بررسی ویژگی های ژئوشیمی و محیط زمین ساختی آداکیت های کواترنری سبلان

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشجوی دکتری پترولوژی، دانشکده علوم، واحد علوم و تحقیقات، دانشگاه آزاد اسلامی، تهران، ایران

2 استادیار، دانشکده علوم، واحد علوم و تحقیقات، دانشگاه آزاد اسلامی، تهران، ایران

3 استادیار، دانشکده علوم، دانشگاه آزاد اسلامی ، مشکین شهر، ایران

چکیده
فعالیت آتشفشانی کواترنر به عنوان آخرین تکاپوی ماگمایی در ایران تکامل بخش مخروط های آتشفشانی بزرگی همچون دماوند، سهند، سبلان، تفتان و بزمان و همچنین روانه های گدازه ای مانند بازالت های ماکو و بلوک لوت است. سبلان، عضو جوانی از مجموعه آتشفشانی سنوزوئیک، متعلق به کمان ماگمایی البرز AMA)) است. در کوه سبلان، مجموعه­ای از سنگ­های آتشفشانی با ترکیب آندزیت، آندزیت بازالتی، داسیت، ریوداسیت و تراکی آندزیت وجود دارد. بافت این سنگ­ها اغلب پورفیریتیک با خمیره میکرولیتی، پورفیریتیک حفره­دار، گاهی گلومروپورفیری، غربالی و تراکیتی می­باشند. از کانی­های اصلی می­توان به پلاژیوکلاز و یک یا چند کانی مافیک مانند هورنبلند و پیروکسن اشاره کرد. کانی­های ثانویه شامل کانی اوپاک، ایدنگزیت، کلریت و کلسیت است. در نمودارهای چند عنصری عادی شده، غنی شدگی نسبی K و Ba ،Rb و تهی شدگی نسبی Ti و Ta ،Nb حاکی از ماگماتیسم متأثر از فرایندهای فرورانشی است. این سنگ ها از نظر ترکیب شیمیایی عناصر اصلی مانند K2O ،Na2O ،MgO ، Al2O3, SiO2 Mg  و  K2O/Na2O و ترکیب عناصر کمیاب مانند Cr ،Ni ،Yb ،Y ،Sr ،Rb Sr/Y  و La/Yb  در محدودۀ سنگ های آداکیتی قرار می گیرند. به علاوه  ژئوشیمی این سنگ ها از جمله تمرکز Cr ،MgO ،Th ،Rb ،Th/Ce و  K2O/Na2O با آداکیت های مشتق از ذوب بخشی ورقه اقیانوسی فرورانده شده هم خوانی بهتری دارد. براساس نمودارهای سنگ زادی، ماگمای آداکیتی سازنده این سنگ ها، از ذوب بخشی یک سنگ منبع اکلوژیتی یا گارنت آمفیبولیتی حاصل از دگرگونی ورقه اقیانوسی فرورانده شده نئوتتیس به زیر ایران مرکزی، به وجود آمده است.

کلیدواژه‌ها

موضوعات


عنوان مقاله English

Investigating the geochemical characteristics and tectonic environment of Quaternary Sablan adakites

نویسندگان English

Akram Abdolahadi 1
Seyed Jamal Sheikh Zakariaee 2
Zahed Mousavi 3
1 PhD student of Petrology, Faculty of Science, Islamic Azad University, Science and Research Unit, Tehran, Iran
2 Assistant Professor, Faculty of Science, Islamic Azad University, Department of Science and Research, Tehran, Iran
3 Assistant Professor, Faculty of Science, Islamic Azad University, Meshkin Shahr, Iran
چکیده English

Quaternary volcanic activity, as the last magmatic effort in Iran, is the evolution of large volcanic cones such as Damavand, Sahand, Sablan, Taftan and Bazman, as well as lava flows such as Mako basalts and Lot block. Sablan, a young member of the Cenozoic volcanic complex, belongs to the Alborz magmatic arc (AMA). In Sablan Mountain, there is a collection of volcanic rocks with the composition of andesite, basaltic andesite, dacite, rhyodacite and trachy andesite. The texture of these rocks is mostly porphyritic with microlithic clay, porous porphyritic, sometimes glomeroporphyric, sieve and trachytic. Among the main minerals, plagioclase and one or more mafic minerals such as hornblende and pyroxene can be mentioned. Secondary minerals include opaque minerals, edengsite, chlorite and calcite. In the normalized multi-element diagrams, relative enrichment of K, Ba, Rb and relative depletion of Ti, Ta, and Nb indicate magmatism affected by subduction processes. In terms of the chemical composition of these rocks, the main elements such as K2O, Na2O, MgO, Al2O3, SiO2 Mg# and K2O/Na2O and the composition of rare elements such as Cr, Ni, Yb, Y, Sr, Rb Sr/Y and La/Yb are in the range Adakite stones are placed. In addition, the geochemistry of these rocks, including the concentration of Cr, MgO, Th, Rb, Th/Ce, and K2O/Na2O, is in better agreement with the adakites derived from partial melting of the subducted oceanic sheet. According to the petrographic diagrams, the adakitic magma forming these rocks was formed from the partial melting of an eclogitic source rock or amphibolite garnet resulting from the metamorphism of the subducted Neotethys oceanic plate under Central Iran. Keywords: petrology, PULL PARAT, petrogenesis, Iran.

کلیدواژه‌ها English

Petrology
PULL PARAT
Petrogenesis
Iran
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