Graham Pearson

Professor

University of Alberta

Canada

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Professor Graham Pearson is a faculty member at the University of Alberta, Canada. His research focuses on the formation and evolution of cratonic lithosphere, with recent articles exploring topics such as diamond formation in different geological environments and the rheological controls on craton stabilization. He employs advanced techniques including machine learning to study mantle processes and the transport of water into the mantle.

Graham Pearson

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Articles (22)

Diamonds from Fort à la Corne – post-Archean formation in exceptionally cool and fertile lherzolitic substrates

Profound pyroxenitic/megacrystic overprinting of the central Superior craton lithosphere recorded by sodic Cr-diopside xenocrysts from the Attawapiskat kimberlites, Ontario, Canada

Cool transient lithospheric thermal conditions driven by subduction recorded by Neoarchean diamonds from Knee Lake, northwestern Superior Craton

Thickening Cratonic Lithosphere by Horizontal Compression in the Presence of Surface Erosion and Sedimentation

A Machine Learning Approach to Single Garnet Geothermometry and Application to Tracing the Fingerprint of Superdeep Diamonds

A Rare Glimpse of Paleoproterozoic Sub‐Arc Mantle: The Ussuit Peridotite, West Greenland

Evaluating the Rheological Controls on Topography Development During Craton Stabilization: Objective Approaches to Comparing Geodynamic Models

Dense hydrated Mg-silicates in diamond: Implications for transport of H 2 O into the mantle

Garnet Pyroxenite Cumulates from Cretaceous Alkaline Intraplate Magmas Underplate the Zealandia Mantle Lithosphere

Extreme redox variations in a superdeep diamond from a subducted slab

Ni isotopes provide a glimpse of Earth’s pre-late-veneer mantle

Widespread PREMA in the upper mantle indicated by low-degree basaltic melts

Diamond preservation in the lithospheric mantle recorded by olivine in kimberlites

Re-healing cratonic mantle lithosphere after the world's largest igneous intrusion: Constraints from peridotites erupted by the Premier kimberlite, South Africa

Comment on “Discovery of davemaoite, CaSiO 3 -perovskite, as a mineral from the lower mantle”

No mantle residues in the Isua Supracrustal Belt

Author Correction: Fingerprinting the Cretaceous-Paleogene boundary impact with Zn isotopes

Heat Generation in Cratonic Mantle Roots—New Trace Element Constraints From Mantle Xenoliths and Implications for Cratonic Geotherms

Deep continental roots and cratons

Modification of Lithospheric Mantle by Melts/Fluids With Different Sulfur Fugacities During the Wilson Cycle: Insights From Lesvos and Global Ophiolitic Peridotites

Fingerprinting the Cretaceous-Paleogene boundary impact with Zn isotopes

Tungsten-182 evidence for an ancient kimberlite source

Collaborators (19)

Andreas Auer

James Scott

Jeroen van Hunen

Simon Kohn

Kristoffer Szilas

Thomas Stachel

David Phillips

Lingyu Zhang

Qiwei Zhang

Richard Walker

Robert Luth

Jon Woodhead

Fabrizio Nestola

Claire A Currie

LUCA BINDI

Pedro Waterton

Gareth Rees Davies

Marissa K. Spencer

Steven D. Jacobsen

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