ଆଲୁମିନିୟମ୍ କିମ୍ବା ଆଲୁମ୍ ଧାରଣ କିମ୍ବା ଧାରଣ କରେ |,

Adjective:

ଆଲୁମ-କାରଣ, ଆଲୁମିନା-କାରଣ,

aluminous's Usage Examples:

occurs in association with crandallite and variscite in fractures in aluminous metamorphic rock, in hydrothermal regions and in phosphate rock deposits.

known as pozzolanic ash (Latin: pulvis puteolanus), is a natural siliceous or siliceous-aluminous material which reacts with calcium hydroxide in the presence.

the minerals olivine, clinopyroxene, orthopyroxene, and an aluminous phase.

His account of the aluminous district of Tolfa and adjacent hills, published in 1786, gained for him.

phillipsite, and that an interaction with sea water actually causes crystalline aluminous tobermorite structures in the mortar to expand and strengthen, making.

Most mafic rocks are metaluminous, having neither excess aluminum nor alkalis.

3Na2O⋅3Al2O3⋅6SiO2⋅Na2SO4 4–40% Cancrinite Na3⋅CaAl3⋅Si3⋅O12CO3 0–20% Aluminous-goethite (aluminous iron oxide) α-(Fe,Al)OOH 10–30% Hematite (iron oxide) Fe2O3.

The aluminous phase is plagioclase in the uppermost mantle, then spinel, and.

of the Paramaca series, which corresponds to a series of micaschists, aluminous paragneisses and black quartzites whose total thickness is about 1 km.

percolated within the tiny cracks in the Roman concrete, it reacted with phillipsite naturally found in the volcanic rock and created aluminous tobermorite.

the iron-endmember annite, and the magnesium-endmember phlogopite; more aluminous end-members include siderophyllite and eastonite.

Examples of peraluminous minerals include biotite, muscovite, cordierite, andalusite and garnet.