Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Richard Vandenberg"'
Publikováno v:
Environmental Geochemistry and Health.
Freeze-drying is widely used in geochemical laboratories for preparing wet solid environmental samples such as sediments and soils before being analyzed for their contents and states of various metal elements and labile organic components that may be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08dab1708f0a796e69fec39b18eb2307
https://doi.org/10.1007/s10653-023-01594-9
https://doi.org/10.1007/s10653-023-01594-9
Publikováno v:
arktos. 6:39-52
Rock materials from three Arctic wells drilled through Middle-Upper Devonian basinal mudrocks between 1969 and 1973 were surveyed with the energy-dispersive X-ray fluorescence tool (ED-XRF) Bruker Tracer IV-SD™. The logs of major oxides acquired fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::20f57db0b6ec55d755c85b4b9cad8aef
https://doi.org/10.1007/s41063-020-00074-z
https://doi.org/10.1007/s41063-020-00074-z
Autor:
Annique van der Boon, Andrew J. Biggin, Daniele Thallner, Mark W. Hounslow, Richard Bono, Jerzy Nawrocki, Krystian Wójcik, Mariusz Paszkowski, Peter Königshof, Tim de Backer, Pavel Kabanov, Sofie Gouwy, Richard VandenBerg, Anne-Christine Da Silva
The Devonian has long been a problematic period for paleomagnetism. Devonian paleomagnetic data are generally difficult to interpret and have complex partial or full overprints– problems that arise in data obtained from both sedimentary and igneous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5847703c7cfbf2612f9e3b5f40b1ca19
http://hdl.handle.net/10852/94386
http://hdl.handle.net/10852/94386
Autor:
Sofie Gouwy, Mark W. Hounslow, Annique van der Boon, Daniele Thallner, Peter Königshof, Tim de Backer, Kristyan Wójcik, Pavel Kabanov, Andrew J. Biggin, Mariusz Paszkowski, Jerzy Nawrocki, Richard K. Bono, Richard Vandenberg
The Devonian has long been a problematic era for paleomagnetism. Devonian data are generally difficult to interpret and have complex partial or full overprints. These problems arise from paleomagnetic data obtained from both sedimentary and igneous r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::39a4890b245d6e5e6ac0e5bd538011ae
https://doi.org/10.5194/egusphere-egu21-9035
https://doi.org/10.5194/egusphere-egu21-9035
Autor:
Jerzy Nawrocki, Pavel Kabanov, Peter Königshof, Andrew J. Biggin, Richard Vandenberg, Mark W. Hounslow, Annique van der Boon, Tim de Backer, Sofie Gouwy, Mariusz Paszkowski, Kristyan Wójcik, Daniele Thallner, Richard K. Bono
The global polarity time scale (GPTS) is relatively unconstrained for the Paleozoic, particularly the Devonian. Constraining the GPTS and reversal frequency for the Devonian is crucial for the understanding of the behaviour of Earth’s magnetic fiel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8fb6507c25698f5aae4599138398209e
https://doi.org/10.5194/egusphere-egu21-9036
https://doi.org/10.5194/egusphere-egu21-9036
Publikováno v:
arktos. 6:53-54
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bcf85ffc043fbd6ae8e1fcfdf42f5103
https://doi.org/10.1007/s41063-020-00076-x
https://doi.org/10.1007/s41063-020-00076-x