Zobrazeno 1 - 10
of 3 495
pro vyhledávání: '"W. Scholl"'
Autor:
Freitag, Matthias
Publikováno v:
Journal of East European Management Studies, 2004 Jan 01. 9(3), 333-337.
Externí odkaz:
https://www.jstor.org/stable/23280834
Autor:
Ruck
Publikováno v:
Archiv des öffentlichen Rechts, 1927 Jan 0152 (N.F. 13)(2), 274-276.
Externí odkaz:
https://www.jstor.org/stable/44301942
Autor:
Kreichgauer, P. Dam.
Publikováno v:
Anthropos, 1925 Sep 01. 20(5/6), 1157-1157.
Externí odkaz:
https://www.jstor.org/stable/40444944
Autor:
Tucker, Mark
Publikováno v:
The Duke Ellington Reader.
Externí odkaz:
https://doi.org/10.1093/oso/9780195054101.003.0022
Autor:
Kai Torsten Kanz
Publikováno v:
Gesnerus. 55:311-312
Akademický článek
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Publikováno v:
Global Encyclopedia of Public Administration, Public Policy, and Governance ISBN: 9783030662516
Global Encyclopedia of Public Administration, Public Policy, and Governance ISBN: 9783319318165
Global Encyclopedia of Public Administration, Public Policy, and Governance ISBN: 9783319318165
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::feb51c87f2206c4de0956c70695d1c86
https://doi.org/10.1007/978-3-030-66252-3_2407
https://doi.org/10.1007/978-3-030-66252-3_2407
Publikováno v:
Geosphere. 16:33-61
This article describes the regional effects of Cenozoic subduction along the outboard margin of the Northern Cordillera (Alaska, USA, and Western Canada), and thereby acquaints the reader with several chapters of the e-book Dynamic Geology of the Nor
Publikováno v:
SPIE Proceedings.
Fiber optic LAN transmission system reliability is ultimately determined by the reliability of the individual components in these systems. For LANs the optoelectronic components are predominantly GaAlAs LEDs and Si photodetectors for 830nm transmissi
Autor:
David W. Scholl
Publikováno v:
Geological Magazine. 158:104-117
The submerged forearcs of Pacific subduction zones of North and South America are underlain by a coastally exposed basement of late Palaeozoic to early Tertiary age. Basement is either an igneous massif of an accreted intra-oceanic arc or oceanic pla