‌زمین دما- فشارسنجی و خاستگاه گابروهای منطقه جغین جنوب شرقی شهرستان رودان، استان هرمزگان

نوع مقاله : مقاله پژوهشی

نویسندگان

دانشگاه هرمزگان

چکیده

سنگ­های افیولیتی جغین، در شرق استان هرمزگان و جنوب شرقی شهرستان رودان در راستای پهنه مکران واقع هستند. در بررسی­های سنگ­شناسی این منطقه، توده­های فرابازی چون دونیت و هارزبورژیت و توده­های بازی شامل گابرونوریت و بازالت شناسایی شده­اند. بر اساس بررسی شیمی کانی­ها، ترکیب پیروکسن­های سنگ­های­ بازی (گابرونوریت) منطقه بیشتر از نوع آهن و منیزیوم­دار و فقیر ازسدیم بوده،که شامل کلینوپیروکسن با ترکیب دیوپسیدی و گاهی نیز اوژیت است و همچنین ارتوپیروکسن­ها بیشتر با ترکیب برونزیتی هستند. کانی­­های پلاژیوکلاز موجود در سنگ­های گابرونوریتی نیز به دونوع با سدیم بالا و کلسیم متوسط تقسیم می­شوند که بیشتر ترکیبی بین آلبیت تا بیتونیت دارند. با توجه به دماسنجی این توده­ها و استفاده از روش دو پیروکسن دمای تشکیل این توده­ها حدود 800-1200 درجه سانتی­گراد تعیین گردید و همچنین در این بین با استفاده از روش فشارسنجی توزیع آلومنیوم در پیروکسن­ها فشار حاکم بر تشکیل کلینوپیروکسن­ها نیز حدود 6-12 کیلوبار برآورد می­شود.    

کلیدواژه‌ها


عنوان مقاله [English]

Geothermobarometry and pryrogenesise of Jaghin Gabbro in southeast of Rudan city, Hormozgan Province

نویسندگان [English]

  • gholamreza Ghadami
  • Habib Ebadi
  • jaber Jamal poor
Hormozgan University
چکیده [English]

Jaghin ophiolite rocks are located in the east of Hormozgan Province and southeast of Rudan city in the ‎direction of the Makran zone. Lithologically, ultrabasic rocks such as dunite and harzburgite, and basic magma, including gabbro-norite and basalt, have been identified. According to chemical crystal analysis, the composition of pyroxenes in basic (Gabbro-norite) rocks is more than iron and magnesium, and poor of sodium, which included clinopyroxen with diopside and sometimes augite composition, as well as orthopyroxene is more than bronzite composition. Plagioclase crystals present in gabbro-norite rocks, also divide into high-sodium and medium-calcium types, which have mostly composition between albite and bitonite. Due to the thermometric of these masses and the utilize of the two-pyroxene method, the ‎temperature of forming these masses is determined to be 800-1200 °C and‎, also using the barometric of aluminum distribution in pyroxenes, the pressure on the clinopyroxenes formation estimated to be about 6-12 kbars.

کلیدواژه‌ها [English]

  • plagioclase
  • pyroxene
  • gabbro-norite
  • dunite
  • basic masses
  • Jaghin
  • Makran zone
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