alkali rock oor Spaans
alkali rock
Vertalings in die woordeboek Engels - Spaans
roca alcalina
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In addition, only Farallones's Monzodiorite has signs classified as tonalites and granodiorites The chemical composition of the intrusive bodies is similar to El Botón's Basalts. These belong to the shoshonitic group with a high concentration of alkali rocks (Na2O + K2O > 5 wt%), high proportions K2O/ Na2O (> 0,6 a los 50% wt de SiO2, >1,0 a los 55% wt de SiO2), low TiO2 (<1,3 % wt), high but changeable Al2O3 (14-19 %wt). Only few bodies such as San Juan's river diorite and small bodies of gabbro placed in Santa Cecilia-La Equis Complex have affinity with calco-alkaline's group.
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These rocks are composed of calcic to intermediate plagioclase, augite-egerine type clinopyroxene and biotite; olivine and flogopite may be present in some mafic rocks and alkali feldspar and quartz may be present in some felsic rocks.
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Lithospheric mantle below southeastern Spain: Evidence from mantle xenoliths in miocene-pliocene alkali rocks
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But, as many minerals develop in these "alkali" rocks that are uncommon elsewhere, it is convenient in a purely formal classification like that outlined here to treat the whole assemblage as a distinct series.
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QAPF diagrams are not used to classify pyroclastic rocks or volcanic rocks if modal mineralogical composition is not determined, instead the TAS classification (Total-Alkali-Silica) is used.
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One classification system compares the amount of alkali elements to the amount of silica on a graph; in this system, Gusev plains rocks lie near the junction of basalt, picrobasalt, and tephrite.
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As a result of the alkali attack, this rock shows a conspicuous chemical reaction (dedolomitization), producing calcite and brucite.
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It is often separated from the others as the "alkali" or "soda" rocks, and there is a corresponding series of mafic rocks.
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This process and combination of activity is highly unusual. The Oki basement gneisses contain evidence of their continental origin, and the extensive alkali volcanic rocks present here are extremely rare elsewhere in the Japanese arc.
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Fonolita.- Volcanic rock formed by alkali feldspar.
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The mineralogy consists of plagioclase (andesine) ± hornblende ± biotite ± alkali feldspar; to the southeast this body is in an intrusive contact with Gabro de Anserma generating a thin contact aureole, and the west presents a wide zone of mylonitic rocks associated with the Mistrató Fault.
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The SiO2 vs. alkalis diagram shows that most rocks are classified as basaltic andesite, andesite, dacite and rhyolite (53 - 78 wt.% of SiO2), following a calc-alkaline trend.
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Pumice is a rock of volcanic origin formulated with silicates of aluminum and alkali metals and used as an abrasive and a bulking agent.
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Pumice is a rock of volcanic origin formulated with silicates of aluminum and alkali metals and used as an abrasive and a bulking agent.
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Pumice is a rock of volcanic origin formulated with silicates of aluminum and alkali metals and used as an abrasive and a bulking agent.
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The diabases and basalts of the Complejo Quebradagrande unit are basic rocks with SiO2 values between 44.95% and 50.80%, high concentrations of MgO in the range between 8.9 and 5.42%, Fe2O3 varies between 14.83 and 7.98%, CaO contents are high between 7.55% and 13.2%, values of TiO2 in the majority of samples are between 1 and 2%, low ratio of alkalis vs SiO2 (0.03 to 0.10 wt %) and low K2O values between 0.07% and 0.47%.
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An important subdivision of these contains a very high percentage of alkalis, especially soda, and consequently has minerals such as nepheline and leucite not common in other rocks.
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In the case of chemical EOR, surfactants (S), alkalis (A) and polymers (P) are used to improve sweep efficiency and displacement in the oil, rock and water system.
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Alkali Flats is a structural basin, formed by a down-faulted crustal block overlain by younger volcanic rocks, of which some contain high lithium values and are considered to be the source of lithium found in subsurface brines in the Clayton Valley area.
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Chemically there exists a difference between the calc-alkaline plutonic rocks of the Cordillera de Talamanca and those of the Cordillera de Tilarán, specially with regard to the alkali content and the iron enrichment, which might be due to crustal thickening during the Upper Miocene.
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20 sinne gevind in 9 ms. Hulle kom uit baie bronne en word nie nagegaan nie.