WebThe most important Jurassic rifting phase in the North Sea area took place during the Late Jurassic and lasted into the Early Cretaceous. During this tectonic epi-sode, major block faulting caused uplift and tilting, creating considerable local topography with erosion and sediment supply. Webments were deposited in the Southern North Sea because of the thermal subsidence following Perm-ian‒Triassic rifting. But there was no volcanic activity during Early Jurassic. During Middle Jurassic, due to the development of the warm mantle plume head, a subaerial thermal dome was formed in the Central North Sea [21]. The Central North …
Late Palaeozoic to Early Cenozoic geological evolution of the ...
Web28 okt. 2003 · Abstract. During the Jurassic – Early Cretaceous, the Danish Central Graben developed as a N–S- to NNW– SSE-trending graben bounded by the Ringkøbing–Fyn High towards the east and the Mid North Sea High towards the west. The graben consists of a system of half-grabens and evolved by faultcontrolled subsidence; three main rift pulses ... Web17 mrt. 2024 · As a result of thermal uplift related to the North Sea Dome (Mid-Cimmerian erosional phase: Underhill & Partington 1993; Graversen 2002, 2006), regional erosion … new york association of school boards
Northern North Sea basin - Wikipedia
WebMiddle-Late Jurassic North Sea Rift Dome was established by recognition of the near base Middle Jurassic erosional unconformity in the central North Sea. Web1 jan. 2005 · The Middle-Late Jurassic North Sea Rift Dome was established by recognition of the near base Middle Jurassic erosional unconformity in the central North Sea. The … Webemergent physical barriers, as exemplified by the Central North Sea Dome with its associated volcanics. The climatic gradient across the 30º of temperate latitude spanned by the European seas governed biotic diversity and biogeography, finding expression in rock-forming biogenic mile bluff clinic address