Skip to main content

TANTALITE [(Fe, Mn)Ta2O6]

The mineral group tantalite [(Fe, Mn)Ta2O6] is the primary source of the chemical element tantalum. It is chemically similar to columbite, and the two are often grouped together as a semi-singular mineral called coltan or "columbite-tantalite" in many mineral guides.
Detailed Description:

 However, tantalite has a much greater specific gravity than columbite (8.0+ compared to columbite's 5.2).[2] Iron-rich tantalite is the mineral tantalite-(Fe) or ferrotantalite and manganese-rich is tantalite-(Mn) or manganotantalite.
Tantalite is also very close to tapiolite. Those minerals have same chemical composition, but different crystal symmetry orthorhombicfor tantalite and tetragonal for tapiolite.[3]

Tantalite is black to brown in both color and streak. Manganese-rich tantalites can be brown and translucent.

PRICE
$125/KG

For more information:

mobile: +2348039721941

contact person: emeaba uche

e-mail: emeabau@yahoo.com



Comments

Popular posts from this blog

BERYLLIUM ORE

A  divalent  element, beryllium is found naturally only combined with other elements in minerals. Notable gemstones which contain beryllium include  beryl  ( aquamarine ,  emerald ) and  chrysoberyl . The free element is a steel-gray, strong, lightweight brittle  alkaline earth metal . It is primarily used as a hardening agent in  alloys , notably  beryllium copper . Structurally, beryllium's very low density (1.85 times that of water), high melting point (1287 °C), high temperature stability and low coefficient of thermal expansion, make it in many ways an ideal aerospace material, and it has been used in rocket nozzles and is a significant component of planned space telescopes. Detailed description Because of its relatively high transparency to X-rays and other  ionizing radiation  types, beryllium also has a number of uses as filters and windows for radiation and particle physics experiments. Commercial use of beryllium m...

SPODUMENE [LiAl(SiO3)2]

Spodumene   is a   pyroxene   mineral   consisting of   lithium   aluminium   inosilicate ,   Li Al ( Si O 3 ) 2 , and is a source of lithium. It occurs as colorless to yellowish, purplish, or lilac kunzite (see below), yellowish-green or emerald-green   hiddenite , prismatic crystals, often of great size.   Detailed d Single crystals of 14.3 m (47 ft) in size are reported from the   Black Hills   of   South Dakota ,   United States . [5] [6] The normal low-temperature form α-spodumene is in the   monoclinic   system whereas the high-temperature β-spodumene crystallizes in the   tetragonal   system. The normal α-spodumene converts to β-spodumene at temperatures above 900 °C. [4]   Crystals are typically heavily striated parallel to the principal axis. Crystal faces are often etched and pitted with triangular markings. Discovery and occurrence Spodumene was first des...

SELENIUM ORE

Selenium (pronounced /s ɨ ˈl ɛ niəm/ si-LEN-ee-əm or /s ɨ ˈliːniəm/ si-LEE-nee-əm ) is a chemical element with the atomic number 34, represented by the chemical symbol Se , an atomic mass of 78.96. It is a nonmetal , chemically related to sulfur and tellurium , and rarely occurs in its elemental state in nature. Detailed description Isolated selenium occurs in several different forms, the most stable of which is a dense purplish-gray semi-metal ( semiconductor ) form that is structurally a trigonal polymer chain. It conducts electricity better in the light than in the dark, and is used in photocells (see section Allotropes below). Selenium also exists in many non-conductive forms: a black glass -like allotrope, as well as several red crystalline forms built of eight-membered ring molecules, like its lighter cousin sulfur. Selenium is found in economic quantities in sulfide ores such as pyrite , partially replacing the sulfur in the ore matrix. Minerals that are s...