Destruction and regrowth of lithospheric mantle beneath large igneous provinces
Large igneous provinces (LIPs) are formed by enormous (ie, frequently> 106 km3) but short-
lived magmatic events that have profound effects upon global geodynamic, tectonic, and …
lived magmatic events that have profound effects upon global geodynamic, tectonic, and …
Episodic kilometre-scale burial and exhumation and the importance of missing section
P Green, I Duddy, P Japsen - Earth-Science Reviews, 2022 - Elsevier
The incompleteness of the stratigraphical record is well documented, and the concept of
“missing time” has attracted renewed attention in recent years. However, the importance of …
“missing time” has attracted renewed attention in recent years. However, the importance of …
Global influence of mantle temperature and plate thickness on intraplate volcanism
The thermochemical structure of lithospheric and asthenospheric mantle exert primary
controls on surface topography and volcanic activity. Volcanic rock compositions and mantle …
controls on surface topography and volcanic activity. Volcanic rock compositions and mantle …
Quantifying the relationship between short‐wavelength dynamic topography and thermomechanical structure of the upper mantle using calibrated parameterization of …
Oceanic residual depth varies on 5,000 km wavelengths with amplitudes of±1 km. A
component of this short‐wavelength signal is dynamic topography caused by convective …
component of this short‐wavelength signal is dynamic topography caused by convective …
The post-Caledonian thermo-tectonic evolution of Fennoscandia
The evolution of Fennoscandia following the early Devonian collapse of the Caledonian
mountains is a matter of debate, due largely to the scarcity of post-Caledonian cover rocks …
mountains is a matter of debate, due largely to the scarcity of post-Caledonian cover rocks …
[HTML][HTML] Episodes of post-Caledonian burial and exhumation in Greenland and Fennoscandia
The forces that drive uplift of the continental lithosphere outside collision zones are a topic of
considerable dispute. Here we review our studies of the post-Caledonian development of …
considerable dispute. Here we review our studies of the post-Caledonian development of …
Climate aridity delays morphological response of Andean river valleys to tectonic uplift
Abstract In the south Central Andes, a complex relationship between climate, tectonics,
erosion and topography is well documented. Building on recent advances in the mechanical …
erosion and topography is well documented. Building on recent advances in the mechanical …
[HTML][HTML] Relative sea level response to mixed carbonate-siliciclastic sediment loading along the Great Barrier Reef margin
The continental shelf along northeastern Australia is the world's largest mixed carbonate-
siliciclastic passive margin and the location of the Great Barrier Reef (GBR). Following sea …
siliciclastic passive margin and the location of the Great Barrier Reef (GBR). Following sea …
Observations and models of dynamic topography: Current status and future directions
The slow cree** motion of Earth's mantle drives transient changes in surface topography
across a variety of spatial and temporal scales. Recent decades have seen substantial …
across a variety of spatial and temporal scales. Recent decades have seen substantial …
Evidence for active upper mantle flow in the Atlantic and Indo-Australian realms since the Upper Jurassic from hiatus maps and spreading rate changes
Histories of large-scale horizontal and vertical lithosphere motion hold important information
on mantle convection. Here, we compare continent-scale hiatus maps as a proxy for mantle …
on mantle convection. Here, we compare continent-scale hiatus maps as a proxy for mantle …