Zobrazeno 1 - 10
of 54
pro vyhledávání: '"W. Hieke"'
Autor:
W. Hieke
Publikováno v:
Marine Geology. 207:259-265
The 1960 bathymetric map of Pfannenstiel showed a submarine volcano west of the Peloponnesus which could not be confirmed by modern bathymetric surveys. Pfannenstiel's interpretation was supported by a report of flames on the sea in 1886. It is most
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc0e34d86f30485c9170230fc8cd6e88
https://doi.org/10.1016/j.margeo.2004.03.007
https://doi.org/10.1016/j.margeo.2004.03.007
Publikováno v:
Marine Geophysical Researches. 24:279-310
In order to understand the structure and evolution of the Mediterranean Ridge accretionary complex, it is necessary to understand the structure and history of its foreland. The Ionian Abyssal Plain is one of the varying types of foreland. The state o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28d39f61b6c60326d17431c96e069bcd
https://doi.org/10.1007/s11001-004-2173-z
https://doi.org/10.1007/s11001-004-2173-z
Autor:
Friedrich Werner, W. Hieke
Publikováno v:
Sedimentary Geology. 135:205-218
A thick mud turbidite, up to 24 m in thickness (termed the “Augias turbidite”) is decribed from the Ionian and Sirte Abyssal Plains and the adjacent slopes of the Calabrian Rise and the Mediterranean Ridge. The material of the megaturbidite is de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::80f649311520bc757347f4f05d8c1a7f
https://doi.org/10.1016/s0037-0738(00)00072-5
https://doi.org/10.1016/s0037-0738(00)00072-5
Autor:
W. Hieke
Publikováno v:
Sedimentary Geology. 135:89-98
Echosounding and SCS records from the Ionian and Sirte Abyssal Plains show, below the Holocene Augias megaturbidite, two additional thick transparent layers which by analogy are interpreted as turbidites. Estimated thicknesses are 10 and 35 m (upper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c33d7f9968111e5648e6ea3652e45c8d
https://doi.org/10.1016/s0037-0738(00)00065-8
https://doi.org/10.1016/s0037-0738(00)00065-8
Publikováno v:
Marine Geology. 132:113-129
This paper presents a “state of knowledge” of the Antaeus/Pan di Zucchero field (the summit area of the Mediterranean Ridge) including morphological, geological, geophysical and micropaleontological data. The area is characterized by elongated el
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f8d8c7e9dd40debd726888b1c5bbd7a
https://doi.org/10.1016/0025-3227(95)00156-5
https://doi.org/10.1016/0025-3227(95)00156-5
Publikováno v:
Marine Geology. 132:63-93
During Meteor Cruise 25 4 in 1993, a multibeam bathymetric (Hydrosweep) survey was carried out on the Mediterranean Ridge in an area south of Crete (comprising the original Olimpi and Prometheus-2 mud diapir fields). The morphology is characterized b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::639f29b5efabaccc4f59f02a7e227ac2
https://doi.org/10.1016/0025-3227(95)00154-9
https://doi.org/10.1016/0025-3227(95)00154-9
Publikováno v:
Earth and Planetary Science Letters. 109:493-504
A mud breccia has been repeatedly cored from four mud diapir fields located on the crest of the Mediterranean Ridge. This breccia is composed of subrounded clasts supported by a clay-rich matrix and ranges in age from Cretaceous to early Miocene. Sed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb74324df785120c2a0f0be15a9c8fd3
https://doi.org/10.1016/0012-821x(92)90109-9
https://doi.org/10.1016/0012-821x(92)90109-9
Autor:
C. Müller, Alina Polonia, W. Hieke, G. A. Dehghani, Maria Bianca Cita, Angelo Camerlenghi, L. Mirabile, Nicoletta Fusi, H. B. Hirschleber
In previous publications, the relationship between the Sirte Abyssal Plain as foreland and the Mediterranean Ridge as accretionary complex was considered to be simple: the foreland is undeformed, the accretionary complex consumes the foreland, the Me
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::127be2d76ed6c229437482ecfb9be4f3
http://hdl.handle.net/10281/12481
http://hdl.handle.net/10281/12481
Autor:
Judith A McKenzie, Alastair H. F. Robertson, R. Sartori, W. Hieke, Floyd W. McCoy, Georges Mascle, Jean-Pierre Réhault
Publikováno v:
Proceedings of the Ocean Drilling Program, 107 Scientific Results
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3266b3a8de2bdd29c06f0eb0151f3dc4
https://doi.org/10.2973/odp.proc.sr.107.179.1990
https://doi.org/10.2973/odp.proc.sr.107.179.1990