Dynamic topography of passive continental margins and their hinterlands since the Cretaceous

RD Müller, R Hassan, M Gurnis, N Flament… - Gondwana …, 2018 - Elsevier
Even though it is well accepted that the Earth's surface topography has been affected by
mantle-convection induced dynamic topography, its magnitude and time-dependence …

Observational estimates of dynamic topography through space and time

M Hoggard, J Austermann, C Randel… - Mantle convection …, 2021 - Wiley Online Library
Earth's mantle undergoes convection on million‐year timescales as heat is transferred from
depth to the surface. While this flow has long been linked to the large‐scale horizontal forces …

Detection of a dynamic topography signal in last interglacial sea-level records

J Austermann, JX Mitrovica, P Huybers, A Rovere - Science Advances, 2017 - science.org
Estimating minimum ice volume during the last interglacial based on local sea-level
indicators requires that these indicators are corrected for processes that alter local sea level …

Topography caused by mantle density variations: observation-based estimates and models derived from tomography and lithosphere thickness

B Steinberger - … Supplements to the Monthly Notices of the …, 2016 - academic.oup.com
Large-scale topography may be due to several causes, including (1) variations in crustal
thickness and density structure,(2) oceanic lithosphere age differences,(3) subcrustal …

Stratigraphic framework for the plume mode of mantle convection and the analysis of interregional unconformities on geological maps

AM Friedrich, HP Bunge, SM Rieger, L Colli… - Gondwana …, 2018 - Elsevier
Mantle convection is a fundamental planetary process. Its plate mode is established and
expressed by plate tectonics. Its plume mode also is established and expressed by …

Influence of mantle flow on the drainage of eastern A ustralia since the J urassic P eriod

T Salles, N Flament, D Müller - Geochemistry, Geophysics …, 2017 - Wiley Online Library
Recent studies of the past eastern Australian landscape from present‐day longitudinal river
profiles and from mantle flow models suggest that the interaction of plate motion with mantle …

Earth's isostatic and dynamic topography—A critical perspective

AM Forte, DB Rowley - Geochemistry, Geophysics, Geosystems, 2022 - Wiley Online Library
Earth's topography arises from the linear superposition of isostatic and dynamic
contributions. The isostatic contribution reflects the distribution of thickness and density of …

Effects of dynamic topography on the Cenozoic carbonate compensation depth

SM Campbell, R Moucha, LA Derry… - Geochemistry …, 2018 - Wiley Online Library
Reconstructions of the carbonate compensation depth (CCD) in the past have been used to
inform hypotheses about the nature of weathering, tectonics, climate change, and the major …

Paleo sea-level changes and relative sea-level indicators: Precise measurements, indicative meaning and glacial isostatic adjustment perspectives from Mallorca …

T Lorscheid, P Stocchi, E Casella… - Palaeogeography …, 2017 - Elsevier
Paleo relative sea-level (RSL) indicators formed during the Marine Isotope Stage (MIS) 5e
have been reported by a large number of studies worldwide. Despite this, three main …

Projected climate change in the western North Pacific at the end of the 21st century from ensemble simulations with a high-resolution regional ocean model

G Yamanaka, H Nakano, K Sakamoto, T Toyoda… - Journal of …, 2021 - Springer
Future climate change in the western North Pacific at the end of the 21st century (2081–
2100) was examined using a high-resolution regional ocean model (10-km mesh) under the …