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Rudna Mine

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Journal Article
Published: 03 February 2016
Seismological Research Letters (2016) 87 (2A): 274–284.
...Łukasz Rudziński; Simone Cesca; Grzegorz Lizurek ABSTRACT On 19 March 2013, a strong, shallow, induced seismic event struck a mining panel in the room‐and‐pillar Rudna copper mine in southeastern Poland. The event caused important damage at the mining tunnel and trapped 19 miners, who were safely...
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Journal Article
Published: 08 March 2016
Bulletin of the Seismological Society of America (2016) 106 (2): 799–805.
... at the source, whereas the Love waves associated with a 2013 Rudna Mine collapse ( M w 4.2) are minimal except where amplified by a deep sedimentary basin. We examine the source of the 19 March 2013 Rudna Mine, Poland, collapse with a full moment tensor inversion method, using the complete waveforms of regional...
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The Rudna Mine region in northern Europe, showing the Quaternary alluvial basin and outcroppings of older rocks (Pawlewicz et al., 2002). Solid triangles are the five stations used with the western United States (WUS) velocity model validation for the 2004 earthquake and for the 2013 Rudna Mine event moment tensor inversion. Open triangles are basin stations employing the modified velocity model and used for the Love‐wave observations. Focal mechanisms are shown for the 2013 Rudna Mine collapse, the 2004 Poland earthquake (University of Utah Seismograph Stations [UUSS] solution in black, others in gray. Swiss Seismological Service [SSS], MedNet Regional CMT [MedNet], and Institute of Geophysics, Polish Academy of Sciences [IGF]). The inset shows the location of the larger map within Europe.The color version of this figure is available only in the electronic edition.
Published: 08 March 2016
Figure 1. The Rudna Mine region in northern Europe, showing the Quaternary alluvial basin and outcroppings of older rocks ( Pawlewicz et al. , 2002 ). Solid triangles are the five stations used with the western United States (WUS) velocity model validation for the 2004 earthquake
Journal Article
Journal: Economic Geology
Published: 01 December 1995
Economic Geology (1995) 90 (8): 2143–2155.
...D. J. Large; J. MacQuaker; D. J. Vaughan; Z. Sawlowicz; A. P. Gize Abstract Minerals of the Cu-Fe-S system from the Lubin and Rudna mines in the Polish Kupferschiefer display textures and compositional trends consistent with copper depletion. The compositions, optical properties, textures...
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Source‐type plot (Tape and Tape, 2013): circles, Utah earthquakes, deviatoric moment tensor solution (Whidden and Pankow, 2012); diamonds, same Utah earthquakes, full moment tensor solutions; black square, Crandall Canyon Mine collapse; gray squares, other Utah mine events; dark star, 2004 Poland earthquake, deviatoric moment tensor solution; stars show the 2004 earthquake and Rudna collapse studied in this article. The Rudna Mine event plots near other known mine collapses.The color version of this figure is available only in the electronic edition.
Published: 08 March 2016
star, 2004 Poland earthquake, deviatoric moment tensor solution; stars show the 2004 earthquake and Rudna collapse studied in this article. The Rudna Mine event plots near other known mine collapses.The color version of this figure is available only in the electronic edition.
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(a) Moment tensor solutions and surface‐wave radiation patterns for the 2013 Rudna Mine and (b) the 2007 Crandall Canyon Mine collapses. Solid waveforms are data, and dashed waveforms are WUS synthetics. The Rudna solution includes only the top five stations and is our preferred solution. Four alluvial stations are not a part of the preferred moment tensor solution, but they are shown below the dashed line in gray for reference. For the moment tensor solution including these alluvial stations, see  Figure S3 available in the electronic supplement to this article. Both Rudna and Crandall solutions have good fits, large isotropic components, and very small double‐couple (DC) components. Rudna is more isotropically dominated at 61% versus 52% for Crandall Canyon. Radiation patterns are constructed using the largest absolute amplitude on the tangential and vertical components for 10–20 s band‐passed data (thick lines) and synthetic (thin lines) waveforms. Crandall synthetics and southern Rudna synthetics are calculated with WUS; the northern, larger Rudna synthetic radiation pattern amplitudes are calculated with WUS basin. The predicted Rudna tangential‐component (Love‐wave) amplitudes using the WUS model match the data from the five stations located on rock fairly well. Crandall Canyon Love‐wave amplitudes are well matched by the synthetics for the majority of stations.The color version of this figure is available only in the electronic edition.
Published: 08 March 2016
Figure 2. (a) Moment tensor solutions and surface‐wave radiation patterns for the 2013 Rudna Mine and (b) the 2007 Crandall Canyon Mine collapses. Solid waveforms are data, and dashed waveforms are WUS synthetics. The Rudna solution includes only the top five stations and is our preferred
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(a) Moment tensor solutions and surface‐wave radiation patterns for the 2013 Rudna Mine and (b) the 2007 Crandall Canyon Mine collapses. Solid waveforms are data, and dashed waveforms are WUS synthetics. The Rudna solution includes only the top five stations and is our preferred solution. Four alluvial stations are not a part of the preferred moment tensor solution, but they are shown below the dashed line in gray for reference. For the moment tensor solution including these alluvial stations, see  Figure S3 available in the electronic supplement to this article. Both Rudna and Crandall solutions have good fits, large isotropic components, and very small double‐couple (DC) components. Rudna is more isotropically dominated at 61% versus 52% for Crandall Canyon. Radiation patterns are constructed using the largest absolute amplitude on the tangential and vertical components for 10–20 s band‐passed data (thick lines) and synthetic (thin lines) waveforms. Crandall synthetics and southern Rudna synthetics are calculated with WUS; the northern, larger Rudna synthetic radiation pattern amplitudes are calculated with WUS basin. The predicted Rudna tangential‐component (Love‐wave) amplitudes using the WUS model match the data from the five stations located on rock fairly well. Crandall Canyon Love‐wave amplitudes are well matched by the synthetics for the majority of stations.The color version of this figure is available only in the electronic edition.
Published: 08 March 2016
Figure 2. (a) Moment tensor solutions and surface‐wave radiation patterns for the 2013 Rudna Mine and (b) the 2007 Crandall Canyon Mine collapses. Solid waveforms are data, and dashed waveforms are WUS synthetics. The Rudna solution includes only the top five stations and is our preferred
Book Chapter

Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2012
EISBN: 9781629490410
.... Image: Manuela Frotzscher. B. Chalcocite veins in uppermost part of Weissliegend sandstone, Rudna mine. C. Massive chalcocite impregnating Weissliegend sandstone, Rudna mine. D. Massive chalcocite impregnation crosscutting Weissliegend sandstone, Rudna mine. E. Photomicrograph of chalcocite (light gray...
Journal Article
Published: 03 March 2021
Seismological Research Letters (2021) 92 (3): 1717–1725.
... the mining‐induced seismic events from Rudna mine in Legnica–Głogów Copper District (LGCD) in the southwest of Poland. The copper ore in the LGCD area is excavated in three deep (up to 1.5 km depth) mines: Rudna, Polkowice–Sieroszowice, and Lubin. The mining activities are carried out in stiff and rigid...
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The dependence between seismic moment and corner frequency for the JAGUARS data (small dark points) in comparison with data from other studies in the low-magnitude range. The Madariaga (1976) source model is assumed to calculate source radii and the lines of constant static stress drop (Vβ=3500 m/s). The data other than the JAGUARS data originate from Pyhäsalmi mine (Oye et al., 2005), Strathcona mine (Urbancic and Young, 1993; Urbancic et al., 1996), the Underground Research Laboratory (Gibowicz et al., 1991; Collins and Young, 2000), Rudna Copper Mine (Domański and Gibowicz, 2008), the G. Kwiatek section G-7/5 of Rudna copper mine (unpublished data; Orlecka-Sikora et al., 2009), California (Ide et al., 2003; Abercrombie and Rice, 2005), Gross Schönebeck Geothermal Laboratory (Kwiatek, Bohnhoff, et al., 2010), Berlín Geothermal Field (Kwiatek and Bulut, 2011), and South African gold mines (McGarr, 1994; Richardson et al., 2005; Yamada et al., 2007). The arrow marks the apparent depletion in the number of events that resulted from the SR method selection procedure (detailed discussion in the text). The color version of this figure is available only in the electronic edition.
Published: 01 December 2011
drop ( V β =3500 m/s). The data other than the JAGUARS data originate from Pyhäsalmi mine ( Oye et al. , 2005 ), Strathcona mine ( Urbancic and Young, 1993 ; Urbancic et al. , 1996 ), the Underground Research Laboratory ( Gibowicz et al. , 1991 ; Collins and Young, 2000 ), Rudna Copper Mine
Journal Article
Published: 30 May 2023
Geochemistry: Exploration, Environment, Analysis (2023) 23 (2): geochem2022-046.
... patterns were observed ( Nieć and Piestrzyński 2007 ). Mineralization may occur: In shales and sandstones. In this case Cu mineralization may occur only in the lower part of the shales, while in their upper part Pb and Zn predominate. It is a common pattern in the Lubin and Rudna mines...
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The dependence between seismic moment (moment magnitude) and radiated energy for different studies within the low-magnitude range (cf. Fig. 8). The lines of constant apparent stress σa are shown as dashed lines assuming shear modulus . Two datasets from Rudna copper mine (Orlecka-Sikora et al., 2009; G. Kwiatek, unpublished data) were removed because they do not incorporate S waves in calculations of radiated energy. The Underground Research Laboratory data of Collins and Young (2000)are not presented as well, as they are not corrected for the finite frequency band, as suggested by Ide and Beroza (2001). The color version of this figure is available only in the electronic edition.
Published: 01 December 2011
Figure 11. The dependence between seismic moment (moment magnitude) and radiated energy for different studies within the low-magnitude range (cf. Fig.  8 ). The lines of constant apparent stress σ a are shown as dashed lines assuming shear modulus . Two datasets from Rudna copper mine
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The dependence between seismic moment (moment magnitude) and radiated energy for different studies within the low-magnitude range (cf. Fig. 8). The lines of constant apparent stress σa are shown as dashed lines assuming shear modulus . Two datasets from Rudna copper mine (Orlecka-Sikora et al., 2009; G. Kwiatek, unpublished data) were removed because they do not incorporate S waves in calculations of radiated energy. The Underground Research Laboratory data of Collins and Young (2000)are not presented as well, as they are not corrected for the finite frequency band, as suggested by Ide and Beroza (2001). The color version of this figure is available only in the electronic edition.
Published: 01 December 2011
Figure 11. The dependence between seismic moment (moment magnitude) and radiated energy for different studies within the low-magnitude range (cf. Fig.  8 ). The lines of constant apparent stress σ a are shown as dashed lines assuming shear modulus . Two datasets from Rudna copper mine
Journal Article
Published: 01 December 2011
Bulletin of the Seismological Society of America (2011) 101 (6): 2592–2608.
... drop ( V β =3500 m/s). The data other than the JAGUARS data originate from Pyhäsalmi mine ( Oye et al. , 2005 ), Strathcona mine ( Urbancic and Young, 1993 ; Urbancic et al. , 1996 ), the Underground Research Laboratory ( Gibowicz et al. , 1991 ; Collins and Young, 2000 ), Rudna Copper Mine...
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Journal Article
Published: 20 October 2020
Bulletin of the Seismological Society of America (2021) 111 (1): 409–423.
... in Rudna mine, Poland ( Kozłowska and Orlecka‐Sikora, 2016 ; Rudziński et al. , 2016 ); and seismic activity in Canadian mines in Ontario (e.g., Vallejos and McKinnon, 2010 ). To ensure both safety and profitable continuation of mine exploitation following the mainshock, it is important to estimate...
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Journal Article
Published: 07 December 2016
Seismological Research Letters (2017) 88 (1): 13–22.
... 2013, Rudna Mine (Poland) induced seismic event and collapse in the light of local and regional moment tensor inversion , Seismol. Res. Lett. 87 , 274–284 . Stec K. ( 2007 ). Characteristics of seismic activity of the Upper Silesian Coal basin in Poland , Geophys. J. Int. 168...
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Journal Article
Published: 02 March 2018
Geochemistry: Exploration, Environment, Analysis (2018) 18 (2): 132–141.
... were further collected at different sites from the Polish Polkowice-Sieroszowice and Rudna mines. In addition, a flotation concentrate from the Lubin concentrator of KGHM (Poland) was included. Although this concentrate originates from a mixture of different mineralized lithotypes (Kupferschiefer...
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Journal Article
Published: 08 December 2023
Geochemistry: Exploration, Environment, Analysis (2023) 23 (4): geochem2023-035.
..., such as spinkopite, yarrowite and geerite, are the preferential Ag carriers in the Rudna and Lubin mining areas ( Fig. 9 ). These minerals have not yet been reported in ore horizons of the studied deposit. Silver content of the studied bornite is lower than in the Lubin–Sieroszowice mining district...
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Journal Article
Published: 01 May 2009
Bulletin of the Seismological Society of America (2009) 99 (2B): 1443–1448.
... period in the Rudna-Polkowice copper mine in Silesia, Poland. On 19 April, 17 hr 50 min 39 sec Central European time, a strong rockburst occurred at 51.47° N, 16.12° E, and 790 m below the Earth’s surface. The epicenter distance was 1.5 km with seismic energy of and . The seismogram...
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Journal Article
Published: 11 July 2018
Seismological Research Letters (2018) 89 (5): 1741–1749.
... . Rudzinski L. Cesca S. , and Lizurek G. 2016 . Complex rupture process of the 19 March 2013, Rudna Mine (Poland) induced seismic event and collapse in the light of local and regional moment tensor inversion , Seismol. Res. Lett. 87 , no.  2 , 11p . doi: 10.1785/0220150150...
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