بررسی شیمی کانی و دما فشار سنجی درشت بلور‌های پلاژیوکلاز، پیروکسن و آمفیبول سنگ‌های آتشفشانی حسین آباد (جنوب شرقی ابهر)

نوع مقاله : مقاله پژوهشی

نویسندگان

1 گروه زمین شناسی، واحد علوم و تحقیقات، دانشگاه آزاد اسلامی، تهران، ایران

2 گروه زمین شناسی، واحد تهران شمال، دانشگاه آزاد اسلامی، تهران، ایران

3 گروه زمین شناسی، دانشگاه لرستان، خرم آباد، ایران

4 گروه زمین شناسی، واحد کهنوج، دانشگاه آزاد اسلامی، کهنوج، ایران

چکیده

منطقه حسین آباد در 120 کیلومتری  جنوب شرقی زنجان واقع است. سنگ­های آتشفشانی در این منطقه دارای سن ائوسن و جوانتر از آن هستند. سنگ­های آتشفشانی طیفی از گدازه­های داسیتی، تراکی آندزیتی و آندزیتی به همراه توف را شامل می­شوند. از نظر کانی­شناسی، سنگ­های آتشفشانی مورد بررسی دارای کوارتز، فلدسپات قلیایی، پلاژیوکلاز فراوان، پیروکسن و آمفیبول هستند. فلدسپات قلیایی از نوع سانیدین و پلاژیوکلازها از نوع الیگوکلاز و آندزین هستند. بافت­های پورفیری، پورفیری ریزسنگی، گلومرو پورفیری و خال خال بافت در این سنگ­ها غالب هستند. بررسی شیمی کانی­های سنگ­های منطقه نشان می­دهد که ترکیب کلینوپیروکسن­های این سنگ­ها از انواع دیوپسید و اوژیت است. آمفیبول موجود در این سنگ­ها از نوع ماگمایی و کلسیمی و دارای ترکیب شیمیایی پارگازیت است. بر اساس نمودارهای تعیین نوع ماگما، ماگمای سازنده سنگ­های آتشفشانی منطقه مورد بررسی قلیایی است. نمودارهای دما-فشارسنجی بر پایهی ترکیب پلاژیوکلاز، پیروکسن و آمفیبول نشان­دهنده دمای 700 تا 750 درجه سانتیگراد و فشار 5 تا 6.5 کیلوبار هستندکه با ژرفای پوسته میانی-زیرین همخوانی دارد. از این رو، این سنگ­ها در یک کرانه فعال قاره­ای تشکیل شده­اند.

کلیدواژه‌ها

عنوان مقاله [English]

Investigation of mineral chemistry and geothermobarometry of plagioclase, pyroxene and amphibole phenocrysts of Hossein Abad volcanic rocks (southeast of Abhar)

نویسندگان [English]

  • Masoud Nazari 1
  • Mohammad Ali Arian 2
  • Ali Solgi 1
  • Reza Zarei Sahamiyeh 3
  • Abdollah Yazdi 4
1 Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran
2 Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran
3 Department of Geology, Lorestan University, Khorramabad, Iran
4 Department of Geology, Kahnooj Branch, Islamic Azad University, Kahnooj, Iran
چکیده [English]

The Hossein Abad area is located 120 km southeast of Zanjan. The volcanic rocks in this area belong to Eocene and younger a ges. Volcanic rocks include dacitic, trachyandesite and andesitic lavas, as well as tuff. Volcanic rocks have quartz, alkali feldspar, abundant plagioclase, pyroxene and amphibole. The alkali feldspar is Sanidine and plagioclases are oligoclase and andesine. The Porphyritic, microlithic porphyritic, glomeroporphyritic and poikilitic textures are predominant in these rocks. Examining the mineral chemistry of rocks in the study area shows that the clinopyroxenes are diopside and augite. Amphiboles in these rocks are magmatic and calcic with the chemical composition of pargasite. Based on magmatic diagrams, rocks in studied area are alkaline. According to the thermobarometric diagrams, these rocks have formed at temperature and pressure ranges of 700-750℃ and 5-6.5 kbar respectively. These values correspond to the depth of middle-lower crust. The rocks are formed in the active continental margin.

کلیدواژه‌ها [English]

  • Thermobarometry
  • amphibole
  • plagioclase
  • volcanic rocks
  • Abhar

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  • تاریخ دریافت: 26 شهریور 1402
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