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Showing 1–7 of 7 results

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Research | 19 November 2019 | Open
Cooling history and emplacement of a pyroxenitic lava as proxy for understanding Martian lava flows
Scientific Reports 9 , 1–7

Rights & permissionsfor article Cooling history and emplacement of a pyroxenitic lava as proxy for understanding Martian lava flows . Opens in a new window.
Amendments and Corrections | 5 June 2018
Publisher Correction: Modification of the Western Gondwana craton by plume–lithosphere interaction
- Jiashun Hu
- , Lijun Liu
- , Manuele Faccenda
- , Quan Zhou
- , Karen M. Fischer
- , Stephen Marshak
- & Craig Lundstrom
Nature Geoscience 11 , 544–544

Rights & permissionsfor article Publisher Correction: Modification of the Western Gondwana craton by plume–lithosphere interaction . Opens in a new window.
Research | 25 March 2019
Ubiquitous lower-mantle anisotropy beneath subduction zones
Nature Geoscience 12 , 301–306

Rights & permissionsfor article Ubiquitous lower-mantle anisotropy beneath subduction zones . Opens in a new window.
Research | 11 October 2009
Deep slab hydration induced by bending-related variations in tectonic pressure
Nature Geoscience 2 , 790–793

Rights & permissionsfor article Deep slab hydration induced by bending-related variations in tectonic pressure . Opens in a new window.
Research | 23 October 2008
Fault-induced seismic anisotropy by hydration in subducting oceanic plates
- ...of anisotropic patterns observed worldwide. Manuele Faccenda and colleagues now show that...
Nature 455 , 1097–1100

Rights & permissionsfor article Fault-induced seismic anisotropy by hydration in subducting oceanic plates . Opens in a new window.
Research | 19 February 2018
Modification of the Western Gondwana craton by plume–lithosphere interaction
- Jiashun Hu
- , Lijun Liu
- , Manuele Faccenda
- , Quan Zhou
- , Karen M. Fischer
- , Stephen Marshak
- & Craig Lundstrom
Nature Geoscience 11 , 203–210

Rights & permissionsfor article Modification of the Western Gondwana craton by plume–lithosphere interaction . Opens in a new window.
Research | 29 February 2016 | Open
Upper- and mid-mantle interaction between the Samoan plume and the Tonga–Kermadec slabs
Nature Communications 7 , 1–9

Rights & permissionsfor article Upper- and mid-mantle interaction between the Samoan plume and the Tonga–Kermadec slabs . Opens in a new window.

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Cooling history and emplacement of a pyroxenitic lava as proxy for understanding Martian lava flows

Publisher Correction: Modification of the Western Gondwana craton by plume–lithosphere interaction

Ubiquitous lower-mantle anisotropy beneath subduction zones

Deep slab hydration induced by bending-related variations in tectonic pressure

Fault-induced seismic anisotropy by hydration in subducting oceanic plates

Modification of the Western Gondwana craton by plume–lithosphere interaction

Upper- and mid-mantle interaction between the Samoan plume and the Tonga–Kermadec slabs

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