سنگ‌نگاری و شیمی کانی زئولیت در گدازه‌های بالشی و دایک‌های دیابازی جنوب غرب الشتر (شمال لرستان)

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه لرستان

2 دانشگاه آزاد اسلامی واحد علوم تحقیقات تهران

3 دانشگاه تبریز

چکیده

گدازه­های بالشی و دایک­های دیابازی منطقه جنوب غرب الشتر میزبان گونه­های مختلف از زئولیت­ها و کانی­های ثانوی هستند. زئولیت­ها به صورت بادامکی و رگه­ای و از تجزیه کانی­های اولیه تشکیل شده­اند. براساس بررسی­های صحرایی، پراش پرتوی ایکس (XRD) و تجزیه ریزکاو الکترونی، زئولیت­های ناترولیت (فراوان­ترین زئولیت)، مزولیت، اسکولسیت و آنالسیم در گدازه­های بالشی و دایک­های دیابازی منطقه مورد بررسی شناسایی شدند. میانگین نسبت  Si/Al برای ناترولیت، مزولیت، اسکولسیت و آنالسیم به ترتیب 46/1، 49/1، 62/1 و 29/2 محاسبه شد. این زئولیت­ها طی دو مرحله از سیال­های گرمابی دگرگونی در طول شکستگی­ها و در حفره­های سنگ میزبان در دمای کمتر از 250 درجه سانتی­گراد تشکیل شده­اند. بررسی ویژگی­های زمین­شیمیایی سنگ میزبان زئولیت­ها نشان می­دهد که نوع ماگمای تشکیل دهنده آنها آهکی قلیایی تا تولئیتی و محیط زمین­ساختی آنها وابسته به محیط­های درون صفحه­ای و مورب است.      

کلیدواژه‌ها

عنوان مقاله [English]

Petrography and mineral chemistry of zeolite in pillow lavas and diabasic dykes, southwest of Aleshtar (north of Lorestan)

نویسندگان [English]

  • Safarpour Feizi 1
  • Ahmadi Khalaji 1
  • Zarei Sahamieh 1
  • Kiani 2
  • Mohammadi Chaghamarani 3
1
2
3
چکیده [English]

The Pillow lava and diabase dykes of the southwestern region of Aleshtar are host different species of zeolites and secondary minerals. Zeolites are formed by the cavities and veins and decomposed from primary minerals. Based on field studies, X-ray diffraction (XRD) and Electron Microprobe Analysis (EPMA), natrolite zeolites (most abundant zeolites), mesolite, scolecite and analcime have been identified in the pillow lava and diabase dykes in the study area. The average Si/Al ratios for natrolite, mesolite, scolecite and analcim are 1.46, 1.49, 1.62 and 2.29, respectively. These zeolites are formed during two stages of metamorphic hydrothermal fluids, during fractures and in the cavities of host rocks and at temperatures below 250 °C. The investigation of the geochemical properties of zeolites host rocks, shows that their magmatic series is calc-alkaline to tholeiitic and their tectonic environment depends on the mid-ocean ridges (MORB).

کلیدواژه‌ها [English]

  • Lorestan
  • Aleshtar
  • petrography
  • Mineral chemistry
  • zeolite

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  • تاریخ دریافت: 14 فروردین 1400
  • تاریخ بازنگری: 29 اردیبهشت 1400
  • تاریخ پذیرش: 11 خرداد 1400

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