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Littérature scientifique sur le sujet « Metodi multiminerali »
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Articles de revues sur le sujet "Metodi multiminerali"
Handari, Murgi. « Pengaruh Multiple Micronutrient Powder Terhadap Kejadian Infeksi Saluran Pernapasan Akut Pada Anak Usia 6-59 Bulan Dengan Anemia ». Jurnal Keperawatan Respati Yogyakarta 6, no 2 (25 mai 2019) : 592. http://dx.doi.org/10.35842/jkry.v6i2.303.
Texte intégralFanani, Anhar Faisal, Nurul Fajrih et Wa Laili Salido. « Penggunaan Minyak Ikan dalam Ransum Ayam Kampung terhadap Profil Lemak Darah ». Jurnal Ilmu dan Teknologi Peternakan Tropis 6, no 1 (7 février 2019) : 14. http://dx.doi.org/10.33772/jitro.v6i1.5572.
Texte intégralKurniasari, Yulinda, Siti Madanijah et Mira Dewi. « Multiple micronutrients supplementation (sprinkles) increased energy and nutrient intake of children aged 1-3 years ». Jurnal Gizi dan Dietetik Indonesia (Indonesian Journal of Nutrition and Dietetics) 6, no 1 (10 janvier 2019) : 7. http://dx.doi.org/10.21927/ijnd.2018.6(1).7-13.
Texte intégralManullang, Dini Hilary, I. Wayan Sudira, I. Ketut Berata et I. Made Merdana. « Ekstrak Etanol Sarang Semut Menyebabkan Kerusakan Struktur Histologi Ginjal Mencit ». Buletin Veteriner Udayana, 27 août 2018, 183. http://dx.doi.org/10.24843/bulvet.2018.v10.i02.p12.
Texte intégralThèses sur le sujet "Metodi multiminerali"
LIANG, WENDONG. « Petrology and multimineral fingerprinting of modern sand derived from the Himalayan orogen ». Doctoral thesis, Università degli Studi di Milano-Bicocca, 2020. http://hdl.handle.net/10281/271022.
Texte intégralSediments and sedimentary rocks can be considered as geological archives that faithfully reflect their provenance information if the bias introduced by physical and chemical processes during transport and deposition can be properly recognized and corrected for. The sediment provenance analysis both in modern and ancient settings is crucial to trace the sediment sources, reconstruct paleoclimate and paleoenvironment, and interpret the evolution of the Earth’s surface. Modern sediments, unaffected by diagenesis and eroded, tansported and deposited under climatic conditions that are fully known, can provide valuable information on the interactions among the different controlling factors that govern source-to-sink systems. Rivers draining the Himalayan orogen provide the good opportunity to trace the source fingerprinting that is documented in modern fluvial and eolian sand and how these signatures reflect the erosion patterns of the modern and paleo-river systems. A multidisciplinary approach based on petrography, minerology, geochemistry and geochronology is emphasized in this research, in order to obtain a comprehensive provenance information. Our research area focused on the modern sands from two river system: Yarlung River and Indus River. In the Yarlung River system, the Nian River was chosen to investigate the petrographic, mineralogical and chronological signature of sediments from Tethys Himalaya, Greater Himalaya, Kangmar gneiss dome and Transhimalayan ophiolitic suture. Different tectonic domains are characterized by distinct heavy mineral assemblages, e.g., the first-cycle sillimanite and garnet in Greater Himalaya, and clinopyroxene, olivine and enstatite in the forearc ophiolites. Sand carried by the Nian River and its major tributaries, mainly reflects Tethys Himalayan characteristics, consistent with the geochronological results. Erosion rates were also evaluated and circumscribed in the middle Yarlung River catchment. The average erosion rate in the Nianchu catchment is estimated at 0.07-0.10 mm/a, twice as that in the middle Yarlung and Lhasa River catchments, which is principally ascribed to the high erodibility of Tethys Himalayan strata. In the Indus River system, minerochemical analysis of amphibole, garnet, epidote and pyroxene grains, and geochronological analysis of detrital zircons, associated with analysis on petrography, bulk-sediment geochemistry and isotopic geochemistry, in aolian sand from Thal Desert and fluvial sand in selected tributaries draining one specific tectonic domain in the upper Indus catchment, were carried out to discriminate compositional signatures, decipher the provenance information, and trace the erosional evolution of the western Himalaya syntaxis. The compositional fingerprints of Thal Desert sand are characterized by litho-feldspatho-quartzose to quartzo-feldspatho-lithic detrital modes and very rich amphibole-dominated heavy-mineral assemblages. The high heavy mineral concentration, less negative εNd, abundant zircon ages at 40-100 Ma, and specific mineral varietal fingerprints, consistently reflect that the Kohistan arc has acted as the main sediment source. Karakorum appears to contribute less while Himalaya shows higher influence on the Thal Desert sands than modern river sands from the Indus. As a Quaternary repository of wind-reworked Indus River sand at the entry point in the Himalayan foreland basin, Thal Desert sands document higher erosion rates than today in the glaciated areas formed largely by batholites granitoids of the Asian active margin. The close compositional and chronological connection between the Thal Desert and the ancient Indus Delta and Fan deposits, shed new light on the reconstructing of paleodrainage and the understanding of relationship between climatic and tectonic forcing that controlled the erosional evolution of the western Himalayan-Karakorum orogen.
Actes de conférences sur le sujet "Metodi multiminerali"
Wang, S. S., L. Z. Xiao, A. Z. Yue et X. Li. « Multimineral non-linear inversion method using geochemical logging data based on Tikhonov regularization ». Dans 79th EAGE Conference and Exhibition 2017. Netherlands : EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701048.
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