Taikanite | |
---|---|
General | |
Category | Silicate mineral |
Formula (repeating unit) | Sr3BaMn2+2(Si4O12)O2 |
IMA symbol | Tka [1] |
Strunz classification | 9.DH.25 |
Crystal system | Monoclinic |
Identification | |
Color | Emerald green, blackish-green |
Fracture | Brittle - Conchoidal |
Mohs scale hardness | 6 to 7 |
Luster | Vitreous |
Density | 4.72 |
Other characteristics | IMA Status Approved (1984) |
References | [2] [3] |
Taikanite is a silicate mineral. It was named after the Taikan Range, Russia, its type locality.
Taikanite is a mineral with a color that ranges from emerald green to blackish-green. It crystallizes in the monoclinic system. It has a high relative density of 4.72. The mineral has a hardness of 6 to 7.
The type locality is the Taikan Range, in the Khabarovsk Krai, Russian Far East, where the mineral was discovered in a manganese deposit. It has also been found in Hotazel, Northern Cape province, South Africa.
Khabarovsk Krai is a federal subject of Russia. It is located in the Russian Far East and is administratively part of the Far Eastern Federal District. The administrative centre of the krai is the city of Khabarovsk, which is home to roughly half of the krai's population and the largest city in the Russian Far East. Khabarovsk Krai is the fourth-largest federal subject by area, and had a population of 1,343,869 as of 2010.
Fluororichterite is a rare amphibole with formula Na(NaCa)Mg5Si8O22F2.
Aurichalcite is a carbonate mineral, usually found as a secondary mineral in copper and zinc deposits. Its chemical formula is (Zn,Cu)5(CO3)2(OH)6. The zinc to copper ratio is about 5:4. Copper (Cu2+) gives aurichalcite its green-blue colors.
Uvarovite is a chromium-bearing garnet group species with the formula: Ca3Cr2(SiO4)3. It was discovered in 1832 by Germain Henri Hess who named it after Count Sergei Uvarov (1765–1855), a Russian statesman and amateur mineral collector. It is classified in the ugrandite group alongside the other calcium-bearing garnets andradite and grossular.
Euclase is a beryllium aluminium hydroxide silicate mineral (BeAlSiO4(OH)). It crystallizes in the monoclinic crystal system and is typically massive to fibrous as well as in slender prismatic crystals. It is related to beryl (Be3Al2Si6O18) and other beryllium minerals. It is a product of the decomposition of beryl in pegmatites.
Cotunnite is the natural mineral form of lead(II) chloride (PbCl2). Unlike the pure compound, which is white, cotunnite can be white, yellow, or green. The density of mineral samples spans range 5.3–5.8 g/cm3. The hardness on the Mohs scale is 1.5–2. The crystal structure is orthorhombic dipyramidal and the point group is 2/m 2/m 2/m. Each Pb has a coordination number of 9. Cotunnite occurs near volcanoes: Vesuvius, Italy; Tarapacá, Chile; and Tolbachik, Russia.
Aenigmatite, also known as cossyrite after Cossyra, the ancient name of Pantelleria, is a sodium, iron, titanium inosilicate mineral. The chemical formula is Na2Fe2+5TiSi6O20 and its structure consists of single tetrahedral chains with a repeat unit of four and complex side branches. It forms brown to black triclinic lamellar crystals. It has Mohs hardness of 5.5 to 6 and specific gravity of 3.74 to 3.85. Aenigmatite forms a solid-solution series with wilkinsonite, Na2Fe2+4Fe3+2Si6O20.
Ayano-Maysky District is an administrative and municipal district (raion), one of the seventeen in Khabarovsk Krai, Russia. It is located in the north of the krai. The area of the district is 167,200 square kilometers (64,600 sq mi). Its administrative center is the rural locality of Ayan. Population: 2,292 (2010 Russian census); 3,271 (2002 Census); 4,802 (1989 Soviet census). The population of Ayan accounts for 42.2% of the district's total population.
Aheylite is a rare phosphate mineral with formula (Fe2+Zn)Al6[(OH)4|(PO4)2]2·4(H2O). It occurs as pale blue to pale green triclinic crystal masses. Aheylite was made the newest member of the turquoise group in 1984 by International Mineralogical Association Commission on New Minerals and Mineral Names.
Aliettite is a complex phyllosilicate mineral of the smectite group with a formula of (Ca0.2Mg6(Si,Al)8O20(OH)4·4H2O) or [Mg3Si4O10(OH)2](Ca0.5,Na)0.33(Al,Mg,Fe2+)2−3(Si,Al)4O10(OH)2·n(H2O).
Chumikan is a rural locality and the administrative center of Tuguro-Chumikansky District of Khabarovsk Krai, Russia, located at the mouth of the Uda River. Population: 1,344 (2002 Census); 1,748 (1989 Soviet census).
Patrónite is the vanadium sulfide mineral with formula VS4. The material is usually described as V4+(S22−)2. Structurally, it is a "linear-chain" compound with alternating bonding and nonbonding contacts between the vanadium centers. The vanadium is octa-coordinated, which is an uncommon geometry for this metal.
Népouite is a rare nickel silicate mineral which has the apple green color typical of such compounds. It was named by the French mining engineer Edouard Glasser in 1907 after the place where it was first described, the Népoui Mine, Népoui, Poya Commune, North Province, New Caledonia. The ideal formula is Ni3(Si2O5)(OH)4, but most specimens contain some magnesium, and (Ni,Mg)3(Si2O5)(OH)4 is more realistic. There is a similar mineral called lizardite in which all of the nickel is replaced by magnesium, formula Mg3(Si2O5)(OH)4. These two minerals form a series; intermediate compositions are possible, with varying proportions of nickel to magnesium.
Hsianghualite is a tectosilicate of lithium, calcium and beryllium, with fluorine, a member of the zeolite group. It was discovered in 1958 and named for the type locality, Hsiang Hua, 香花, meaning fragrant flower.
Tuguro-Chumikansky District is an administrative and municipal district (raion), one of the seventeen in Khabarovsk Krai, Russia. It is located in the center of the krai. The area of the district is 96,069 square kilometers (37,092 sq mi). Its administrative center is the rural locality of Chumikan. Population: 2,255 (2010 Russian census); 2,860 (2002 Census); 3,610 (1989 Soviet census). The population of Chumikan accounts for 47.0% of the district's total population.
Fluorellestadite is a rare nesosilicate of calcium, with sulfate and fluorine, with the chemical formula Ca10(SiO4)3(SO4)3F2. It is a member of the apatite group, and forms a series with hydroxylellestadite.
Marshite (CuI) is a naturally occurring isometric halide mineral with occasional silver (Ag) substitution for copper (Cu). Solid solution between the silver end-member miersite and the copper end-member marshite has been found in these minerals from deposits in Broken Hill, Australia. The mineral's name is derived from the person who first described it, an Australian mineral collector named Charles W. Marsh. Marsh drew attention to native copper iodide (Marshite) in the 1800s emphasizing its natural occurrence, it is not to be confused with copper (I) iodide a substance commonly synthesized in laboratory settings.
Bilibinskite is an Au – Cu – Pb telluride. It is a rare mineral that was named after Soviet geologist Yuri Bilibin (1901–1952), who researched the geology of gold deposits during the time of the USSR.
The Taikan Range is a mountain range in Khabarovsk Krai, Russian Far East. The closest inhabited place is Chumikan, Tuguro-Chumikansky District. The nearest airport is Chumikan Airport.
The Selemdzha Range is a range of mountains in the Russian Far East. Administratively it belongs partly to Amur Oblast and partly to the Khabarovsk Krai of the Russian Federation.