1-20 OF 728 RESULTS FOR

Harz

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Series: Geological Society, London, Special Publications
Published: 22 April 2024
DOI: 10.1144/SP542-2023-52
EISBN: 9781786206398
... of the eastern Harz Mountains ( Fig. 3 ). Friedel et al. (2019) favour a pure tectonic origin for the mélanges. In our view, the mélanges contain both sedimentary and tectonic features and are classified here in terms of tectono-sedimentary mélanges. The Harzgerode Mélange Complex consists of an up to 1200 m...
FIGURES | View All (15)
Journal Article
Journal: Geophysics
Published: 12 April 2011
Geophysics (2011) 76 (3): B71–B77.
...Georg Kaufmann; Douchko Romanov; Ralf Nielbock Abstract Unicorn cave in the southern Harz Mountains of Germany is a show cave in dolomitic rocks of the Zechstein Formation. The cave's trunk passage is interrupted by larger rooms. The overburden is only around 15 m. The passages are filled...
FIGURES | View All (6)
Journal Article
Published: 01 March 2003
Journal of Paleontology (2003) 77 (2): 293–303.
...Eberhard Gischler; Michael R. Sandy; Jörn Peckmann Abstract A new genus Ibergirhynchia , a member of the rhynchonellide superfamily Dimerelloidea, is described for the species Terebratula contraria Roemer, 1850 , from Early Carboniferous deposits of the Harz Mountains, Germany. Ibergirhynchia...
FIGURES | View All (10)
Journal Article
Published: 01 April 2002
The Canadian Mineralogist (2002) 40 (2): 739–745.
...Christopher J. Stanley; Alan J. Criddle; Hans-Jürgen Förster; Andrew C. Roberts Abstract La tischendorfite, idéalement Pd 8 Hg 3 Se 9 , est une nouvelle espèce minérale provenant de Eskaborner Stollen (accès d’Eskeborn) à Tilkerode, montagnes Harz, en Allemagne. Elle se présente en...
FIGURES
Journal Article
Journal: Geology
Published: 01 May 2001
Geology (2001) 29 (5): 471.
FIGURES
Journal Article
Journal: Geology
Published: 01 March 2001
Geology (2001) 29 (3): 271–274.
...Jörn Peckmann; Eberhard Gischler; Wolfgang Oschmann; Joachim Reitner Abstract Early Carboniferous (latest Visean) seep deposits occur on top of the drowned Middle Devonian–Late Devonian Iberg atoll reef, Harz Mountains, Germany. These deposits include limestone with a low-diversity but high...
FIGURES | View All (5)
Journal Article
Journal: PALAIOS
Published: 01 April 1995
PALAIOS (1995) 10 (2): 180–189.
Journal Article
Published: 01 October 1992
European Journal of Mineralogy (1992) 4 (5): 1053–1068.
Journal Article
Journal: GSA Bulletin
Published: 01 May 1976
GSA Bulletin (1976) 87 (5): 830–831.
Journal Article
Journal: GSA Bulletin
Published: 01 May 1976
GSA Bulletin (1976) 87 (5): 831–832.
Journal Article
Journal: GSA Bulletin
Published: 01 January 1975
GSA Bulletin (1975) 86 (1): 77–82.
...TIMOTHY A. ANDERSON Abstract Rocks in the Harz Mountains probably accumulated during an episode of Carboniferous subduction. Oceanic crust moving relatively southeast was consumed at a Benioff zone dipping southeast. Pelagic and abyssal sediments, graywacke, basalt, keratophyre, and other rocks...
Journal Article
Published: 01 December 1963
Journal of Sedimentary Research (1963) 33 (4): 914–918.
...Hans Gerhard Huckenholz Abstract "Mineral, chemical, and textural compositions of classical graywackes from the Harz mountains (Germany) and of classical arkoses from the Auvergne (France) are discussed. The type graywackes cannot be defined by the presence of a matrix; nor does the presence...
Series: Miscellaneous Publications
Published: 01 January 1998
DOI: 10.32375/1998-MP45.13
EISBN: 9781732014862
Image
Compositional variations of amphibole in the chromitites, dunites, and harzburgites of the Lycian ophiolite. The gray squares and triangles in a–f represent interstitial amphibole (Rollinson 2008) and amphibole inclusions, respectively (Uysal et al. 2009; Borisova et al. 2012; Huang et al. 2017; Liu et al. 2017; Qiu et al. 2018; Xiong et al. 2018a; Wojtulek et al. 2019). The fields of intraplate amphibole (I-Amp) and suprasubduction amphibole (S-Amp) in mantle xenoliths are from Coltorti et al. (2007). The fields of hydrothermal Amp, Amp in the dunitic transition zone (DTZ), and Amp inclusion in chromite of the DTZ are from Rospabé et al. (2017). Data for amphibole in ophiolitic peridotite, shown in dotted line, are from Liu et al. (2010), Khedr et al. (2014), Çelik et al. (2018), and Slovenec and Šegvić. (2018). (Color online.)
Published: 01 February 2022
Figure 6. Compositional variations of amphibole in the chromitites, dunites, and harzburgites of the Lycian ophiolite. The gray squares and triangles in a–f represent interstitial amphibole ( Rollinson 2008 ) and amphibole inclusions, respectively ( Uysal et al. 2009 ; Borisova et al. 2012 ; H
Image
Photomicrograph of ultramafic rocks near the Tavreh listwaenite: (a) harzburgite, olivine shows a mesh texture due to serpentinization and chromite is seen as a minor mineral; (b) dunite, the microfractures in olivine grains have been filled by serpentine as a mesh structure; (c) serpentinized harzburgite with orthopyroxene and olivine grains remnants; (d) serpentinite. Abbreviations: Ol (olivine), Chr (chromite), Opx (orthopyroxene) and Sp (serpentine).
Published: 16 June 2020
Fig. 4. Photomicrograph of ultramafic rocks near the Tavreh listwaenite: ( a ) harzburgite, olivine shows a mesh texture due to serpentinization and chromite is seen as a minor mineral; ( b ) dunite, the microfractures in olivine grains have been filled by serpentine as a mesh structure; ( c ) ser
Image
Diabase quarry in the Harz Mountains, Hercynian Forest.
Published: 20 February 2020
Figure 1. Diabase quarry in the Harz Mountains, Hercynian Forest.
Image
(a) Mafic and ultramafic rocks and rhyolites from the Andes (basalts, harzburgite, lamprophyre, lherzolite, websterite and wehlerite) and the Superior Province (basalt, boninite, clinopyroxenite, dunite gabbro, komatiite, lamprophyre, peridotite, ferro-picrite, pyroxenite and wherlite) (Georoc database 2012) as well as banded-iron formation samples (Beukes & Klein 1990; Klein & Beukes 1993; Klein & Ladeira 2000, 2002) from various locales plotted on the IOCG alteration discrimination diagram. The figure shows that the vast majority of these samples are superimposed to the Ca-Fe alteration fields of the diagram. The alteration degree of these samples is unknown; (b) Samples of carbonaceous and metacarbonaceous rocks (limestones, calc-silicates, carbonate, dolomite, marble), carbonatites, potassic sedimentary and metasedimentary rocks (arenite, metaarkose), skarns and pegmatites plotted on the IOCG alteration diagram (National Geochemical Database of the U.S. Geological Survey 2008). The figure shows that the carbonaceous rocks, the carbonatites and the skarns are mostly superimposed to the Ca-Fe alteration fields, that the potassic sedimentary and metasedimentary rocks mostly overlap the K alteration field and the pegmatites overlap both the Na and K alteration fields. The alteration degree of these samples is unknown.
Published: 27 September 2013
Fig. 12. (a) Mafic and ultramafic rocks and rhyolites from the Andes (basalts, harzburgite, lamprophyre, lherzolite, websterite and wehlerite) and the Superior Province (basalt, boninite, clinopyroxenite, dunite gabbro, komatiite, lamprophyre, peridotite, ferro-picrite, pyroxenite and wherlite)
Image
Outcrop map of the Harz Mountains, the Subhercynian basin, and surrounding outcrop geology (after von Eynatten et al. 2008). The Teufelsmauer outcrop and the Heidelberg Formation are marked.
Published: 01 June 2012
F ig 1— Outcrop map of the Harz Mountains, the Subhercynian basin, and surrounding outcrop geology (after von Eynatten et al. 2008 ). The Teufelsmauer outcrop and the Heidelberg Formation are marked.
Image
(a) The Harz Mountains in northern Germany, with the working area around Unicorn cave marked. (b) Location of Unicorn cave (red) beneath the Brandköpfe ridge near the village of Scharzfeld. (c) Plan view of Unicorn cave (red), with the four gravimetric profiles shown on top. The profiles, labeled 1–4, start at the open circles. Profile 1 is also used for the ERI.
Published: 12 April 2011
Figure 1. (a) The Harz Mountains in northern Germany, with the working area around Unicorn cave marked. (b) Location of Unicorn cave (red) beneath the Brandköpfe ridge near the village of Scharzfeld. (c) Plan view of Unicorn cave (red), with the four gravimetric profiles shown on top
Image
Crustal-scale cross section from the Harz mountains to the Tornquist Zone, simplified after deep reflection seismic data interpreted in DEKORP BASIN Research Group (1999), Deeks and Thomas (1995), and Kockel (2003). Moderate dips and flattening at depth of the major faults suggest dominantly thrust/reverse kinematics of Late Cretaceous inversion. Cross section trace in Figure 1. AFT—Apatite fission track ages.
Published: 01 November 2008
Figure 2. Crustal-scale cross section from the Harz mountains to the Tornquist Zone, simplified after deep reflection seismic data interpreted in DEKORP BASIN Research Group (1999) , Deeks and Thomas (1995) , and Kockel (2003) . Moderate dips and flattening at depth of the major faults suggest