کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4696932 1351857 2016 14 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
The development of regolith exploration geochemistry in the tropics and sub-tropics
ترجمه فارسی عنوان
توسعه ژئوشیمی اکتشاف رگولیت در مناطق گرمسیری و مناطق خشک
کلمات کلیدی
ژئوشیمی چشم انداز، زمین زمینی، آب و هوا، نمونه برداری، تحلیل و بررسی
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات زمین شناسی اقتصادی
چکیده انگلیسی


• A brief history of geochemical exploration
• Pioneering use of exploration geochemistry in tropical Africa
• Landscape geochemistry as a framework to describe dispersion and exploration models
• Landscape models in exploration, and the formation of secondary Au, Ni and U deposits

This essay traces the development of geochemical exploration from its early beginnings in the modern era during the 1930s, concentrating especially in its application to deeply weathered terrain in the tropics and sub-tropics. Following promising results obtained in temperate regions in North America and Europe, test orientation surveys were conducted to see whether similar procedures were applicable in the tropics, where conventional geological prospecting was largely precluded due to the extensive cover of a deep lateritic regolith and consequent lack of outcrop. After initial work in Sierra Leone and Nigeria, the emphasis transferred to East Africa in the 1950s and 1960s, aimed principally at Cu exploration. Many of the basic principles for exploration in dominantly residual, free-draining terrain were quickly established in this period. Exploration in terrains with more complex weathering histories, however, raised a number of difficulties due to leaching and secondary concentrations of elements, problems in selecting and identifying appropriate sample media, and extensive transported overburden. These were encountered especially in more arid regions in Australia and Africa during exploration for Ni and Au during the 1970s and 1980s. This led to a change in approach, placing weathering and geochemical dispersion in the context of regolith and landscape evolution –a return to the early concept of landscape geochemistry. The 3D expression of mineralization in the landscape is depicted as empirical conceptual models, that account for both relict features and active processes, and portray element associations, dispersion mechanisms and host materials. They also indicate suitable sample media, sampling intervals and procedures for analysis and interpretation.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Ore Geology Reviews - Volume 73, Part 3, March 2016, Pages 380–393
نویسندگان
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