The Carlsberg Fault zone is a concealed tectonic formation that runs across Copenhagen city centre, [1] a side branch of the Trans-European Suture Zone. It is one of the most significant faults in the Copenhagen area [2] being 400 to 700 meters wide and can be followed for about 30 km. [3] It runs just east of the Frederiksberg Gardens in Copenhagen. [4] [5] The Frederiksberg Municipality collects about half of its water from the fault zone. [6]
The Carlsberg Fault is located in a NNW-SSE striking fault system in the border zone between the Danish Basin and the Baltic Shield. [1] [7] Recent earthquakes indicate that this area is tectonically active. [1]
It was described for the first time in 1925 at the Carlsberg Breweries. [3]
- ^ a b c Admin (26 April 2007). "Search". Retrieved 2018-05-02.
- ^ " Efforts to include geological and geodetic observations in the assessment of earthquake activity in Denmark Archived 2018-05-02 at the Wayback Machine". Søren Gregersen and Peter H. Voss, Geological Survey of Denmark and Greenland. Accessed 2 May 2018.
- ^ a b " Copenhagen". Geological Survey of Denmark and Greenland. Accessed 2 May 2018., backup
- ^ Nielsen, Lars; Thybo, Hans; Jørgensen, Mette I. (2005). "Integrated seismic interpretation of the Carlsberg fault zone, Copenhagen, Denmark". Geophysical Journal International. 162 (2): 461. Bibcode: 2005GeoJI.162..461N. doi: 10.1111/j.1365-246X.2005.02664.x. Archived from the original on 2013-04-01.
- ^ Nielsen, Lars; Thybo, Hans (2004). "Location of the Carlsberg fault zone from seismic controlled-source fan recordings". Geophysical Research Letters. 31 (7): n/a. Bibcode: 2004GeoRL..31.7621N. doi: 10.1029/2004GL019603.
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^
"Vand fra Frederiksbergs undergrund" [Water from Frederiksberg's Underground]. Frederiksberg Forsyning (in Danish). Archived from the original on 4 May 2012. Retrieved 16 Oct 2014.
{{ cite web}}: CS1 maint: bot: original URL status unknown ( link) - ^ Kammann, Janina; Hübscher, Christian; Ole Boldreel, Lars; Nielsen, Lars (6 July 2016). "High-resolution shear-wave seismics across the Carlsberg Fault zone south of Copenhagen — Implications for linking Mesozoic and late Pleistocene structures". Tectonophysics. 682: 56–64. Bibcode: 2016Tectp.682...56K. doi: 10.1016/j.tecto.2016.05.043. ISSN 0040-1951.
 | This tectonics article is a stub. You can help Wikipedia by expanding it. |
The Carlsberg Fault zone is a concealed tectonic formation that runs across Copenhagen city centre, [1] a side branch of the Trans-European Suture Zone. It is one of the most significant faults in the Copenhagen area [2] being 400 to 700 meters wide and can be followed for about 30 km. [3] It runs just east of the Frederiksberg Gardens in Copenhagen. [4] [5] The Frederiksberg Municipality collects about half of its water from the fault zone. [6]
The Carlsberg Fault is located in a NNW-SSE striking fault system in the border zone between the Danish Basin and the Baltic Shield. [1] [7] Recent earthquakes indicate that this area is tectonically active. [1]
It was described for the first time in 1925 at the Carlsberg Breweries. [3]
- ^ a b c Admin (26 April 2007). "Search". Retrieved 2018-05-02.
- ^ " Efforts to include geological and geodetic observations in the assessment of earthquake activity in Denmark Archived 2018-05-02 at the Wayback Machine". Søren Gregersen and Peter H. Voss, Geological Survey of Denmark and Greenland. Accessed 2 May 2018.
- ^ a b " Copenhagen". Geological Survey of Denmark and Greenland. Accessed 2 May 2018., backup
- ^ Nielsen, Lars; Thybo, Hans; Jørgensen, Mette I. (2005). "Integrated seismic interpretation of the Carlsberg fault zone, Copenhagen, Denmark". Geophysical Journal International. 162 (2): 461. Bibcode: 2005GeoJI.162..461N. doi: 10.1111/j.1365-246X.2005.02664.x. Archived from the original on 2013-04-01.
- ^ Nielsen, Lars; Thybo, Hans (2004). "Location of the Carlsberg fault zone from seismic controlled-source fan recordings". Geophysical Research Letters. 31 (7): n/a. Bibcode: 2004GeoRL..31.7621N. doi: 10.1029/2004GL019603.
-
^
"Vand fra Frederiksbergs undergrund" [Water from Frederiksberg's Underground]. Frederiksberg Forsyning (in Danish). Archived from the original on 4 May 2012. Retrieved 16 Oct 2014.
{{ cite web}}: CS1 maint: bot: original URL status unknown ( link) - ^ Kammann, Janina; Hübscher, Christian; Ole Boldreel, Lars; Nielsen, Lars (6 July 2016). "High-resolution shear-wave seismics across the Carlsberg Fault zone south of Copenhagen — Implications for linking Mesozoic and late Pleistocene structures". Tectonophysics. 682: 56–64. Bibcode: 2016Tectp.682...56K. doi: 10.1016/j.tecto.2016.05.043. ISSN 0040-1951.
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| This tectonics article is a stub. You can help Wikipedia by expanding it. |