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All abstracts by Richard Wirth at Goldschmidt2019
| Recycling Oceanic Crust in Mantle Revealed by Diamond within Chromitite from the Mirdita Ophiolite (Albania)
Wu W, Yang J, Wirth R, Zheng J, Lian D & Qiu T |
03b/09:45/Mo |
| Mineral Inclusions in Ophiolite-Hosted Diamonds Provide Strong Evidence of a Deep Mantle Origin
Robinson PT, Yang J, Wirth R & Lian D |
03b/11:00/Mo |
| Deep Subduction in the Archean Indicated by Ultrahigh-Pressure Polymorphs of Chromite and Rutile in Archean Ophiolitic Podiform Chromite
Kusky T, Wang L, Huang Y, Robinson P, Wirth R & Ning W |
03b/14:30/Mo |
| Multi-Stage Process of the Purang Ophiolitic Chromitites (SW Tibet): Insights from Magnesiochromite-Hosted Silicate Mineral and Other Inclusions
Xiong F, Yang J, Dilek Y, Wirth R & Xu X |
03b/68/Mo |
| Attachment of the Rock-Inhabiting Fungus K. Petricola A95 to Olivine Enhances Mineral Dissolution by Preventing the Precipitation of Iron (Oxyhydr)oxides
Gerrits R, Pokharel R, Breitenbach R, Feldmann I, Radnik J, Wirth R, Schuessler J, von Blanckenburg F, Gorbushina A & Schott J |
11e/463/Mo |
| Nanostructure of Platinum Group Minerals in Ural-Alaskan-Type Intrusions: From Magmatic to Hydrothermal Environments
Pushkarev E, Ballhaus C, Wirth R, Gottman I, Kamenetsky V & Shreiber A |
04c/15:00/Tu |
| Pt-Re-Os Dating of the Pt-Alloys from the Kondyor Zoned Mafic-Ultramafic Complex (Far East Russia)
Luguet A, Nowell G, Pushkarev E, Ballhaus C, Wirth R & Schreiber A |
03i/16:15/Tu |
| Alluvial Diamonds from Iron-Saturated Mantle beneath Northeastern Margin of Siberian Craton
Shatsky V, Ragozin A, Logvinova A, Wirth R & Sobolev N |
03i/153/Tu 03i/09:40/Fr |
| Metastable Phases in Foraminifer Amphistegina sp. Shells and Implications for Biomineralisation
Jacob D, Wirth R, Schreiber A, Erez J, Branson O & Eggins S |
04o/16:15/Fr |
| First Molecular Identification of Fungi Microfossils in 715-810 Millions-Years Shale Rock
Bonneville S, Delpomdor F, Préat A, Chevalier C, Araki T, Abyaneh M, Steele A, Schreiber A, Wirth R & Benning LG |
07e/16:30/Fr |
