Results 1 to 10 of about 14,415 (244)

Diamond preservation in the lithospheric mantle recorded by olivine in kimberlites [PDF]

open access: yesNature Communications, 2023
The diamond potential of kimberlites is difficult to assess due to several mantle and magmatic processes affecting diamond content. Traditionally, initial evaluations are based on the compositions of mantle-derived minerals (garnet, chromite ...
Andrea Giuliani   +8 more
doaj   +3 more sources

Geodynamic and Isotopic Constraints on the Genesis of Kimberlites, Lamproites and Related Magmas From the Finnish Segment of the Karelian Craton

open access: yesGeochemistry, Geophysics, Geosystems, 2022
Despite the scientific and economic significance of kimberlites and related magmas, their origin is unclear. Here, we address this issue using whole‐rock and perovskite‐derived Sr‐Nd‐Hf isotopes for the three occurrences of kimberlite, lamproites and ...
Hayden Dalton   +7 more
doaj   +2 more sources

Primordial neon and the deep mantle origin of kimberlites [PDF]

open access: yesNature Communications
The genesis of kimberlites is unclear despite the economic and scientific interest surrounding these diamond-bearing magmas. One critical question is whether they tap ancient, deep mantle domains or the shallow convecting mantle with partial melting ...
Andrea Giuliani   +10 more
doaj   +2 more sources

DNA sequencing, microbial indicators, and the discovery of buried kimberlites [PDF]

open access: yesCommunications Earth & Environment, 2023
Population growth and technological advancements are placing growing demand on mineral resources. New and innovative exploration technologies that improve detection of deeply buried mineralization and host rocks are required to meet these demands.
Rachel L. Simister   +6 more
doaj   +2 more sources

Kimberlite eruptions driven by slab flux and subduction angle [PDF]

open access: yesScientific Reports, 2023
Kimberlites are sourced from thermochemical upwellings which can transport diamonds to the surface of the crust. The majority of kimberlites preserved at the Earth’s surface erupted between 250 and 50 million years ago, and have been attributed to ...
Ben R. Mather   +4 more
doaj   +2 more sources

Mapping global kimberlite potential from reconstructions of mantle flow over the past billion years. [PDF]

open access: yesPLoS ONE, 2022
Kimberlites are the primary source of economic grade diamonds. Their geologically rapid eruptions preferentially occur near or through thick and ancient continental lithosphere.
Anton Grabreck   +2 more
doaj   +2 more sources

Tracking the Late Jurassic apparent (or true) polar shift in U‐Pb‐dated kimberlites from cratonic North America (Superior Province of Canada)

open access: yesGeochemistry, Geophysics, Geosystems, 2015
Different versions of a composite apparent polar wander (APW) path of variably selected global poles assembled and averaged in North American coordinates using plate reconstructions show either a smooth progression or a large (∼30°) gap in mean ...
Dennis V. Kent   +4 more
doaj   +2 more sources

Derivation of Lamproites and Kimberlites from a Common Evolving Source in the Convective Mantle: the Case for Southern African ‘Transitional Kimberlites’

open access: yesJournal of Petrology, 2023
‘Transitional kimberlite’ is a collective term previously used to classify rocks occurring in southern Africa that show bulk rock geochemical and Sr–Nd isotope features intermediate between (cratonic) lamproites and kimberlites. However, it is now well
S. Sarkar   +6 more
semanticscholar   +1 more source

Olivine in Kimberlites: Magma evolution from deep mantle to eruption

open access: yesJournal of Petrology, 2022
Elucidating the origin, composition and physical properties of primary kimberlite melts is crucial to our understanding of their source, petrogenesis, ascent mechanisms and ultimately the origin of diamonds.
A. Abersteiner   +4 more
semanticscholar   +1 more source

Trends and rhythms in carbonatites and kimberlites reflect thermo-tectonic evolution of Earth

open access: yesGeology, 2022
Earth’s thermo-tectonic evolution determines the way the planet’s interior and surface interact and shows temporal changes in both trends and periodic rhythms.
Shuangliang Liu   +9 more
semanticscholar   +1 more source

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