Passive-active rift basin in central and west Europe
The North German Basin is a passive-active rift basin located in central and west Europe, lying within the southeasternmost portions of the North Sea and the southwestern Baltic Sea and across terrestrial portions of northern Germany, Netherlands, and Poland.[1] The North German Basin is a sub-basin of the Southern Permian Basin, that accounts for a composite of intra-continental basins composed of Permian to Cenozoic sediments, which have accumulated to thicknesses around 10–12 kilometres (6–7.5 mi).[2][3] The complex evolution of the basin takes place from the Permian to the Cenozoic, and is largely influenced by multiple stages of rifting, subsidence, and salt tectonic events. The North German Basin also accounts for a significant amount of Western Europe's natural gas resources, including one of the world's largest natural gas reservoir, the Groningen gas field.[4]
^Hubscher, C. (October 28, 2009). "Structure and evolution of the Northeastern German Basin and its transition onto the Baltic Shield". Marine and Petroleum Geology. 27 (4): 923–938. doi:10.1016/j.marpetgeo.2009.10.017.
^Cite error: The named reference Scheck was invoked but never defined (see the help page).
^Gemmer, Lykke (September 2002). "Late Cretaceous–Cenozoic evolution of the North German Basin—results from 3-D geodynamic modelling". Tectonophysics. 373 (1–4): 39–54. doi:10.1016/s0040-1951(03)00282-8.
^Cite error: The named reference Gautier was invoked but never defined (see the help page).
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