمدحسن. شیمی سنگ و ایزوتوپ‌های Sr-Nd توده‌های نیمه‌عمیق مافیک- حدواسط کاشمر، شاهدی بر فرورانش حوضه پشت کمان سبزوار به زیر بلوک لوت. مجله زمین شیمی ایران, 1404; 25(4): 711-726. doi: 10.29252/ijcm.25.4.711

شیمی سنگ و ایزوتوپ‌های Sr-Nd توده‌های نیمه‌عمیق مافیک- حدواسط کاشمر، شاهدی بر فرورانش حوضه پشت کمان سبزوار به زیر بلوک لوت

مجله بلورشناسی و کانی شناسی ایران
مقاله 3، دوره 25، شماره 4 - شماره پیاپی 68، دی 1396، صفحه 711-726    اصل مقاله (1.82 M)
شناسه دیجیتال (DOI): 10.29252/ijcm.25.4.711
نویسندگان
علیرضا الماسی* 1؛ رضا ارجمندزاده2؛ ژوزه فرانسیسکو سانتوز3؛ محمدحسن کریم‌پور4
1دانشگاه لرستان
2دانشگاه پیام نور
3دانشگاه آویرو
4دانشگاه فردوسی
چکیده
براساس شواهد صحرایی، توده­های نیمه­عمیق مافیک-حدواسط کاشمر به دو مجموعه قدیمی (غالبا استوک­های گابرو، دیوریت، کوارتزدیوریت/مونزودیوریت) و مجموعه جدید (دسته آذرین تیغه­های موازی کوارتزمونزودیوریتی) تقسیم می­شوند. از لحاظ روابط قطع­شدگی، مجموعه قدیمی سنی بین قدیمی­ترین واحدهای آتشفشانی منطقه (57 میلیون سال) و گرانیتوئیدهای ائوسن (40 میلیون سال) دارد، اما دسته دایک­های موازی به پس از ائوسن (الیگوسن ؟) نسبت داده می­شوند. توده­های نیمه­عمیق مافیک-حدواسط با ویژگی آهکی-قلیایی پتاسیم بالا تا شوشونیتی، متاآلومین تا کمی پرآلومین، غنی­­شدگی LILE/HFSE و LREE [8/6-3/5La/Yb)N = )] و تخلیه از HREE، یادآور کمان­های منطقه فرورانش­اند. این ویژگی­ها به همراه بی­هنجاری منفی Eu نشان­دهنده تشکیل ماگما در عمق پایداری پلاژیوکلاز و آلودگی ماگما با پوسته قاره­ای است، که طی ذوب سنگ گارنت باقیمانده است. روند خطی اکسید عناصر اصلی و فرعی در نمودارهای هارکر دلالت بر اهمیت تبلور جدایشی در تکامل ماگمایی دارد. میانگین نسبت­های ایزوتوپ اولیه 87Sr/86Sr و 143Nd/144Nd (در 50 میلیون سال) برای نمونه­های مجموعه قدیم به ترتیب دارای گستره 7062/0-7054/0 و 51264/0-51262/0 و میزان εNdi دارای گستره 08/1 تا 42/1 است. نسبت­های ایزوتوپ اولیه 87Sr/86Sr و 143Nd/144Nd (در 30 میلیون سال) برای دسته دایک­های موازی به ترتیب 7056/0 و 51263/0 و مقدار εNdi آن 59/0 است. مقادیر εNdi مثبت و ISr کم در همه سنگ ها همراه با TDM اشان (8/0-6/0) ، دلالت بر این دارد که از ذوب بخشی منبع گوشته سنگ­کره­ای، که با گدازه­های حاصل از فرایندهای فرورانش قبل تر از آن تعدیل شده است، تشکیل شده اند. براساس نمودارهای Th/Ta نسبت به Nb/Ta و نمودار Nb/Y نسبت به Zr/Y، هر دوی فرآیندهای فرورانش و کافت­زایی در تشکیل سنگ های کاشمر دخیل بوده­اند. این ویژگی با فرورانش پوسته اقیانوسی سبزوار به زیر قلعه لوت سازگار است.
کلیدواژه‌ها
توده‌های نیمه عمیق؛ زمین‌شیمی؛ ایزوتوپ‌های Sr-Nd؛ پشت کمان؛ کاشمر
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