یافته‌های نوین زمین‌شناسی کاربردی

یافته‌های نوین زمین‌شناسی کاربردی

بررسی تبادلات آب به سنگ(W/R) در سیستم­ های کربناته با استفاده از شواهد سنگ ­شناسی و زمین ­شیمی عنصری (مثالی از سازند آسماری، جنوب باختری لرستان)

نویسندگان
1 دانشجوی کارشناسی‌ارشد مهندسی نفت، واحد مشهد، دانشگاه آزاد اسلامی، مشهد، ایران
2 گروه مهندسی نفت، معدن و زمین‌شناسی، واحد مشهد، دانشگاه آزاد اسلامی، مشهد، ایران
3 شرکت ملی حفاری ایران، ایران
چکیده
به‌منظور بررسی تبادلات آب به سنگ و به دنبال آن تحلیل سیستم­های دیاژنزی و کانی­شناسی اولیه واحدهای کربناته سازند آسماری، یک برش چینه­شناسی سطح­الارضی واقع در تاقدیس ریت (جنوب‌باختری لرستان) به ضخامت 131 متر انتخاب و مورد نمونه­برداری قرار گرفته است. سنگ­شناسی این سازند تناوبی از سنگ‌های­آهکی و آهکی دولومیتی می­باشد. در این پژوهش تعداد 23 نمونه به روش تجزیه عنصری EDX مورد آنالیز قرار گرفته­ و عناصر اصلی و فرعی در آن­ها جهت تفسیر سیستم­های دیاژنزی و کانی­شناسی اولیه استفاده شده است. شواهد زمین­شیمی عنصری نشان داد نمونه­های مورد مطالعه در محدوده­ سنگ­آهک­های آراگونیتی گوردون تاسامانیا و کربنات­های آراگونیتی سازند مزدوران قرار دارند که دلیلی بر آراگونیتی بودن کانی­شناسی اولیه سنگ­آهک­های سازند آسماری در برش مورد مطالعه دارد. ترسیم مقادیر Sr/Ca در برابرMn بیانگر یک سیستم دیاژنزی غالب بسته تا کمی باز به صورت ضعیف و با تبادل آب به سنگ پایین(W/R) برای کربنات­های سازند آسماری در برش تاقدیس ریت می­باشد. وجود کانی­شناسی اولیه آراگونیتی، ناپیوستگی نه‌چندان شدید و طولانی مدت، آب و هوا و کنترل‌کننده­های ذاتی سنگ مانند تراوایی، کانی­شناسی اولیه و پتانسیل دیاژنزی می­تواند کنترل کننده مهمی در میزان نسبت آب به سنگ باشد. این عوامل در رأس سازند آسماری سبب شده‌اند که بخش بالایی این توالی تحت تأثیر دیاژنز جوی بسیار ضعیف قرار گیرد؛ محدود بودن سیمان‌های دیاژنز جوی در نمونه‌های مورد مطالعه و انحلال جزئی اجزای زیستی در این سازند، می‌تواند شاهدی بر این موضوع باشد. بنابراین می­توان گفت سیستم دیاژنزی در توالی­های سازند کربناته آسماری در برش تاقدیس ریت یک سیستم دیاژنزی غالباً بسته بوده و به سمت بالای توالی به صورت ضعیف باز می­باشد.
کلیدواژه‌ها

عنوان مقاله English

Investigating water-to-rock exchanges (W/R) in carbonate system Using Petrographic and Elemental Geochemistry Evidence (An example of the Asmari Formation, Southwestern Lorestan)

نویسندگان English

Lefteh Kabizadeh Arab 1
Mohsen Allameh 2
Ramin Mokfi 3
1 M.Sc. Student, Dept. of Petroleum Engineering, Ma. C., Islamic Azad University, Mashhad, Iran
2 Dept. of Petroleum Engineering, Mining and Geology, Ma. C., Islamic Azad University, Mashhad, Iran
3 National Iranian Drilling Company, Iran
چکیده English

In order to investigate water-to-rock exchanges and subsequent to the diagenetic systems and the primary mineralogy of the carbonate units of the Asmari Formation, a 131-meter-thick surface stratigraphic section located in the Rit anticline (southwestern Lorestan) was selected and sampled. The lithology of this formation comprises alternating layers of carbonate and dolomitic carbonate rocks. In this study, 23 samples were analyzed using elemental EDX analysis to determine the major and trace element composition and interpret the diagenetic systems and original mineralogy. Elemental geochemical evidence indicates that the studied samples fall within the compositional range of aragonitic limestones from Gordon, Tasmania, and aragonitic carbonates of the Mozduran Formation. This supports the interpretation that the original mineralogy of the Asmari limestones in the studied section was aragonitic. Plotting Sr/Ca ratios against Mn contents reveals a predominantly closed to slightly open diagenetic system, characterized by weak water–rock interaction (W/R), for the Asmari carbonates in the Rit anticline section. The presence of primary aragonitic mineralogy, the lack of significant discontinuities, the prevailing climatic conditions, and intrinsic rock properties such as permeability, original mineralogy, and diagenetic potential appear to have played key roles in controlling the water-to-rock ratio. These factors contributed to the limited impact of meteoric diagenesis in the upper part of the sequence, as evidenced by the scarcity of meteoric cement and the partial dissolution of bioclasts in the studied samples. Thus, it can be concluded that the diagenetic system within the carbonate succession of the Asmari Formation at the Rit anticline is dominantly closed, becoming weakly open towards the top of the sequence.

کلیدواژه‌ها English

Asmari Formation
Diagenetic System
Elemental Geochemistry
Zagros
Lorestan
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  • تاریخ دریافت 14 تیر 1404
  • تاریخ بازنگری 24 مرداد 1404
  • تاریخ پذیرش 25 شهریور 1404