نتایج جستجو برای: secondary minerals

تعداد نتایج: 324064  

2002
John D. Arthington

Pasture forage is the most significant contributor to the trace mineral nutrition of grazing beef cattle. Mineral supplementation in beef cattle can be divided into two broad categories, macro-minerals and micro-minerals. These categories are based on the amount of mineral required in the cow’s diet. As a rule of thumb, micro-minerals are required in amounts less than 1 gram per day compared to...

2006
B. K. G.

An account is given of the interactions between clay minerals and organic polymers with particular reference to their applications in agriculture, foundation engineering and industry.

Journal: :iranian journal of earth science 0
jamal tarrah islamic azad university, bandar abbas branch, geology department, bandar abbas, iran zahra abedpour islamic azad university, bandar abbas branch, geology department, bandar abbas, iran karl strauss institute of mineralogy-geochemistry and salt deposits, university of clausthal, germany thomas schirmer institute of mineralogy-geochemistry and salt deposits, university of clausthal, germany kurt mengel institute of mineralogy-geochemistry and salt deposits, university of clausthal, germany

ten chromite ores from ophiolite complexes in se iran were analyzed mineralogically by xrd, chemically by xrf, and mineral chemistry by epma. the identified paragenesis of silicate minerals of chromite ores with the x-ray diffraction is pronounced differently. it consists of secondary phases formed as serpentine, cr-containing chlorite (kaemmererite), chromic garnet (uarovite) with preserved pa...

Journal: :زمین شناسی اقتصادی 0
علی امامعلی پور مستوره یوسفی مهدیه کریملو

alteration of ophiolitic ultramafic rocks, formation of listwaenite and associated mineralization are interesting phenomena of metallogeny of khoy ophiolite. it seems that the hydrothermal circulations responsible for mercury mineralization were derived from geothermal systems caused by intermediate to acidic magmatism in neogene-pleistocene time. reactivation of brecciated serpentinite with hy...

Journal: :زمین شناسی اقتصادی 0
علی عابدینی رحیم معصومی علی اصغر کلاگری

kajal kaolin deposit is located ~20 km northwest of hashtjin, ardebil province. field evidence and laboratory investigations show that the deposit is an alteration product of ignimbrites, tuffs, and trachy-andesites of eocene age. according to mineralogical data, the major rock-forming minerals include kaolinite, montmorillonite, polygorskite, orthoclase, zeolite (stilbite), quartz, and chalced...

2011
Ellery D. Ingall Jay A. Brandes Julia M. Diaz Martin D. de Jonge David Paterson Ian McNulty W. Crawford Elliott Paul Northrup

Phosphorus K-edge X-ray absorption near-edge structure (XANES) spectroscopy was performed on phosphate mineral specimens including (a) twelve specimens from the apatite group covering a range of compositional variation and crystallinity; (b) six non-apatite calcium-rich phosphate minerals; (c) 15 aluminium-rich phosphate minerals; (d) ten phosphate minerals rich in either reduced iron or mangan...

Journal: :Applied Geochemistry 2021

Secondary minerals could be effective scavengers of toxic arsenic (As) and thallium (Tl). In environments polluted by mining, these elements are abundant both in acid rock/mine drainage scenarios, as well carbonate-buffered environments. this study we have investigated the behavior As Tl during weathering mine waste dumps an associated technosol sample from Crven Dol locality (Allchar Tl–As–Sb–...

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