Wykaz publikacji wybranego autora

Jarosław Majka, dr hab. inż., prof. AGH

profesor nadzwyczajny

Faculty of Geology, Geophysics and Environmental Protection
WGGiOŚ-kmpig

  • 2018

    [dyscyplina 1] dziedzina nauk ścisłych i przyrodniczych / nauki o Ziemi i środowisku

[poprzednia klasyfikacja] obszar nauk przyrodniczych / dziedzina nauk o Ziemi / geologia

Identyfikatory Autora Informacje o Autorze w systemach zewnętrznych

ORCID: 0000-0002-6792-6866 orcid iD

ResearcherID: S-2673-2018

Scopus: 25422587700

PBN: 5e7094a3878c28a0473c0c9e

OPI Nauka Polska

System Informacyjny AGH (SkOs)

1
  • $^{40}Ar/^{39}Ar$ dates controlled by white mica deformation and strain localization: Insights from comparing in situ laser ablation and single-grain fusion techniques
2
  • Brittle deformation during eclogitization of early paleozoic blueschist
3
  • Cambrian ages for metavolcanic rocks in the Lower Köli Nappes, Swedish Caledonides: implications for the status of the Virisen arc terrane
4
  • Carbonate alteration of ophiolitic rocks in the Arabian-Nubian Shield of Egypt: sources and compositions of the carbonating fluid and implications for the formation of Au deposits
5
  • Comment on the paper: “Evolution of a gneiss in the Seve nappe complex of central Sweden – Hints at an early Caledonian, medium-pressure metamorphism” by Li et al. (2020)
6
  • Contrasting coronas: microscale fluid variation deduced from monazite breakdown products in altered metavolcanic rocks associated with the Grängesberg apatite-iron oxide ore, Bergslagen, Sweden
7
  • Deciphering late Devonian-early Carboniferous \emph{P–T–t} path of mylonitized garnet-mica schists from Prins Karls Forland, Svalbard
8
  • Deciphering the tectonometamorphic history of subducted metapelites using quartz-in-garnet and Ti-in-quartz (QuiG–TiQ) geothermobarometry — a key for understanding burial in the Scandinavian Caledonides
9
  • Decompressional equilibration of the Midsund granulite from Otrøy, Western Gneiss Region, Norway
10
  • Detrital zircon signatures of the Baltoscandian margin along the Arctic Circle Caledonides in Sweden: the Sveconorwegian connection
11
  • Detrital zircon U-Pb geochronology of a metasomatic calc-silicate in the Tsäkkok Lens, Scandinavian Caledonides
12
  • Devonian subduction and syncollisional exhumation of continental crust in Lofoten, Norway
13
  • Differences in decompression of a high-pressure unit: a case study from the Cycladic Blueschist Unit on Naxos Island, Greece
14
  • Do the oldest conodonts in the world come from Svalbard?
15
  • Early Neoproterozoic magmatism and Caledonian metamorphism recorded by the Marma terrane, Seve Nappe Complex, northern Swedish Caledonides
16
  • Eclogite and garnet pyroxenite from Stor Jougdan, Seve Nappe Complex, Sweden: implications for UHP metamorphism of allochthons in the Scandinavian Caledonides
17
  • Ediacaran metazoan fossils with siliceous skeletons from the Digermulen Peninsula of Arctic Norway
18
19
  • Exhumation of continental margin rocks from mantle depths to orogenic foreland: example from the Seve Nappe Complex of the central Scandinavian Caledonides
20
  • Exhumation of the high-pressure Richarddalen Complex in NW Svalbard: insights from $^{40}Ar/^{39}Ar$ geochronology
21
  • Exhumation of the high-pressure Tsäkkok Lens, Swedish Caledonides: insights from the structural and white mica $^{40}Ar/^{39}Ar$ geochronological record
22
  • Experimental constraints on the relative stabilities of the two systems monazite-(Ce) – allanite-(Ce) – fluorapatite and xenotime-(Y) – (Y,HREE)-rich epidote – (Y, HREE)-rich fluorapatite, in high Ca and Na-Ca environments under P-T conditions of 200-1000 MPa and $450-750^{\circ}$C
23
  • Fluorapatitie-monazite-allanite relations in the Grängesberg apatite-iron oxide ore district, Bergslagen, Sweden
24
  • Garnet-quartz inclusion thermobarometry and Lu-Hf chronology detail the pre-ultra-high pressure metamorphic history of the Grapesvare Nappe, Scandinavian Caledonides
25
  • Geochronological constraints on Caledonian strike-slip displacement in Svalbard, with implications for the evolution of the Arctic