Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Dirk Liss"'
Autor:
Federico Ferrari, Lisa Hammond, Uta Ulrich, Stefan Reichenberger, Ludovic Loiseau, Jutta Agert, Jenny Kreuger, Benedict Miles, Florian Hegler, Dirk Liss, Richard Gibson, Wiebke Tüting, Russell L. Jones, Ton van der Linden, Horst Staudenmaier, Michael Stemmer, Wolfram König, Nicole Baran, Robin Sur, Arnaud Boivin, Anne Louise Gimsing, Anton Poot, Andy Newcombe, Annette E. Rosenbom, Graham Reeves, Andy Massey, Laurent Monrozies, Andreas Schwen
Publikováno v:
JOURNAL OF CONSUMER PROTECTION AND FOOD SAFETY
JOURNAL OF CONSUMER PROTECTION AND FOOD SAFETY, 2019, 14, pp.1-93. ⟨10.1007/s00003-019-01211-x⟩
JOURNAL OF CONSUMER PROTECTION AND FOOD SAFETY, 2019, 14, pp.1-93. ⟨10.1007/s00003-019-01211-x⟩
Groundwater monitoring is recommended as a higher-tier option in the regulatory groundwater assessment of plant protection products in the European Union. However, to date little guidance has been provided on study designs. SETAC EMAG-Pest GW, a grou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::640c9094130a141a4d37b8ed84656562
https://hal.archives-ouvertes.fr/hal-02380958
https://hal.archives-ouvertes.fr/hal-02380958
Publikováno v:
Journal of the Geological Society. 161:927-938
A large-scale palaeomagnetic study (125 specimens from 88 sampling localities) has been carried out on the Whin Sill complex and its associated dykes in northern England. The dominant carrier of remanent magnetization of the doleritic rocks is relati
Publikováno v:
Geophysical Research Letters. 33
[1] Coe-Modified Thellier (CMT) and Microwave (MW) paleointensity experiments were conducted on samples from the multi-phase late Carboniferous (ca. 301 Ma) to early Permian (ca. 270 Ma) Great Whin Sill complex. Statistically comparable results were
Publikováno v:
Geology. 30:715
Ropy flow structures that form in dikes and sills are very similar to ropy lava structures (pahoehoe), but are of intrusive origin. They are unusual among magma-flow indicators in that they provide a frozen record of the magma flow. Our observations