نتایج جستجو برای: k2o and cao

تعداد نتایج: 16830800  

کریم‌پور, محمد حسن, ملک‌زاده شفارودی, آزاده ,

The Homond Cu-Au porphyry prospecting area is located southwest of Birjand. Subvolcanic monzonitic to dioritic rocks are highly altered. The main alteration zones are: quartz-sericite-calcite-pyrite, propylitic and carbonate. The content of major, trace and rare earth elements (REE) of the rocks changes due to alteration. The changes are less in some such as TiO2, MnO, P2O5, Nb, Gd, Y, Eu and h...

2016
Wenxiang Zhang Qingzhong Ming Zhengtao Shi Jie Niu Huai Su

Lacustrine deposits at the margin of the southeastern Tibetan Plateau (SETP) are sensitive indicators for the evolution of the southwest Asian monsoon (SWAM) during the Quaternary. Thus, they can provide insight into the Quaternary climatic history and their relationship with global climatic changes. The results of the geochemical analysis of the Xiaozhongdian Basin section at the SETP suggest ...

Journal: :Metallurgical and Materials Transactions B 2012

Journal: :Spectrochimica acta. Part A, Molecular and biomolecular spectroscopy 2011
Tirtha Som Basudeb Karmakar

An antimony oxide based monolithic glass with very high Sb2O3 content (70 mol%) in the system K2O-B2O3-Sb2O3 (KBS) has been prepared for the first time. Its phonon energy (602 cm(-1)), evaluated by infrared reflection spectroscopy, is found to be very close to that of fluoride glasses (500-600 cm(-1)). After doping with different rare-earth ions, their UV-vis absorption and photoluminescence pr...

Journal: :Acta Crystallographica Section A Foundations of Crystallography 2002

Forouzandeh, Seyed khalil, Hafezi Moghaddas, Hamid, Nasiri, Yaghoub, Taghdisi Nikbakht, Samira, Zarei Darmian, Mohammad amin, Zirjanizadeh, Sedigheh,

The Kuhkamar shale with a thickness of 354 m is composed of siliciclastic rocks (sandstone and shale). Petrography studies of the sandstones in this area show two petrofacies including arkose and sub-arkose. These sandstones composed of sub rounded to moderately sorted; therefore, compositionaly to texturaly, they are immature to submature with mono and polycrystalline quartz and k-feldespar. I...

2009
FABIO FERRI STEFANO POLI

Phase relationships in metapelites were experimentally investigated in the model system CaO^K2O^FeO^MgO^Al2O3^SiO2^H2O on four synthetic compositions differing in their K2O content and K2O/Al2O3 ratio. Experiments were carried out at pressures ranging from 0 8 to 1 4 GPa and temperatures from 620 to 7408C under different fluid-buffered conditions. The stability of the assemblage garnet^biotite^...

2010
J. A. Bryant G. M. Yogodzinski T. G. Churikova

Primitive arc magmatism and mantle wedge processes are investigated through a petrologic and geochemical study of high-Mg# (Mg/Mg ? Fe [ 0.65) basalts, basaltic andesites and andesites from the Kurile-Kamchatka subduction system. Primitive andesitic samples are from the Shisheisky Complex, a field of Quaternary-age, monogenetic cones located in the Aleutian–Kamchatka junction, north of Shiveluc...

2001
G. L. CLARKE N. R. DACZKO C. NOCKOLDS

Matlab scripts that apply the Bence & Albee (1968) matrix correction algorithm to X-ray intensity data collected as element maps on a Cameca SX-50 microprobe are used to produce two-dimensional maps of oxide weight percent and cation proportions for SiO2, Al2O3, FeO, MnO, MgO, CaO, Na2O and K2O. Once generated, large data sets of mapped oxide weight percent values or cation numbers that retain ...

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