269 results on '"Pearson, D.G."'
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2. The relative roles of ancient and juvenile crust in building accretionary orogens – Minimal ancient crust involved in the magmatic evolution of a North American Cordillera accreted terrane indicated by igneous zircon Hf-O
3. Zircon geochronology and Hf–O isotopes of the Nulliak supracrustal assemblage (Saglek Block–Canada): Constraints on deposition age and setting, metamorphic age and environments of zircon crystallization
4. Geochronology of scapolite pegmatites from the Nordøyane ultra-high-pressure domain, Western Gneiss Region, Norway: Protracted crystal-melt reaction during Scandian exhumation
5. Extent and age of Mesoarchean components in the Nagssugtoqidian orogen, West Greenland: Implications for tectonic environments and crust building in cratonic orogenic belts
6. Deep carbon through time: Earth’s diamond record and its implications for carbon cycling and fluid speciation in the mantle
7. Trace element analysis of high-Mg olivine by LA-ICP-MS – Characterization of natural olivine standards for matrix-matched calibration and application to mantle peridotites
8. The application of trace elements and Sr–Pb isotopes to dating and tracing ruby formation: The Aappaluttoq deposit, SW Greenland
9. Diamond-forming media through time – Trace element and noble gas systematics of diamonds formed over 3 billion years of Earth’s history
10. A common parentage-low abundance trace element data of gem diamonds reveals similar fluids to fibrous diamonds
11. A whole-lithosphere view of continental growth
12. Timing and origin of magmatism in the Sverdrup Basin, Northern Canada—Implications for lithospheric evolution in the High Arctic Large Igneous Province (HALIP)
13. The uniquely high-temperature character of Cullinan diamonds: A signature of the Bushveld mantle plume?
14. Statistical approaches to the discrimination of crust- and mantle-derived low-Cr garnet – Major-element-based methods and their application in diamond exploration
15. U-Pb and Lu-Hf isotopes of the Archean orthogneiss complex on eastern Hall Peninsula, southern Baffin Island, Nunavut: Identification of exotic Paleo- to Mesoarchean crust beneath eastern Hall Peninsula
16. Geobarometric evidence for a LM/TZ origin of CaSiO3 in a sublithospheric diamond
17. The transition zone as a host for recycled volatiles: Evidence from nitrogen and carbon isotopes in ultra-deep diamonds from Monastery and Jagersfontein (South Africa)
18. The aluminum-in-olivine thermometer for mantle peridotites — Experimental versus empirical calibration and potential applications
19. Contextual representations of negative images modulate intrusion frequency in an intrusion provocation paradigm
20. Evidence for H2O-bearing fluids in the lower mantle from diamond inclusion
21. Investigating metasomatic effects on the 187Os isotopic signature: A case study on micrometric base metal sulphides in metasomatised peridotite from the Letlhakane kimberlite (Botswana)
22. Duration and periodicity of kimberlite volcanic activity in the Lac de Gras kimberlite field, Canada and some recommendations for kimberlite geochronology
23. Plume impingement on the Siberian SCLM: Evidence from Re–Os isotope systematics
24. Precise Pb isotope ratio determination of picogram-size samples: A comparison between multiple Faraday collectors equipped with 1012 Ω amplifiers and multiple ion counters
25. Precise U-Pb Age for the Great Whin Dolerite Complex, N.E. England and Its Significance
26. Mesoarchean diamonds formed in thickened lithosphere, caused by slab-stacking
27. An eclogitic diamond from Mir pipe (Yakutia), recording two growth events from different isotopic sources
28. Triple oxygen isotope evidence for a hot Archean ocean
29. Ancient roots of tungsten in western North America
30. Trace elements in gem diamond from Akwatia, Ghana and DeBeers Pool, South Africa
31. The 190Pt–186Os decay system applied to dating platinum-group element mineralization of the Bushveld Complex, South Africa
32. No mantle residues in the Isua Supracrustal Belt
33. Hydrous mantle transition zone indicated by ringwoodite included within diamond
34. Formation of the North Atlantic Craton: Timing and mechanisms constrained from Re–Os isotope and PGE data of peridotite xenoliths from S.W. Greenland
35. Re–Os isotope and PGE constraints on the timing and origin of gold mineralisation in the Witwatersrand Basin
36. Combined Sr isotope and trace element analysis of melt inclusions at sub-ng levels using micro-milling, TIMS and ICPMS
37. Geochemistry of hypabyssal kimberlites from Lac de Gras, Canada: Comparisons to a global database and applications to the parent magma problem
38. Crystallization of megacrysts from protokimberlitic fluids: Geochemical evidence from high-Cr megacrysts in the Jericho kimberlite
39. An alternative model for silica enrichment in the Kaapvaal subcontinental lithospheric mantle
40. Highly siderophile element behaviour accompanying subduction of oceanic crust: Whole rock and mineral-scale insights from a high-pressure terrain
41. The Formation and Evolution of Cratonic Mantle Lithosphere – Evidence from Mantle Xenoliths
42. Mantle Samples Included in Volcanic Rocks
43. Protogenetic sulfide inclusions in diamonds date the diamond formation event using Re-Os isotopes
44. Extreme platinum-group element fractionation and variable Os isotope compositions in Philippine Sea Plate basalts: Tracing mantle source heterogeneity
45. Precise and accurate 186Os/ 188Os and 187Os/ 188Os measurements by Multi-collector Plasma Ionisation Mass Spectrometry, part II: Laser ablation and its application to single-grain Pt–Os and Re–Os geochronology
46. Precise and accurate 186Os/ 188Os and 187Os/ 188Os measurements by multi-collector plasma ionisation mass spectrometry (MC-ICP-MS) part I: Solution analyses
47. Formation of Archaean continental lithosphere and its diamonds: the root of the problem
48. Methods for the microsampling and high-precision analysis of strontium and rubidium isotopes at single crystal scale for petrological and geochronological applications
49. Corrigendum to “Onset of new, progressive crustal growth in the central Slave craton at 3.55 Ga” by Reimink et al., 2019
50. Hafnium isotopes in zircons document the gradual onset of mobile-lid tectonics
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