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Journal articles on the topic 'Frimurarbarnhuset i Kristineberg (Sweden)'

Author: Grafiati

Published: 4 June 2021

Last updated: 3 February 2022

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1

Dehghannejad, Mahdieh, Alireza Malehmir, Christopher Juhlin, and Pietari Skyttä. "3D constraints and finite-difference modeling of massive sulfide deposits: The Kristineberg seismic lines revisited, northern Sweden." GEOPHYSICS 77, no. 5 (September 1, 2012): WC69—WC79. http://dx.doi.org/10.1190/geo2011-0466.1.

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The Kristineberg mining area in the western part of the Skellefte ore district is the largest base metal producer in northern Sweden and currently the subject of extensive geophysical and geologic studies aimed at constructing 3D geologic models. Seismic reflection data form the backbone of the geologic modeling in the study area. A geologic cross section close to the Kristineberg mine was used to generate synthetic seismic data using acoustic and elastic finite-difference algorithms to provide further insight about the nature of reflections and processing challenges when attempting to image the steeply dipping structures within the study area. Synthetic data suggest processing artifacts manifested themselves in the final 2D images as steeply dipping events that could be confused with reflections. Fewer artifacts are observed when the data are processed using prestack time migration. Prestack time migration also was performed on high-resolution seismic data recently collected near the Kristineberg mine and helped to image a high-amplitude, gently dipping reflection occurring stratigraphically above the extension of the deepest Kristineberg deposit. Swath 3D processing was applied to two crossing seismic lines, west of the Kristineberg mine, to provide information on the 3D geometry of an apparently flat-lying reflection observed in both of the profiles. The processing indicated that the reflection dips about 30° to the southwest and is generated at the contact between metasedimentary and metavolcanic rocks, the upper part of the latter unit being the most typical stratigraphic level for the massive sulfide deposits in the Skellefte district.

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2

Skyttä, P., T. Bauer, T. Hermansson, M. Dehghannejad, C. Juhlin, M. García Juanatey, J. Hübert, and P. Weihed. "Crustal 3-D geometry of the Kristineberg area (Sweden) with implications on VMS deposits." Solid Earth 4, no. 2 (October 31, 2013): 387–404. http://dx.doi.org/10.5194/se-4-387-2013.

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Abstract. Structural analysis of the Palaeoproterozoic volcanogenic massive sulfide (VMS) hosting Kristineberg area, Sweden, constrained by existing magnetotelluric (MT) and seismic reflection data, reveals that the complex geometry characterized by non-cylindrical antiformal structures is due to transpression along the termination of a major high-strain zone. Similar orientations of the host rock deformation fabrics and the VMS ore lenses indicate that the present-day geometry of the complex VMS deposits in the Kristineberg area may be attributed to tectonic transposition. The tectonic transposition was dominantly controlled by reverse shearing and related upright to overturned folding, with increasing contribution of strike-slip shearing and sub-horizontal flow towards greater crustal depths. Furthermore, the northerly dip of the previously recognized subsurface crustal reflector within the Kristineberg area is attributed to formation of crustal compartments with opposite polarities within the scale of the whole Skellefte district. The resulting structural framework of the main geological units is visualized in a 3-D model which is available as a 3-D PDF document through the publication website.

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3

Skyttä, P., T. Bauer, T. Hermansson, M. Dehghannejad, C. Juhlin, M. García, J. Hübert, and P. Weihed. "Structural evolution of the VMS-hosting Kristineberg area, Sweden – constraints from structural analysis and 3-D-modelling." Solid Earth Discussions 4, no. 2 (October 8, 2012): 1281–315. http://dx.doi.org/10.5194/sed-4-1281-2012.

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Abstract. Structural mapping and 3-D-modelling with constraints from magnetotelluric (MT) and reflection seismic investigations have been used to provide a geological synthesis of the geometrically complex Kristineberg area in the western part of the Palaeoproterozoic Skellefte district. The results indicate that, like the south-eastern parts of the Skellefte district, the area was subjected to SSE-NNW transpressional deformation at around 1.87 Ga. The contrasting structural geometries between the Kristineberg and the central Skellefte district areas may be attributed to the termination and splaying of a major ESE-WNW-striking high-strain zone into several branches in the northern part of the Kristineberg area. The transpressional structural signature was preferentially developed within the southern of the two antiformal structures of the area, "the Southern antiform", which exposes the deepest cut through the crust and hosts all the economic volcanogenic massive sulphides (VMS) deposits of the area. Partitioning of the SSE-NNW transpression into N–S and E–W components led to formation of a characteristic "flat-steep-flat" geometry defining a highly non-cylindrical hinge of for the Southern antiform. Recognition of the transpressional structural signatures including the "flat-steep-flat" geometry and the distinct pattern of sub-horizontal E–W trending to moderately SW-plunging mineral lineations in the deeper crustal parts of the Kristineberg area is of significance for VMS exploration in both near mine and regional scales. The 3-D-model illustrating the outcomes of this study is available as a 3-D-PDF document through the publication website.

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4

Årebäck, Hans, Timothy J. Barrett, Stig Abrahamsson, and Pia Fagerström. "The Palaeoproterozoic Kristineberg VMS deposit, Skellefte district, northern Sweden, part I: geology." Mineralium Deposita 40, no. 4 (October 27, 2005): 351–67. http://dx.doi.org/10.1007/s00126-005-0476-x.

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5

Barrett, Timothy J., Wallace H. MacLean, and Hans Årebäck. "The Palaeoproterozoic Kristineberg VMS deposit, Skellefte district, northern Sweden. Part II: chemostratigraphy and alteration." Mineralium Deposita 40, no. 4 (November 18, 2005): 368–95. http://dx.doi.org/10.1007/s00126-005-0001-2.

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6

Dehghannejad, Mahdieh, Christopher Juhlin, Alireza Malehmir, Pietari Skyttä, and Pär Weihed. "Reflection seismic imaging of the upper crust in the Kristineberg mining area, northern Sweden." Journal of Applied Geophysics 71, no. 4 (August 2010): 125–36. http://dx.doi.org/10.1016/j.jappgeo.2010.06.002.

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7

Holmström, Henning, Ursula J. Salmon, Erik Carlsson, Paraskev Petrov, and Björn Öhlander. "Geochemical investigations of sulfide-bearing tailings at Kristineberg, northern Sweden, a few years after remediation." Science of The Total Environment 273, no. 1-3 (June 2001): 111–33. http://dx.doi.org/10.1016/s0048-9697(00)00850-0.

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8

Vivallo, Waldo, and Mats Willdén. "Geology and geochemistry of an early Proterozoic volcanic arc sequence at Kristineberg, Skellefte district, Sweden." Geologiska Föreningen i Stockholm Förhandlingar 110, no. 1 (March 1988): 1–12. http://dx.doi.org/10.1080/11035898809453113.

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9

Hannington, Mark D., Ingrid M. Kjarsgaard, Alan G. Galley, and Bruce Taylor. "Mineral-chemical studies of metamorphosed hydrothermal alteration in the Kristineberg volcanogenic massive sulfide district, Sweden." Mineralium Deposita 38, no. 4 (August 7, 2002): 423–42. http://dx.doi.org/10.1007/s00126-002-0299-y.

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10

Ehsan, Siddique Akhtar, Alireza Malehmir, and Mahdieh Dehghannejad. "Re-processing and interpretation of 2D seismic data from the Kristineberg mining area, northern Sweden." Journal of Applied Geophysics 80 (May 2012): 43–55. http://dx.doi.org/10.1016/j.jappgeo.2012.01.004.

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11

Pérez Rodríguez, Nathalie, Emma Engström, Ilia Rodushkin, Peter Nason, Lena Alakangas, and Björn Öhlander. "Copper and iron isotope fractionation in mine tailings at the Laver and Kristineberg mines, northern Sweden." Applied Geochemistry 32 (May 2013): 204–15. http://dx.doi.org/10.1016/j.apgeochem.2012.10.012.

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12

Carlsson, Erik, Jonas Thunberg, Björn Öhlander, and Henning Holmström. "Sequential extraction of sulfide-rich tailings remediated by the application of till cover, Kristineberg mine, northern Sweden." Science of The Total Environment 299, no. 1-3 (November 2002): 207–26. http://dx.doi.org/10.1016/s0048-9697(02)00249-8.

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13

Skyttä, Pietari, Tobias Hermansson, Sten-Åke Elming, and Tobias Bauer. "Magnetic fabrics as constraints on the kinematic history of a pre-tectonic granitoid intrusion, Kristineberg, northern Sweden." Journal of Structural Geology 32, no. 8 (August 2010): 1125–36. http://dx.doi.org/10.1016/j.jsg.2010.06.020.

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14

de los Ángeles García Juanatey, María, Juliane Hübert, Ari Tryggvason, and Laust B. Pedersen. "Imaging the Kristineberg mining area with two perpendicular magnetotelluric profiles in the Skellefte Ore District, northern Sweden." Geophysical Prospecting 61, no. 1 (February 17, 2012): 200–219. http://dx.doi.org/10.1111/j.1365-2478.2011.01040.x.

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15

Chmielowski, Riia M., Nils Jansson, Mac Fjellerad Persson, and Pia Fagerström. "3D modelling of hydrothermal alteration associated with VHMS deposits in the Kristineberg area, Skellefte district, northern Sweden." Mineralium Deposita 51, no. 1 (May 16, 2015): 113–30. http://dx.doi.org/10.1007/s00126-014-0572-x.

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16

Carlsson, Erik, Björn Öhlander, and Henning Holmström. "Geochemistry of the infiltrating water in the vadose zone of a remediated tailings impoundment, Kristineberg mine,northern Sweden." Applied Geochemistry 18, no. 5 (May 2003): 659–74. http://dx.doi.org/10.1016/s0883-2927(02)00156-7.

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17

Widerlund, Anders, Gustav Ebenå, and Jan Landin. "Potential biogeochemical and ecological development of a flooded tailings impoundment at the Kristineberg Zn–Cu mine, northern Sweden." Science of The Total Environment 333, no. 1-3 (October 2004): 249–66. http://dx.doi.org/10.1016/j.scitotenv.2004.05.010.

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18

Widerlund, Anders, Elena Shcherbakova, Jerry Forsberg, Henning Holmström, and Björn Öhlander. "Laboratory simulation of flocculation processes in a flooded tailings impoundment at the Kristineberg Zn–Cu mine, northern Sweden." Applied Geochemistry 19, no. 10 (October 2004): 1537–51. http://dx.doi.org/10.1016/j.apgeochem.2004.01.025.

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19

MULLER, B., M. AXELSSON, and B. OHLANDER. "Adsorption of trace elements on pyrite surfaces in sulfidic mine tailings from Kristineberg (Sweden) a few years after remediation." Science of The Total Environment 298, no. 1-3 (October 21, 2002): 1–16. http://dx.doi.org/10.1016/s0048-9697(02)00141-9.

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20

Hübert, Juliane, María de los Ángeles García Juanatey, Alireza Malehmir, Ari Tryggvason, and Laust B. Pedersen. "The upper crustal 3-D resistivity structure of the Kristineberg area, Skellefte district, northern Sweden revealed by magnetotelluric data." Geophysical Journal International 192, no. 2 (November 27, 2012): 500–513. http://dx.doi.org/10.1093/gji/ggs044.

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21

Hidalgo, Kelvis Pérez, and Erling Nordlund. "Deformation analysis in connection with bending and shear failure of a monitored stope in the Kristineberg mine in Sweden." International Journal of Mining and Mineral Engineering 5, no. 3 (2014): 181. http://dx.doi.org/10.1504/ijmme.2014.064479.

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22

M�ller, B., M. D. Axelsson, and B. �hlander. "Analyses of trace elements on quartz surfaces in sulfidic mine tailings from Kristineberg (Sweden) a few years after remediation." Environmental Geology 45, no. 1 (December 1, 2003): 98–105. http://dx.doi.org/10.1007/s00254-003-0861-7.

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23

García Juanatey, María de los Ángeles, Ari Tryggvason, Christopher Juhlin, Ulf Bergström, Juliane Hübert, and Laust B. Pedersen. "MT and reflection seismics in northwestern Skellefte Ore District, Sweden." GEOPHYSICS 78, no. 2 (March 1, 2013): B65—B76. http://dx.doi.org/10.1190/geo2012-0169.1.

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A seismic reflection and MT survey was carried out along a 27-km long transect in northwestern Skellefte District, as part of a bigger 3D modeling project. The main motivation for the data acquisition is to elucidate the geologic relationship between the known mineralizations in the Adak mining camp to the north and in the well studied Kristineberg area south of the transect. The seismic reflection data were acquired with a VIBSIST system, and show reflectivity down to 3 s. Apart from the conventional processing for crystalline environments, the seismic data was also subject to an azimuthal binning procedure and cross-dip analysis, allowing the orientation of planar reflectors in 3D. Regarding the MT data, it is primarily of good quality along the 17 installed sites. The inversion of the determinant of the impedance tensor yielded a stable 2D resistivity model, dominated by resistors corresponding to the postorogenic intrusions along the transect. Adding the location of the analyzed seismic reflectors in the MT inversion rendered an integrated model that facilitated a preliminary joint interpretation of the data sets. Overall, the results are in good agreement with surface observations and reveal a crude configuration of the geologic units below the transect. The most prominent outcomes are the lateral and depth extent of the large postorogenic intrusions in the area reaching to 5- or 6-km depth, the dimensions of the nearly vertical Brännäs gabbro extending to 6-km depth, and the presence of enhanced conductivities along the transect at about 10 km depth. The latter is probably related to the deep conductor previously identified in the district.

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24

Malehmir, Alireza, Hans Thunehed, and Ari Tryggvason. "The Paleoproterozoic Kristineberg mining area, northern Sweden: Results from integrated 3D geophysical and geologic modeling, and implications for targeting ore deposits." GEOPHYSICS 74, no. 1 (January 2009): B9—B22. http://dx.doi.org/10.1190/1.3008053.

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The Kristineberg mining area in the western part of the Paleoproterozoic Skellefte Ore District, northern Sweden, is well known for its base-metal and recent gold discoveries. A pilot 3D geologic model has been constructed on a crustal scale, covering an area of [Formula: see text] to depths of [Formula: see text]. Constrained 3D inverse and forward gravity modeling have been performed to confirm and refine previous modeling along seismic profiles using mainly 2.5D techniques. The 3D inverse gravity modeling was geared to generating isodensity surfaces that enclose regions within the model of anomalous density contrast. The 3D forward gravity modeling was conducted to include faulting and folding systems that are difficult to include in the inversion. The 3D geologic model supports many previous interpretations but also reveals new features of the regional geology that are important for future targeting of base-metal and gold deposits. The margins of a thick granite in the south dip steeply inward, suggesting the possibility of room to accommodate another large base-metal deposit if the granitic rocks are juxtaposed with volcanic rocks at depth. Gravity modeling also suggests the observed Bouguer gravity high within the western metasediments can be explained by a large mafic intrusion that has dioritic to tonalitic composition and no significant magnetic signature. Because mafic-ultramafic intrusions within metasediments can indicate gold, this interpretation suggests the western metasediments have a high gold potential.

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25

Widerlund, Anders, Elena Shcherbakova, Erik Carlsson, Henning Holmström, and Björn Öhlander. "Laboratory study of calcite–gypsum sludge–water interactions in a flooded tailings impoundment at the Kristineberg Zn–Cu mine, northern Sweden." Applied Geochemistry 20, no. 5 (May 2005): 973–87. http://dx.doi.org/10.1016/j.apgeochem.2004.12.003.

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26

Majoran, Stefan, and Stefan Agrenius. "Preliminary observations on living <i>Krithe praetexta praetexta</i> (Sars, 1866), <i>Sarsicytheridea bradii</i> (Norman, 1865) and other marine ostracods in aquaria." Journal of Micropalaeontology 14, no. 2 (October 1, 1995): 96. http://dx.doi.org/10.1144/jm.14.2.96.

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Abstract. More than fifty years ago, Elofson (1941) showed that it is fully possible to maintain living cultures of marine ostracods in aquaria. He concentrated particularly on determining the generation length of several species. In this study, we provide some preliminary observations on the mode of life and morphological variations of marine ostracods kept in aquaria. They derive from a water depth of 40m in the Gullmar Fjord (58°17′N and 11°29′E), west coast of Sweden. The dominant species are Krithe praetexta praetexta (Sars, 1866) and Sarsicytheridea bradii (Norman, 1865). Other species housed in the aquaria are: Jonesia acuminata (Norman, 1865), Palmoconcha guttata (Norman, 1865), Palmoconcha laevata (Norman, 1865), Cytheropteron latissimum (Norman, 1865), Pterygocythereis jonesii (Baird, 1850), Acanthocythereis dunelmensis (Norman, 1865), Robertsonites tuberculatus (Sars, 1866), Elofsonella concinna (Jones, 1857) and Argilloecia conoidea (Sars, 1923).MATERIAL AND METHODSThe study was carried out at the Kristineberg Marine Research Station, west coast of Sweden, from July of 1992 to June of 1994. Sediment from a depth of 40 m in the Gullmar Fjord was sieved to remove the macrofauna and frozen, then thawed to constitute a 10–20 mm thick sediment layer in two 501 aquaria. The sediment consisted of 8 % sand (>63 μm), 44 % silt (>3.9 μm) and 49 % clay (<3.9 μm), and with a water content of 71 % ± 5% (σ = 2.4). Ostracods from the ≥250 μm sieve fraction of the dredge sample (from a depth of 40 m) were added to the aquaria. They were kept. . .

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27

Malehmir, Alireza, Cedric Schmelzbach, Emmanuel Bongajum, Gilles Bellefleur, Christopher Juhlin, and Ari Tryggvason. "3D constraints on a possible deep >2.5 km massive sulphide mineralization from 2D crooked-line seismic reflection data in the Kristineberg mining area, northern Sweden." Tectonophysics 479, no. 3-4 (December 2009): 223–40. http://dx.doi.org/10.1016/j.tecto.2009.08.013.

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28

Pagel, Mark. "Ancestral Sequence Reconstruction. Based on a meeting held in Kristineberg, Sweden, 30–31 March 2005. Edited by David A. Liberles. Oxford and New York: Oxford University Press. $100.00. xiii + 252 p.; ill.; index. 978‐0‐19‐929918‐8. 2007." Quarterly Review of Biology 83, no. 3 (September 2008): 303–4. http://dx.doi.org/10.1086/592626.

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29

"Prediction of mining conditions at depth in Kristineberg mine, Sweden." International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts 33, no. 4 (June 1996): 184. http://dx.doi.org/10.1016/0148-9062(96)85256-9.

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30

"Analysis of ground support methods at the Kristineberg Mine in Sweden." International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts 31, no. 1 (February 1994): A55. http://dx.doi.org/10.1016/0148-9062(94)92759-6.

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