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  • 1
    Publication Date: 2023-07-10
    Keywords: Aluminium oxide; Barium; Caesium; Calcium oxide; Cerium; Chromium; DRILL; Drilling/drill rig; Dysprosium; E-Hang_Weinberg; Erbium; Europium; Event label; Gadolinium; Gauss-Krueger Hochwert; Gauss-Krueger Rechtswert; Gauss-Krueger Streifen; Gehege-Querschlag; Grube_Hühn; Hafnium; Holmium; Inductively coupled plasma - mass spectrometry (ICP-MS); Iron oxide, Fe2O3; Lanthanum; Latitude of event; Lead; Longitude of event; Loss on ignition; Lutetium; Magnesium oxide; Manganese oxide; Neodymium; Nickel; Niobium; OUTCROP; Outcrop sample; Phosphorus pentoxide; Potassium oxide; Praseodymium; Rock type; Rubidium; Samarium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; Strontium; Sum; Tantalum; Terbium; Thorium; Thulium; Thuringian Forest, Germany; Tiefer_Stollen; Titanium dioxide; Tsl_28/79; Tsl_3/77; Tsl_42/79; Tsl_66/79; Uranium; Vanadium; X-ray fluorescence (XRF); Ytterbium; Yttrium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 2632 data points
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Fresenius' Zeitschrift für analytische Chemie 224 (1967), S. 407-413 
    ISSN: 1618-2650
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Zusammenfassung Durch Zonenschmelzen konnte hochreiner Schwefel dargestellt werden, dessen Verunreinigungsgehalt (Kohlenstoff: weniger als 2,4 · 10−4%, Silicium 1,3 · 10−6%, Magnesium: 4,0 · 10−6%) wesentlich kleiner war als bei allen nach anderen Verfahren gereinigten Schwefelproben. Ein Verfahren zur Bestimmung von Silicium, Eisen und Magnesium in kleinen Schwefeleinwaagen durch Spektralanalyse ohne vorherige Anreicherung wurde ausgearbeitet.
    Notes: Summary High-purity sulphur was prepared by zone melting. The percentage of impurities (carbon 〈 2.4×10−4%, silicon 1.3×10−6%, magnesium 4.0×10−6%) was considerably smaller than in sulphur purified by other procedures. A method is described for the determination of silicon, iron and magnesium in sulphur samples by direct spectroscopic analysis without enrichment of the elements to be analysed.
    Type of Medium: Electronic Resource
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  • 3
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    In:  Geological Society Special Publication 223: 259-288.
    Publication Date: 2007-10-08
    Description: Permo-Carboniferous rifting in Europe was accompanied by the widespread emplacement of mantle-derived magmas forming regional dyke swarms and sills in northern England, Scotland, Norway and southern Sweden during the late Stephanian and early Autunian. The trends of the dyke swarms intersect at a focal point in the Kattegat south of the Oslo Graben, and are probably all related to a single magmatic centre that could be plume-related. The WNW- to NW-trending dyke swarm at the SW margin of the Fennoscandian Shield in southern Sweden is composed mainly of tholeiitic dolerites, with lesser amounts of alkaline mafic rocks (camptonites, alkali basalts and spessartites) and trachytes. The alkaline mafic rocks are enriched in Ba, Sr, Nb, P and CO2, implying a metasomatic enrichment of their upper-mantle source prior to melting. After generation of alkaline melts by relatively small degrees of partial melting, increased extension was accompanied by the formation of subalkaline tholeiitic magmas. Whole-rock compositions (Mg-numbers between 55 and 30) and mineral chemistry (olivine Fo60-Fo40; clinopyroxene approximately Wo30En45Fs15; plagioclase An70-An50) indicate relatively evolved melts that have undergone crystal fractionation of olivine and clinopyroxene. Two groups of dolerites can be distinguished on the basis of bivariate element plots, e.g. Zr-TiO2 and La-Sm. Although both groups show enrichment in the whole range of incompatible trace elements, slight differences in mantle-normalized trace-element patterns and different Nb/La ratios suggest that they were generated from two different sources. Group I dolerites were formed from a (re-)enriched, but isotopically mildly depleted, sublithospheric garnet-bearing mantle source (Nb/La mostly 〉0.9, {varepsilon}Ndi = +4 to +3, where {varepsilon}Ndi is the initial Nd isotope ratio), whereas group II dolerites seem to indicate mixing of the asthenospheric-derived magmas with lithospheric mantle melts (Nb/La mostly 〈0.9, {varepsilon}Ndi = 0 to -1). Increasing Th/Ta ratios together with decreasing U/Nb ratios from group I towards group II dolerites further reflect progressive crustal contamination.
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  • 4
    Publication Date: 2018-01-26
    Description: The Tornquist Fan, reflecting the northern part of the Trans-European Suture Zone, comprises a series of fault zones and major single faults, striking mainly subparallel to the SW margin of the Fennoscandian Shield. The deep-seated faults of Wiek, Nord Jasmund and Schaabe, which cross the northern part of Rügen Island and areas of the adjacent Baltic Sea from NW to SE, originated in the late Paleozoic. They are accompanied by younger faults, especially in the Pomeranian Bay, that were formed by Mesozoic tectonic processes. Based on reprocessed offshore seismic lines east of Rügen, a polyphase evolution for the Wiek Fault System is proposed. It implies changes in the stress field since the Caledonian Orogeny. Crustal extension in the Middle Devonian led to the formation of basins along the SW margin of Laurussia. Subsequent compressional movements, induced by the distant Variscan Orogeny, resulted in segmentation and block faulting of the Rügen Basin prior to the late Carboniferous. These Paleozoic faults were reactivated by Mesozoic extensional stress regimes. In addition, new en echelon faults were generated, contemporaneously with the formation of the Western Pomeranian Fault System. Since the Late Cretaceous (Africa–Iberia–Europe convergence), selected major normal faults have been reactivated as reverse faults.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 5
    Publication Date: 2018-03-12
    Description: Based on reprocessed offshore seismic lines acquired during oil and gas exploration in the 1980s, we reconstruct the formation and reactivation of major fault systems in the southern Baltic Sea area since the late Paleozoic. The geological evolution of different crustal blocks from the Caledonian Avalonia–Baltica collision until the Late Cretaceous–Paleogene inversion tectonics is also examined. The detected fault systems occur in the northern part of the Trans-European Suture Zone (TESZ) and belong either to the late Paleozoic Tornquist Fan or to the complex Western Pomeranian Fault System (WPFS) generated during Mesozoic extensional movements. While the NW–SE-trending deep Wiek Fault separates the Arkona High from the Middle Rügen Block, the NNW–SSE-trending Agricola Fault demarcates the Middle Rügen Block to the Falster Block in the west. Together with the Plantagenet Fault and numerous younger faults in the Mesozoic cover, it forms the Agricola Fault System. Furthermore, structural analyses of the Prerow Fault Zone above the Prerow salt pillow and the Werre Fault Zone crossing the Grimmen High indicate a complex fault history.
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 6
    Publication Date: 1967-09-01
    Print ISSN: 0016-1152
    Topics: Chemistry and Pharmacology
    Published by Springer
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  • 7
    Publication Date: 2004-01-01
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 8
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/conferenceObject
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  • 9
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-09-12
    Description: Northern Germany is a weak seismicity region with low level of exposure to seismic hazard. Accordingly, seismic hazard assessment has been pursued with low priority in the past. Rather poor observational conditions in the North German Basin are also a limiting factor for seismic monitoring. In a multi-institutional collaboration, we have been able to increase the number of permanent broadband stations in the North German Federal States of Schleswig-Holstein and Mecklenburg-Vorpommern from previously four in the year 2013 to currently fifteen. All data of the network are freely available through the EIDA node at the Federal Institute for Geosciences and Natural Resources (BGR) in Hannover. Three complementary seismic arrays, notably on the islands of Heligoland in the North Sea and on Rügen in the Baltic Sea, improve monitoring capabilities of offshore areas. Data from these seismic arrays also provide an opportunity to investigate properties of oceanic microseism in epicontinental seas. In addition to the development and operation of the seismic network, continuous event detection and analysis routines have been established at Kiel University. Besides low magnitude earthquakes, other natural phenomena like rockslides on cliffs or subrosion events have been repeatedly detected. Known controlled explosions provide an opportunity to quantify detection and location capabilities of the network. The recent destruction of the Nord Stream gas pipelines proved the importance of ongoing network expansion, and the need and reliability of routine seismic monitoring in this region.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
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