Zobrazeno 1 - 10
of 72
pro vyhledávání: '"Wilfried Bauer"'
Publikováno v:
Energy Geoscience, Vol 5, Iss 1, Pp 100220- (2024)
The evaluation of reservoir quality was accomplished on the Late Paleocene to Early Eocene Narimba Formation in Bass Basin, Australia. This study involved combination methods such as petrophysical analysis, petrography and sedimentological studies, r
Externí odkaz:
https://doaj.org/article/877823a52a0143a2a97679df1110172a
Autor:
Peter Hallas, Wilfried Bauer
Publikováno v:
Geosciences, Vol 11, Iss 3, p 111 (2021)
The metamorphic sole, tectonically welded to the base of the Samail ophiolite in a supra-subduction system, is assumed to play the main role in strain accumulation during later thrusting onto the Arabian Plate (i.e., during obduction). The present st
Externí odkaz:
https://doaj.org/article/95c2f96de09c4d54b3e8b6ec787dd385
Publikováno v:
Polar Research, Vol 35, Iss 0, Pp 1-15 (2016)
The metamorphic basement of the Heimefrontfjella in western Dronning Maud Land (Antarctica) forms the western margin of the major ca. 500 million year old East African/East Antarctic Orogen that resulted from the collision of East Antarctica and grea
Externí odkaz:
https://doaj.org/article/641166ba14b34e8d936a2306f82ad10f
Autor:
Ian Lewis, Gisbert Weckbecker, Herbert A. Schmid, Steven W.J. Lamberts, Viktor Boerlin, Joost van der Hoek, Günter Bovermann, Lukas Oberer, Janos Pless, Nagarajan Chandramouli, Wilfried Bauer, Rainer Albert, Christian Bruns
Publikováno v:
CHIMIA, Vol 58, Iss 4 (2004)
A rational drug design approach involving transposition of functional groups from SRIF into a reduced size cyclohexapeptide template has led to the discovery of SOM230, a novel, stable cyclohexapeptide somatostatin mimic which exhibits unique high af
Externí odkaz:
https://doaj.org/article/d902474928ed4ac9b119a949dab0d176
The Saih Hatat Dome is a tectonic window in northeastern Oman with a NW-SE extension of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::419dc095ac28d6ac444e1c201391d7ee
https://doi.org/10.5194/egusphere-egu23-5179
https://doi.org/10.5194/egusphere-egu23-5179
The Indian Ocean Monsoon is one of the largest land-ocean coupled events on Earth. Its occurrence is not only of climatic importance but also has a considerable economic impact on the livelihood of people/countries within its coverage zone. The monso
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::241eb01778e1c5ae53cfad7ad3bbc3d4
https://doi.org/10.5194/egusphere-egu23-11475
https://doi.org/10.5194/egusphere-egu23-11475
Autor:
André Cravinho, Ana P. Jesus, Bruno Moreira, António Mateus, Bernhard Pracejus, Jorge Figueiras, Mathieu Benoit, Wilfried Bauer, Fernando Rocha
Publikováno v:
Economic Geology.
Despite the substantial amount of research on the Cretaceous Samail ophiolite in Oman, the factors controlling the size and metal endowment of the mafic-hosted, Cu-Au(-Zn-Ag) volcanogenic massive sulfide (VMS) deposits remain elusive. This work shows
Publikováno v:
Canadian Journal of Earth Sciences.
Subaerial rise of Earth's first continents took place 3.3–3.2 Ga years ago. This had significant influence on the ocean, atmosphere, and biosphere. Two important sedimentological consequences of continental emersion were (1) development of terrestr
Autor:
Andreas Scharf, Wilfried Bauer, Frank Mattern, Mohammed Al-Wardi, Bernhard Pracejus, Ivan Callegari, Gianluca Frijia, Daniel Moraetis
Publikováno v:
Geological Society, London, Memoirs. 54:67-103
The tectonic evolution of the Oman Mountains as of the Neoproterozoic begins with a major extensional event, the Neoproterozoic Abu Mahara rifting. It was followed by the compressional Nabitah event, still during the Neoproterozoic, in Oman but possi
Autor:
Ivan Callegari, Wilfried Bauer, Gianluca Frijia, Daniel Moraetis, Bernhard Pracejus, Andreas Scharf, Mohammed Al-Wardi, Frank Mattern
Publikováno v:
Geological Society, London, Memoirs. 54:11-47
This chapter provides comprehensive descriptions of 52 numbered formations/rock units of the Southeastern Oman Mountains, based on available literature. The oldest eight siliciclastic and carbonate formations are positioned below the ‘Hercynian’