خاستگاه، سنگ‌شناسی و زمین‌شیمی سنگ‌های خروجی گستره مس زندی (راین)، جنوب شرق استان کرمان

نوع مقاله : مقاله پژوهشی

نویسندگان

گروه زمین شناسی ، دانشکده علوم پایه ، دانشگاه سیستان و بلوچستان ، زاهدان ، ایران

چکیده

گستره مس زندی (استان کرمان) در منطقه‌ای کنار روستای گور در 70 کیلومتری جنوب شرق شهرستان راین واقع است. این گستره از نظر تقسیمات زمین‌شناسی ایران، در پهنه ایران مرکزی (کمربند آتشفشانی ارومیه- دختر) و نوار ماگمایی دهج- ساردوئیه قرار دارد. در این گستره روانه‌هایی وجود دارند که بر اساس بررسی­های صحرایی و سنگ­نگاری، ترکیب سنگ‌شناسی آنها اغلب حدواسط تا اسیدی شامل آندزیت، تراکی آندزیت، داسیت، ریولیت و سنگ‌های آذرآواری وابسته به آن­ها و به مقدار کم بازالت و آندزیت بازالت است. آنها اغلب دارای بافت پورفیری با خمیره ریزسنگی هستند. سنگ‌های حدواسط تا اسیدی  از کانی‌های پلاژیوکلاز، هورنبلند، بیوتیت و کوارتز تشکیل شده­اند و سنگ‌های بازالتی دارای کانی‌های پیروکسن و پلاژیوکلاز هستند. در نمودارهای عنکبوتی الگوی عناصر فرعی و خاکی نادر بهنجار شده نسبت به مراجع کندریت و گوشته اوّلیه، عناصر خاکی نادر سبک (LREE) غنی‌شدگی ضعیفی نسبت به عناصر خاکی نادر سنگین (HREE) دارند. اغلب عناصر در نمودارهای مختلف زمین شیمیایی الگوی به نسبت مشابه با سنگ­های وابسته به مناطق کرانه فعال قاره را نشان می­دهند. عناصر Rb,Th و Ba ناهنجاری مثبت و عناصر Ti و P < /span> ناهنجاری منفی نشان می­دهند. نمودارهای سنگ­زایی و زمین­ساختی ماگمایی به همراه ناهنجاری به نسبت منفی Eu در سنگ­های مورد بررسی بیانگر وابستگی آنها به ماگماهای مناطق فرورانشی است. از این رو، به نظر می­رسد که این سنگ‌ها مشابه بسیاری از سنگ‌های پهنه آتشفشانی-نفوذی ارومیه- دختر در نتیجه ماگماهای برآمده از فرورانش صفحه عربی به زیر صفحه ایران، بوجود آمده­اند.

کلیدواژه‌ها

عنوان مقاله [English]

Origin, petrology and geochemistry of extrusive rocks in the Zandi Copper deposit (Rayen), Southeastern Kerman Province

نویسندگان [English]

  • Neda moslamemehni
  • habib Biabangard
Department of Geology, Faculty of Basic Sciences, University of Sistan and Baluchistan, Zahedan, Iran
چکیده [English]

The Zandi copper (Kerman Province) is located about 70 Km of Rayan city and adjacent of Gavar village.  Based on geological classification of Iran, this region belongs to Iranian Central Zone (Urmia- Dokhtar) and Dehaj-Sardoiyeh magmatic belt. In this area, there are a lot of acidic to intermediate lava flows with andesite, trachy andesite, dacite, rhyolite, and pyroclastic rocks and low basaltic and basaltic andesite in composition. These rocks have usually porphyric textures. Acidic to intermediate lavas are composed of plagioclase, hornblende, biotite and quartz minerals and basaltic rocks have plagioclase with pyroxene. In the spider diagrams, accessory and rare earth elements patterns of normalized to Chondrite and primary mantle; show light rare earth elements (LREE) are lower enriching than heavy rare earth elements (HREE). Most of elements in different geochemical diagrams show a relatively similar pattern to the rocks belonging to the active continental margin regions. Rb, Th and Ba elements have positive anomalies while Ti and P elements have negative anomalies. The petrogenetic and tectonomagmatic diagrams with nearly negative anomaly in the Eu element in these lavas indicate their dependence on magmatic subduction zone. It seems that these lavas are formed similar to many rocks in volcano-plutonic Urmia-Dokhtar Zone, which resulted magmas from subduction of the Arabian plate under the Iranian plate.

کلیدواژه‌ها [English]

  • extrusive rocks
  • Zandi copper
  • calc-alkaline
  • Neotethyan
  • Urmia-Dokhtar
  • Iran

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