3 edition of Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara found in the catalog.
Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara
Per Adolf Geijer
Bibliography: p. 274-278.
|Statement||by Per Geijer.|
|Series||Scientific and practical researches in Lapland arranged by Luossavaara-Kiirunavaara Aktiebolag : Geology of the Kiirunavaara district ;, 2|
|LC Classifications||QE282 .G4|
|The Physical Object|
|Pagination||vii, 278 p. :|
|Number of Pages||278|
|LC Control Number||11013242|
GEIJER, P., Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara. (Scientific and practical researches in Lapland arranged by Luossavaara-Kiirunavaara Aktiebolag). Stockholm. — Rapport till Chefen för SGU rörande apatittillgångar inom . Scientific and practical researches in Lapland arranged by Luossavaara-Kiiruna-vaaraN Aktiebolag. Geology of the Kiruna district. 2. Igneous rocks and iron ores of Kiirunavaara, Luossavaara, and Tuolluvaara. By Per A. Geijer. Stock-holm, Size 10| x 7?, pp. viii. and Maps and lllustrations. Presented. Sweden?Norrland. Sjogren.
Ore body description The Kiirunavaara ore body, as well as the other magnetite-apatite ores in the region, were deposited during the Svecokarelian orogeny (Billström et al., ) in the range of – Ga (Cliff et al., ). The ore body is large, sheet-like and extends approximately 4km along strike. Igneous rock is one of the three main rock types, the others being sedimentary and metamorphic rock.. Igneous rocks are rocks formed from molten material is made liquid by the heat inside the Earth's mantle.. When magma comes out onto the surface of the Earth, it is called cools down to form rocks such as tuff and basalt. Intrusive rocks are made when the magma slowly cools.
Igneous rocks are classified on the basis of their composition and their texture. Magma, and the igneous rock it becomes, has a range of chemical example, basalt is a mafic lava flow rock which originates from melting of the upper mantle. The way that magma turns into a solid rock gives it a distinctive igneous texture. Kiruna is located in the north of Sweden, kilometres (90 mi) north of the Arctic circle. The city centre is built on the Haukavaara hill at an altitude of m, high above the Torne river to the north and the Kalix river to the south. Other parts of the town are Lombolo and Tuolluvaara. Near Kiruna are the mountains Kiirunavaara and Luossavaara. Kiirunavaara is an iron ore mine that is the town's Country: Sweden.
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Excerpt from Igneous Rocks and Iron Ores of Kiirunavaara, Luossavaara and Tuolluvaara The region examined by the writer comprises the two ore mountains Km runavaara and Luossavaara and the continuation towards the sides and north ward of the igneous rocks forming their slopes, further on, the ore mountain Tuolluvaara and some exposures located chieﬂy north of the latter and con sisting of rocks more or less closely related to the ore-bearing Author: Per Geijer.
IGNEOUS ROCKS AND IRON ORES OF KIIRUNA-VAARA, LUOSSAVAARA AND TUOLLUVAARA Paperback – January 1, by Per Geijer (Author) See all formats and editions Hide other formats and editions. Price New from Used from Pamphlet Author: Per Geijer. Additional Physical Format: Online version: Geijer, Per Adolf, Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara.
Stockholm: P.A. Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara by Geijer, Per Adolf, Publication date Topics Rocks, Igneous, Petrology -- Lapland, Iron ores -- Lapland Publisher Stockholm: P.A.
Norstedt Collection cdl; americanaPages: The Tuolluvaara deposit is situated in rhyo-dacitic rocks 6 km northeast of Kiirunavaara. The ore mainly has the character of a large ore breccia and the content of apatite is rather low. STOP 1—The Luossavaara Open Pit and View over Kiruna.
Download PDF: Sorry, we are unable to provide the full text but you may find it at the following location(s): (external link) http Author: Per Adolf Geijer. Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara.
Scientific and Practical Researches in Lapland Arranged by Luossavaara^Kiirunavaara Aktiebolag,Cited by: Buy Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara [Hardcover] by Per Adolf, Geijer (ISBN:) from Amazon's Book Store.
Everyday low prices and free delivery on Author: Geijer, Per Adolf. I b. hOGBOM, The Gellivare Iron Mountain. PER GEIJER, Igneous Rocks and Iron Ores of Kiirunavaara, Luossavaara and Tuolluvara.
OTTO SJOGREN, Bidrag till Kirunaomradets Glacialgeologi. NILS SUNDIUS, Beitrage zur Geologie des sudlichen Teils des Kirunagebiets. REGINALD A. DALY, Origin of the Iron Ores at Kiruna.
bodies like Luossavaara or Tuolluvaara. They form irregular bulbous masses and have been termed as “ore breccias”. However, Kiruna is a concordant body, i.e. it is tabular and concordant with whose host rocks. The Kiruna ore is dominantly magnetite, although hematite has been indicated by drilling.
The ore contains circa 30 % apatite (mainlyFile Size: KB. Genesis of the Per Geijer apatite iron ores, Kiruna area, northern Sweden Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara.
Econ. Geol. 5, – Author: Olof Martinsson. Igneous Rock can be obtained by quarrying rocks on the Western Plateau. Usage Edit. Igneous Rock can be used for crafting Igneous Bricks or given as a neutral gift.
Craft Edit. Igneous Rock is a required ingredient when crafting the following item:From: Quarrying. An important argument for a magmatic affiliation of the Kiruna type of ore is the presence of ore breccia which accompany the main ore bodies.
According to Parák (a and b) the main ore bodies are not of the same origin as the breccias. This is based on data from the Luossavaara deposit in northern Sweden: the main ore and the breccia have different chemical by: Luossavaara-Kiirunavaara AB (LKAB) operates an iron ore mine, three concentration plants and three pelletising plants in Kiruna, Sweden.
The current methods of separation at the beneficiation plants are low intensity magnetic separation (LIMS) and reverse flotation (i. e., apatite is floated and magnetite depressed), where the wet LIMS stage is regarded as the crucial part of the Cited by: 1.
footwall of the Kiirunavaara iron ore, northernmost Sweden Lindgren, rocks of intermediate to acid composition (e.g. GeijerIgneous rocks and iron ores of Kiirunavaara, Luossavaara. Geijer, P. Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara.
Geologie des Kirunagebiets 2, pp. () Parak, T. Kiruna iron ores are not “intrusive-magmatic ores of Cited by: Ore deposits related to mafic igneous rocks • Range from largest, most extensive igneous petrologic systems in the world (e.g., Bushveld Complex) down to moderate-sized bodies like carbonatites.
• Magmatic segregation deposits: –formed in intrusive bodies –ore deposits formed during fractional crystallisation • Exceptions. Kiruna is the type area for apatite iron ores, and the Kiirunavaara deposit is the largest and best known example.
It contains more than 2, Mt of high-grade ore. Totally about 40 apatite iron ore deposits are known from northern Norrbotten (Fig. Individual deposits have an average content of Fe and P varying between 30 to 70 percent and. The Kiruna mine is the largest and most modern underground iron ore mine in the world.
The mine is located in Kiruna in Norrbotten County, Lapland, Sweden. The mine is owned by Luossavaara-Kiirunavaara AB (LKAB), a large Swedish mining company. In the mine produced million tonnes of iron ore.
The Kiruna mine has an ore body which is 4 km ( mi) long, 80 metres ( ft) Country: Sweden. Geijer, P. Geology o/ the Kiruna district, 2. Igneous rocks and i~'on ores o~ Kiirunavaara, Luos- ~avaara and Scientific and practical researches in Lapland arranged by Luossavaara- Kiirunavaara Aktiebolag, Stockholm.
Gerasimovsky, V. Geochemistry o] the llimaussaq Alkaline Massi/ (in Russian), Nauka, by:. ESKOLA PENTTI () Conditions during the earliest geological times Ann. Fennicae Ser. A36, No. 4. GEIJER PER () Igneous rocks and iron ores of Kiirunavaara, Luossavaara and Tuolluvaara Stockholm.
GEIJEB PEB () Some Swedish occurrences of bornite and chalcocite Sveriges Geol. Undersokn Ser. C, no. Cited by: 4.Ore Deposit Type: Epigenetic discordant irregular Rock Type: Mafic (intrusive or extrusive) Igneous Commodity Class: Copper, Vermiculite, Phosphate, Magnetite (Iron Ore), REE’s Tectonic Setting (formation): 3 Theories: Direct generation by very low degree partial melts in mantle - Liquid immiscibility between carbonate and silicate meltFile Size: KB.The apatite-iron-oxide ores of the Grängesberg Mining District (GMD) represents the largest iron ore accumulation in the classic Bergslagen ore province4, with a past production of Mt of ore, averaging 60% Fe and % by: