تکامل فیزیکوشیمیایی سیال گرمابی در سامانه مس پورفیری کوه اسفند، جنوب جیرفت، استان کرمان

زمین شناسی اقتصادی

دوره 16، شماره 2 - شماره پیاپی 41، 1403، صفحه 163-206   

نوع مقاله: مقاله پژوهشی

شناسه دیجیتال (DOI): 10.22067/econg.2024.1108

نویسندگان

افسانه سلطانی¹؛ علیرضا زراسوندی^{* 2}؛ نادر تقی پور³؛ محسن رضایی⁴؛ عادل ساکی⁵؛ مرتضی سجادیان⁶؛ غزال زراسوندی⁷

¹دانشجوی دکتری، گروه زمین‏ شناسی، دانشکده علوم زمین، دانشگاه شهید چمران اهواز، اهواز، ایران

²استاد، گروه زمین ‏شناسی، دانشکده علوم زمین، دانشگاه شهید چمران اهواز، اهواز، ایران

³دانشیار، دانشکده علوم زمین، دانشگاه دامغان، دامغان، ایران

⁴استادیار، گروه زمین ‏شناسی، دانشکده علوم زمین، دانشگاه شهید چمران اهواز، اهواز، ایران

⁵دانشیار، گروه زمین ‏شناسی، دانشکده علوم زمین، دانشگاه شهید چمران اهواز، اهواز، ایران

⁶کارشناس ارشد تحقیقات اکتشاف، مرکز تحقیقات و فناوری شرکت معدنی و صنعتی گلگهر، کرمان، ایران

⁷دانشجوی کارشناسی، گروه زمین‏ شناسی، دانشکده علوم زمین، دانشگاه شهید چمران اهواز، اهواز، ایران

چکیده

کانسار مس کوه اسفند در جنوبی ‏ترین بخش از کمربند ماگمایی ارومیه- دختر واقع‌شده است. توده ‏های نفوذی با طیف دیوریت تا کوارتزدیوریت و گرانودیوریت الیگوسن- میوسن در مجموعه آتشفشانی ائوسن جای گرفته ‏اند. بر اساس طبقه ‏بندی رگه- رگچه ‏ها، مرحله کانی ‏سازی اصلی شامل کوارتز پیریت کالکوپیریت مرتبط با دگرسانی پتاسیک است. بر اساس بررسی‌های سنگ‌نگاری، میان‌بارهای سیال در کانی کوارتز در سه گروه اصلی و هفت گروه فرعی طبقه ‏بندی می‏شوند: 1- میان‌بارهای سیال غنی از گاز شامل: میان‌بارهای سیال تک فازی گازی (V)، میان‌بارهای سیال دوفازی غنی از گاز ساده (VL) و میان‌بارهای سیال غنی از گاز همراه با فاز کدر (VLS) ، 2- میان‌بارهای سیال غنی از مایع شامل: میان‌بارهای سیال دوفازی غنی از مایع ساده (LV) و میان‌بارهای سیال غنی از مایع همراه با فاز کدر (LVS) و 3- میان‌بارهای سیال شور شامل: میان‌بارهای سیال سه فازی شور ساده (LVH) و میان‌بارهای سیال شور چند فازی (LVHS) حاوی فاز جامد هالیت هماتیت انیدریت سیلویت کالکوپیریت). میان‌بارهای سیال شور چند فازی با دما و شوری بالا (358 تا 598 درجه سانتی‏ گراد و 42 تا 70 درصد شوری معادل نمک طعام) با منشأ ماگمایی نخستین سیالات تشکیل‏ دهنده کانسار و میا‌ن‌بارهای سیال دوفازی غنی از مایع با دما و شوری پایین (290 تا490 درجه سانتی‏گراد و 11 تا 20 درصد شوری معادل نمک طعام) با منشأ ماگمایی- جوی مرتبط با آخرین گردش سیال گرمابی و اختلاط با سیال با شوری پایین‏ تر ‏هستند. کاهش دما ناشی از وقوع فرایند جوشـش ثانویه و اخـتلاط سـیالات ماگمایی و جوی به ناپایداری کمپلکس کلریدی حامل فلز مس و کانی‏ سازی در شرایط مساعد منجر‌شده است.

کلیدواژه‌ها

میان بارهای سیال؛ جوشش ثانویه؛ اختلاط سیال؛ رگه – رگچه؛ کوه اسفند؛ کمربند ماگمایی ارومیه- دختر

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