The Warren Township Anorthosite Project is an advanced specialty industrial minerals development opportunity located 100 km west of Timmins, Ontario in the Porcupine Mining Division. The project property consists of a 21 year, 673.7 ha renewable surface and mining rights Lease. The Lease is 100% owned by Avalon and is renewable for further terms.
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The chemical formula of pure anorthite is CaAl2Si2O8. Anorthite is found in mafic igneous rocks. Anorthite is rare on the Earth but abundant on the Moon. Most anorthosite in the western part of the Marcy massif is relatively massive, allowing Davis (1971) to map anorthosite in the St. Regis quadrangle by mafic mineral content. Crosby (1969) attempted to classify anorthosite by mineralogy by marking large areas on outcrops and counting enclosed mineral percentages, but found any simple classification difficult to map, as did Whitney and Olmsted Anorthosites also occur as inclusions in other igneous rocks ranging in composition from kimberlite to basalt to granite. Some can be demonstrated to be xenolithic, and represent fragments of other anorthosite types incorporated into ascending magmas.
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However, the point is actually anorthosite, which was much less useful for abrasives. A Deposit Model for Magmatic Iron-Titanium-Oxide Deposits Related to Proterozoic Massif Anorthosite Plutonic Suites. By Laurel G. Woodruff, Suzanne W. Nicholson, and David L. Fey AlSiCal-Towards a greener mineral and metal industry in Europe A new European project is funded by the EUs H2020 programme. The AlSiCal project aims at developing an innovative technology to reduce the environmental impact of producing alumina, silica and calcium carbonate by using alternative mineral resources.
This and many more mineral specimens are available for sale at Se hela listan på geologyforinvestors.com mixing models suggests that the anorthosite is exceedingly pure, containing >95vol% plagioclase in most areas and commonly ~99–100vol%.
A Deposit Model for Magmatic Iron-Titanium-Oxide Deposits Related to Proterozoic Massif Anorthosite Plutonic Suites. By Laurel G. Woodruff, Suzanne W. Nicholson, and David L. Fey
Some can be demonstrated to be xenolithic, and represent fragments of other anorthosite types incorporated into ascending magmas. Others, however, are cognate, and represent accumulations of plagioclase from their host magmas.
The rock type of Dushan jade belongs to zoisitized anorthosite. Anorthite, the major mineral of Philippines rock, belongs to the plagioclase isomorphous series. Diopside is the minor mineral with the highest content in Philippines rock and was altered by tremolitization.
Scanning electron micrograph of anorthite. Anorthite in Thin Section Thin Section GigaPans. Anorthite in plane polars Anorthite in crossed polars.
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- Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality.
Oxides, mostly magnetite or ilmenite, are also common. Anorthosite, type of intrusive igneous rock composed predominantly of calcium-rich plagioclase feldspar.
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The rock type of Dushan jade belongs to zoisitized anorthosite. Anorthite, the major mineral of Philippines rock, belongs to the plagioclase isomorphous series. Diopside is the minor mineral with the highest content in Philippines rock and was altered by tremolitization.
The term anorthosite, from Frenc anorthose (term for plagioclase) was coined by Sterry Hunt. The foliation pattern formed by mafic minerals on a structural map of the 3000 km 2 Adirondack anorthosite massif by Balk (1931) was interpreted to be a primary feature, suggesting the massif consists of one large intrusion bordered on the east by a few smaller intrusions (Buddington, 1939).
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mixing models suggests that the anorthosite is exceedingly pure, containing >95vol% plagioclase in most areas and commonly ~99–100vol%. These new data place important constraints on magma ocean crystallization scenarios, which must produce a zone of highly
2020-02-21 · Strictly speaking, the name “anorthosite” is applied to a rock composed of 90 to 100 of calcium-rich plagioclase feldspar and small amounts of high temperature minerals like pyroxene, olivine, magnetite (Fe3O4) or ilmenite (FeTiO3). The Majoqqap Qaava anorthosite deposit is located 125 km southeast of Greenland’s capital Nuuk on the southwest coast only 12 km from the ice-free coast of Qeqertarsuatsiaat Kangerdluat (Fiskenæs Fjord). The open pit mine will extract raw anorthosite, comprising the feldspar mineral Bytownite. Occurrences and Mineral Deposits. Strictly speaking, the name “anorthosite” is applied to a rock composed of 90 to 100 of calcium-rich plagioclase feldspar and small amounts of high temperature minerals like pyroxene, olivine, magnetite (Fe3O4) or ilmenite (FeTiO3).