scholarly journals Mineral Composition of Blood Sausages – A Two-Case Study

Food Industry ◽  
10.5772/53591 ◽  
2013 ◽  
Author(s):  
Daphne D. ◽  
Luz H. ◽  
Enrique A. ◽  
Irma Caro ◽  
Ana Fernandez-Diez ◽  
...  
Keyword(s):  

2021 ◽  
pp. 3-11
Author(s):  
B.N. Ivanov ◽  
◽  
N.A. Donskoy ◽  
V.O. Syomka ◽  
S.M. Bondarenko ◽  
...  

Paper research aim is to identify characteristics of spacious distribution of radioactive- and associated elements in albitites according to depth and ore-level attribution: case study of 35th survey line of Novokostiantynivka deposit. Geochemical characteristics of Novokostiantynivka deposit are defined by presence of upper and lower ore-bearing levels. Geochemical anomalies related to upper ore-bearing level have complex character (uranium, thorium, lanthanum, yttrium, ytterbium, vanadium, and zirconium). At apical part of the deposit (Eastern fault) the albitites of blended type (chlorite, rybekite, aegerine) are dominant. La, Th, Y, and U define geochemical trend. These elements are likely to be related to rare-earth mineralization (monazite, apatite, xenotime), to a lesser extent to thorium and uranium mineralization with subordinate zircon. At deeper levels (Western fault) albitites’ mineral composition becomes more monotonous of rybekite-aegerine, and aegerine. The lead elements are Zr, Y, V, U, Th; Zr and Y noticeably dominate over other elements. Both elements and, maybe, part of U are related to zircon (malacon) which is predominant over rare-earth and thorium mineralization. Geochemical anomalies related to lower ore-bearing level are distinctive with monometallic (uranium) trend. The albitites of large column-like body have rybekite-aegerine, or aegerine mineral composition; phlogopite occurs often. Associated elements like Th, La, Y, Yb, V, Zr specific to albitites of upper ore level are not characteristic to deeper one. Based on seldom minor Th, La, and Y content spikes, rare-earth and thorium mineralization is immaterial. Regarding Zr and V, their contents are not over but most of the time less than background values. Apparently, zircon is not formed in albitites of lower ore-level; vanadium content in darkcolored minerals becomes insignificant, and single lead element is uranium. The most essential feature of Novokostiantynivka deposit is a succession of complex mineralization with monometallic one with depth.



2019 ◽  
Vol 13 (4) ◽  
pp. 2529-2541 ◽  
Author(s):  
Saba Bhatti ◽  
Jameel Ahmed Baig ◽  
Tasneem Gul Kazi ◽  
Hassan Imran Afridi ◽  
Ashfaque Ahmed Pathan




2014 ◽  
Vol 67 (2) ◽  
pp. 127-136 ◽  
Author(s):  
Čedomir Benac ◽  
Maja Oštrić ◽  
Sanja Dugonjić Jovančević


2012 ◽  
Vol 496 ◽  
pp. 453-456 ◽  
Author(s):  
Si Qing Liu ◽  
Bao Liang Ge ◽  
Bao Xu Song ◽  
Wan Ping Wang

Tin resources are mainly distributed in Yunnan and Guangxi autonomous regions, China. Tin ores in these areas are characterized by polymetallic constituents, including copper, zinc, lead and other associated elements that can be recovered. Due to the complex mineral composition and texture of the ores, gravity concentration, flotation as well as some combined processing techniques used in some major concentrators are reviewed and discussed. Case study shows that the comprehensive utilization of the tin ores can be realized to produce some marketable products for smelters. But much work on recovery of the fine fractions of tin shall still be done to get a good processing performance for the resource sustainable development



Geofluids ◽  
2022 ◽  
Vol 2022 ◽  
pp. 1-17
Author(s):  
Zhaojing Song ◽  
Junqian Li ◽  
Xiaoyan Li ◽  
Ketong Chen ◽  
Chengyun Wang ◽  
...  

Analyzing the characteristics of rock brittleness in low-permeability mudstone and shale (MS) formations is imperative for efficient hydraulic fracturing stimulation. Rock brittleness depends on the mineral composition, organic matter abundance, and bedding structure. Based on the MS from Shahejie Formation mineral composition (clay mineral, felsic mineral, and calcareous mineral contents), total organic content, and bedding structure (laminated, laminar, and massive), six types of lithofacies were identified: clay-rich MS, felsic-rich MS, calcareous-rich MS, clay MS, felsic MS, and calcareous MS. The quartz, feldspar, calcite, and dolomite of the Shahejie Formation are brittle minerals. Consequently, lithofacies with high felsic and calcareous mineral contents are more brittle. In addition, laminated and laminar MS are also conducive to hydraulic fracturing. Therefore, laminated, organic-rich, and calcareous-rich MS are the dominant lithofacies for hydraulic fracturing in the Shahejie Formation. The lithofacies and brittleness index were predicted by the response characteristics between mineral compositions and logging curves. The 3521–3552 m section of well B11x is dominated by calcareous-rich MS with developed laminae, representing a favorable section for hydraulic fracturing. Fragile minerals and oil are widely developed in the lower part of the lower 1st member of the Shahejie Formation (Es1L) in the southwestern part of Zhaohuangzhuang-Suning, where hydraulic fracturing can be used to increase shale oil production.



Author(s):  
Сергей Анатольевич Светов ◽  
Александра Владимировна Степанова ◽  
Светлана Юрьевна Чаженгина ◽  
Евгения Николаевна Светова ◽  
Зоя Павловна Рыбникова ◽  
...  




CATENA ◽  
2014 ◽  
Vol 119 ◽  
pp. 166-173 ◽  
Author(s):  
Marek Drewnik ◽  
Michał Skiba ◽  
Wojciech Szymański ◽  
Marcin Żyła


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