Crustal fault reactivation facilitating lithospheric folding/buckling in the central Indian Ocean
High-quality, normal-incidence seismic reflection data confirm that tectonic deformation in the central Indian Ocean occurs at two spatial scales: whole lithosphere folding with wavelengths varying between 100 and 300 km, and compressional reactivation ...
Beekman, F. +3 more
core +1 more source
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Rogers HF, Mandea M.
europepmc +2 more sources
Waned mantle upwelling contributes to a heavily deformed northern smooth plains on Mercury. [PDF]
Xie J, Zhan Y, Gong S, Huang C, Zhang J.
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Newly Identified Early Cretaceous High-Mg Diorites in the Southern Dayaoshan Area of South China: Petrogenesis and Geodynamic Implications. [PDF]
Wei Y, Meng L, Zhang Y.
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MODERN APPROACHES ALLOCATION AND THE LITHOSPHERE MAGNETIC FIELD MODELING
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Melt burst events in a dominantly amagmatic lithosphere at Gakkel Ridge in the Arctic Ocean. [PDF]
Zhou F, Grevemeyer I, Dyment J.
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Mantle melting and lithospheric structure beneath eastern Australia's Cenozoic volcanoes from 3D magnetotellurics. [PDF]
Margiono R, Heinson G.
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Modeling of the Arabian/Nubian shield's geothermal structure: a multi-parametric analysis using geophysical and geological tools. [PDF]
Haggag M +5 more
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Mode of intracontinental mountain building controlled by lower crustal composition and mantle lithosphere depletion. [PDF]
Xu X +14 more
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