کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
9535080 | 1640267 | 2005 | 15 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Penetration of surface-evaporated brines into the Proterozoic basement and deposition of Co and Ag at Bou Azzer (Morocco): Evidence from fluid inclusions
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موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی
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چکیده انگلیسی
Chlorinity, cation (Na/Ca ca. 2.2) and halogen ratios (Cl/Br from 300 to 360) are typical of deep basinal brines, especially of surface-evaporated brines that have exceeded halite saturation. The primary brines were modified by fluid-rock interaction during burial and migration through the basement. Ag-deposition was probably favoured by dilution and cooling due to the mixing of brines with less saline fluids. Similarities between the Ag-brines from Bou Azzer, Zgounder and Imiter suggest a regional scale circulation of basinal brines during extension probably later than the Triassic, during the early stages of rifting of the Atlantic.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of African Earth Sciences - Volume 41, Issues 1â2, January 2005, Pages 25-39
Journal: Journal of African Earth Sciences - Volume 41, Issues 1â2, January 2005, Pages 25-39
نویسندگان
Samira Essarraj, Marie-Christine Boiron, Michel Cathelineau, David A. Banks, Mohamed Benharref,