| 词条 | Carlsberg Fault zone |
| 释义 |
The Carlsberg Fault zone is a concealed tectonic formation that runs across Copenhagen city centre.[1] It is one of the most significant faults in the Copenhagen area[2] and can be followed for about 30 km.[3] 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][4] Recent earthquakes indicate that this area is tectonically active.[1] It was described for the first time in 1925 at the Carlsberg Breweries.[3] References1. ^1 2 {{cite web|last1=Admin|accessdate=2018-05-02|title=Search|url=http://research.ku.dk/search/?pure=en/publications/integrated-seismic-interpretation-of-the-carlsberg-fault-zone-copenhagen-denmark(4fc002b0-74c3-11db-bee9-02004c4f4f50).html|date=26 April 2007}} {{tectonics-stub}}{{geology-stub}}2. ^"Efforts to include geological and geodetic observations in the assessment of earthquake activity in Denmark". Søren Gregersen and Peter H. Voss, Geological Survey of Denmark and Greenland. Accessed 2 May 2018. 3. ^1 "Copenhagen". Geological Survey of Denmark and Greenland. Accessed 2 May 2018., [https://web.archive.org/web/20050330152419/http://www.geus.dk/vand-og-data/baseline_hinsby_et_al_2003_limestone.pdf backup] 4. ^{{cite journal|title=High-resolution shear-wave seismics across the Carlsberg Fault zone south of Copenhagen — Implications for linking Mesozoic and late Pleistocene structures|url=https://www.sciencedirect.com/science/article/pii/S0040195116301792|journal=Tectonophysics|date=6 July 2016|issn=0040-1951|pages=56–64|volume=682|doi=10.1016/j.tecto.2016.05.043|first1=Janina|last1=Kammann|first2=Christian|last2=Hübscher|first3=Lars|last3=Ole Boldreel|first4=Lars|last4=Nielsen}} 1 : Geology of Denmark |
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