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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Primary terms
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Asia
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Kamchatka Russian Federation
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Tolbachik (2)
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Canada
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carbon
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geochemistry (1)
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hydrology (1)
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igneous rocks
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Invertebrata (1)
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Ronneburg Mine
Polycrystallinity of green rust minerals and their synthetic analogs: Implications for particle formation and reactivity in complex systems
Ronneburgite, K 2 MnV 4 O 12 , a new mineral from Ronneburg, Thuringia, Germany: Description and crystal structure
NEW MINERALS
Does the bazhenovite structure really contain a thiosulfate group? A structural and spectroscopic study of a sample from the type locality
Starovaite, KCu 5 O(VO 4 ) 3 , a new mineral from fumarole sublimates of the Tolbachik volcano, Kamchatka, Russia
New minerals and nomenclature modifications approved in 2019
S,F,Cl-rich Mineral Assemblages from Burned Spoil Heaps in the Rosice-Oslavany Coalfield, Czech Republic
Organic Matter in Black Slate Shows Oxidative Degradation Within Only a Few Decades
Hydroxylellestadite from Cioclovina Cave (Romania): Microanalytical, structural, and vibrational spectroscopy data
Modeling Multiphase Reactive Transport in a Waste Rock Pile with Convective Oxygen Supply All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher.
EARLY OLIGOCENE RIPARIAN AND SWAMP FORESTS WITH A MASS OCCURRENCE OF ZINGIBEROIDEOPHYLLUM (EXTINCT ZINGIBERALES) FROM SAXONY, CENTRAL GERMANY
The Pristiograptus dubius (Suess, 1851) species group and iterative evolution in the Mid- and Late Silurian
Geochemical behaviour and mineralogical transformations during spontaneous combustion of a coal waste pile in Oslavany, Czech Republic
On the mineralogy of the “Anthropocene Epoch”
Dokuchaevite, Cu 8 O 2 (VO 4 ) 3 Cl 3 , a new mineral with remarkably diverse Cu 2+ mixed-ligand coordination environments
ENCYCLOPEDIA OF MINERAL NAMES: THIRD UPDATE
Lateral Subsurface Flow in a Soil Cover over Waste Rock in a Humid Temperate Environment All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher.
Redox-controlled selenide mineralization in the Upper Old Red Sandstone
SEG Newsletter 57 (April)
Fossil fuels, ore and industrial minerals
Abstract The mining of metallic and non-metallic commodities in Central Europe has a history of more than 2000 years. Today mainly non-metallic commodities, fossil fuels and construction raw materials play a vital role for the people living in Central Europe. Construction raw materials, albeit the most significant raw material, are not considered further here; for details refer to thematic maps issued by local geological surveys and comprehensive studies such as the textbook by Prentice (1990) . Even if many deposits in Central Europe, especially metallic deposits, are no longer extensive by world standards, the huge number and variety of deposits in Central Europe is unique and allows the student of metallogenesis to reconstruct the geological history of Central Europe from the Late Precambrian to the Recent in a way best described as ‘minerostratigraphy’. The term ‘deposit’ is used in this review for sites which were either mined in the twentieth century or are still being operated. A few sites that underwent exploration or trial mining have also been included in order to clarify certain concentration processes. They are mentioned explicitly in the text to avoid confusion with real deposits. Tonnage and grade are reported in the text only for the most important deposits. Production data for the year 2005 are listed in Table 21.1 for the countries under consideration. Reserves and production data of hydrocarbons in Central European basins are given in Table 21.2 . In the present study, Central Europe covers the Variscan core zones in the extra-Alpine part of Central Europe stretching from eastern France (Massif Central) into Poland where the contact between the Variscan Orogen and the Baltic Shield is concealed by a thick pile of platform sediments. In a north-south direction, Central Europe stretches from central Denmark to the southern boundary of the Po Plain in Italy, making the entire Variscan Foreland Basin, the Alpine Mountain Range, the Western Carpathians and the North Dinarides part of the study area. An outline of the geological and geographical settings is shown in Figure 21.1 . The precise geographical position of mineral sites, wells of special interest, hydrocarbon provinces, oil shale deposits and coal fields may be deduced from Tables 21.3 to 21.11 and the map ‘Mineral and energy resources of Central Europe’, at a scale 1:2 500 000 (see CD inside back cover).