Search results for "Mineral resource classification"

showing 5 items of 15 documents

Deformation and metamorphism at the base of the Helgeland nappe complex, northwest of Grong (Northern Norway)

1984

Pelites, carbonate-silicate rocks and mafic rocks occurring at the base of the Helgeland nappe complex northwest of Grong (N. Norway) were subjected together with the crystalline basement to medium grade metamorphism and threefold deformation during Caledonian times.

PeliteGeneral Earth and Planetary SciencesMetamorphismSedimentologyDeformation (meteorology)MaficPetrologyStructural geologyMineral resource classificationGeologyNappeGeologische Rundschau
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The Nahe Caldera — A resurgent Caldera in the permocarboniferous Saar Nahe basin, SW-Germany

1984

In the Saar Nahe basin, SW-Germany, a large resurgent caldera complex of Lower Permian age was recognized recently, for which the name „Nahe Caldera” is proposed.

PermianSaar–Nahe BasinGeochemistryGeneral Earth and Planetary SciencesCalderaSedimentologyStructural geologyMineral resource classificationGeomorphologyGeologyGeologische Rundschau
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Areal extent and first U-Pb age of the Pre-Damaran Abbabis complex in the central Damara belt of South West Africa (Namibia)

1978

The Proterozoic Abbabis Complex emerges from beneath the metasediments of the Late Precambrian Damara Supergroup within mantled gneiss domes and anticlinoria over a wide area in the central granite zone of the Pan African Damara belt. U-Pb dating of composite-, size-, and non-magnetic fractions of metamict zircons from two samples of Abbabis granite-gneiss from the farm Abbabis yielded a concordia intercept age of 1925 −280 +330 Ma. It is speculated that the Abbabis basement rocks are continuous under the Damaran metasedimentary cover and may link up with the Franzfontein basement inlier of similar age. This conclusion supports the ensialic character of the northeastern branch of the Damara…

PrecambrianBasement (geology)ProterozoicGeochemistryGeneral Earth and Planetary SciencesSedimentologyStructural geologyGeomorphologyMineral resource classificationGeologyGneissZirconGeologische Rundschau
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Mines and quarries production: A driver analysis of withdrawals in Italy

2020

Abstract The growing demand for non-energy mineral resources has determined relevant withdrawals as well as import-export flows. This paper aims to disentangle the drivers of raw non-energy mineral resources extraction in Italy. Using a new dataset of raw resources extracted from mines and quarries in the 21 Italian regions (19 regions and 2 autonomous provinces of Trento and Bolzano) for the period 2013–2016, our empirical analysis confirms the relevance of mining and quarrying producer price index as well as the manufacturing and construction sectors as main drivers. In line with the Hotelling (1931)'s theory, a positive relationship between m&q mineral resources extraction intensity and …

Producer price indexEconomics and EconometricsPluckingSociology and Political Science020209 energyNon-energy mineral resourceNon-renewable natural resource02 engineering and technologyMining and quarrying price index010501 environmental sciencesManagement Monitoring Policy and Law01 natural sciencesMineral resource classificationAgricultural economicsGeography0202 electrical engineering electronic engineering information engineeringHotelling's theoryPositive relationshipProduction (economics)Mining and quarrying mineralLawHotelling's theory Mining and quarrying minerals Mining and quarrying price index Non-energy mineral resources Non-renewable natural resources0105 earth and related environmental sciences
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The carbonates of the Permian Lakes of North Massif central, France

1992

During the Permian, large fluvio-lacustrine basins occurred within the West European Hercynian chain. The deposits were mainly detrital (conglomerates, sandstones and pelites). The two studied sites, Couy borehole and Aumance basin contain several dolomitic beds alternating with pelites containing Ostracods. The carbonate layers constitute various dolomitized facies with dolosparite, laminated and bituminous dolomites, oolites, oncolites and stromatolites, and pedological nodules. Microfacies are varied. The dolomite crystals can be either isolated rhombs scattered in pelites or rhombs and xenomorphic crystals cementing sandstones; in dolomicrites, dolomicrosparites and dolosparites, crysta…

geographygeography.geographical_feature_categoryPermianDolomiteMassifMineral resource classificationPaleontologychemistry.chemical_compoundchemistryGeochemistry and PetrologyFaciesPeliteCarbonateGeologyOncoliteCarbonates and Evaporites
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