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Publikováno v:
Geofluids, Vol 2018 (2018)
Underpressures (subhydrostatic heads) in the Paleozoic units underlying the Great Plains of North America are a consequence of Cenozoic uplift of the area. Based on tectonostratigraphic data, we have developed a cumulative uplift history with superim
Externí odkaz:
https://doaj.org/article/9bbce6ac29ed4a67930295dcdc8879e0