Palaeogeological hiatus surface mapping: a tool to visualize vertical motion of the continents

Dynamic topography is a well-established consequence of global geodynamic models of mantle convection with horizontal dimensions of >1000 km and amplitudes up to 2 km. Such physical models guide the interpretation of geological records on equal dimensions. Continent-scale geological maps therefor...

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Veröffentlicht in:	Geological magazine 2019-02, Vol.156 (2), p.308-319
1. Verfasser:	FRIEDRICH, ANKE M.
Format:	Artikel
Sprache:	eng
Schlagworte:	absolute age Amplitudes Anchors Basins biostratigraphy Boundaries Bremen Germany calibration Cenozoic Central Europe chronostratigraphy Convection Cretaceous dates Datum (elevation) Deep wells Dimensions Duration Dynamic topography Erosion Europe geodynamics Geologic mapping Geological data Geological mapping Geological maps Geological time Geology geophysical methods geophysical surveys Geophysics Germany Lower Saxony Germany Mantle convection Mapping Mesozoic Original Article Palaeotopography paleorelief plate tectonics Precambrian Resolution sedimentation seismic methods Seismic profiles Shape solid Earth (tectonophysics) Stratigraphy Surface motion surveys Temporal resolution Tertiary topography Topography (geology) U/Pb unconformities Vertical motion vertical movements Visualization Wavelength
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