Geothermal heat flow in Antarctica: current and future directions
A Burton-Johnson, R Dziadek… - The Cryosphere …, 2020 - tc.copernicus.org
Antarctic geothermal heat flow (GHF) affects the temperature of the ice sheet, determining its
ability to slide and internally deform, as well as the behaviour of the continental crust …
ability to slide and internally deform, as well as the behaviour of the continental crust …
Crustal evolution of divergent and transform segments of the Brazilian Equatorial Margin derived from integrated geophysical data: Insights from basement grain …
DL de Castro, DC Oliveira, DRH Herrera… - Earth-Science …, 2022 - Elsevier
The present comprehensive multidisciplinary geophysical study provides new insights into
the structural architecture and tectonic development of the Brazilian Equatorial Margin …
the structural architecture and tectonic development of the Brazilian Equatorial Margin …
Lithospheric structural dynamics and geothermal modeling of the Western Arabian Shield
Understanding the dynamics of suturing and cratonisation and their implications are vital in
estimating the link between the lithospheric mantle architecture and geothermal resources …
estimating the link between the lithospheric mantle architecture and geothermal resources …
Timing of the martian dynamo: New constraints for a core field 4.5 and 3.7 Ga ago
The absence of crustal magnetic fields above the martian basins Hellas, Argyre, and Isidis is
often interpreted as proof of an early, before 4.1 billion years (Ga) ago, or late, after 3.9 Ga …
often interpreted as proof of an early, before 4.1 billion years (Ga) ago, or late, after 3.9 Ga …
Weak magnetism of Martian impact basins may reflect cooling in a reversing dynamo
Understanding the longevity of Mars's dynamo is key to interpreting the planet's atmospheric
loss history and the properties of its deep interior. Satellite data showing magnetic lows …
loss history and the properties of its deep interior. Satellite data showing magnetic lows …
A global Curie depth model utilising the equivalent source magnetic dipole method
The depth to the Curie isotherm provides a snapshot into the deep thermal conditions of the
crust, which helps constrain models of thermally controlled physical properties and …
crust, which helps constrain models of thermally controlled physical properties and …
Review of Curie point depth determination through different spectral methods applied to magnetic data
Spectral methods have been applied for more than 40 yr to calculate the depth to magnetic
sources and the Curie point depth or Moho depth. Unfortunately, conceptual, theoretical and …
sources and the Curie point depth or Moho depth. Unfortunately, conceptual, theoretical and …
Eight good reasons why the uppermost mantle could be magnetic
Abstract Wasilewski et al.(1979) concluded that no magnetic remanence existed in the
uppermost mantle and that even if present, such sources would be at temperatures too high …
uppermost mantle and that even if present, such sources would be at temperatures too high …
Magnetism in cold subducting slabs at mantle transition zone depths
The Earth's crust–mantle boundary, the Mohorovičić discontinuity, has been traditionally
considered to be the interface between the magnetic crust and the non-magnetic mantle …
considered to be the interface between the magnetic crust and the non-magnetic mantle …
[HTML][HTML] A mantle plume origin for the Palaeoproterozoic Circum-Superior large Igneous Province
Abstract The Circum-Superior Large Igneous Province (LIP) consists predominantly of
ultramafic-mafic lavas and sills with minor felsic components, distributed as various …
ultramafic-mafic lavas and sills with minor felsic components, distributed as various …