Zobrazeno 1 - 10
of 13
pro vyhledávání: '"H. B. Hirschleber"'
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:
Takaya Iwasaki, Shuichi Kodaira, Rolf Mjelde, N. Tomita, A. Goldschmidt-Rokita, R.K. Hassan, T. Kanazawa, Hideki Shimamura, H. B. Hirschleber, Markvard A. Sellevoll
Publikováno v:
Journal of Geodynamics. 22:189-206
A detailed model for the continent/ocean transition of the Lofoten passive volcanic margin, N. Norway, has been obtained by use of seismic wide-angle data from Ocean Bottom Seismographs (OBSs), combined with results from other geophysical data. The O
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0238be22c777c1208307e740a5e0fa72
https://doi.org/10.1016/0264-3707(96)00016-6
https://doi.org/10.1016/0264-3707(96)00016-6
Autor:
Shuichi Kodaira, Hideki Shimamura, Martin Bellenberg, H. B. Hirschleber, Toshihiko Kanazawa, Takaya Iwasaki
Publikováno v:
Geophysical Journal International. 124:724-740
SUMMARY In 1988, an extensive seismic refraction and wide-angle reflection study was performed at the Lofoten passive continental margin, off northern Norway, by using three-component ocean bottom seismographs. The Lofoten margin was formed by contin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1bb1c91480b10d8f9121babb1eece7fb
https://doi.org/10.1111/j.1365-246x.1996.tb05634.x
https://doi.org/10.1111/j.1365-246x.1996.tb05634.x
Autor:
T. Kanazawa, H. Krahn, A. Goldschmidt-Rokita, S. Tomita, H. B. Hirschleber, Takaya Iwasaki, Hideki Shimamura, Jens Hartmann, Shuichi Kodaira
Publikováno v:
Geophysical Journal International. 121:907-924
SUMMARY In 1988, an extensive geophysical experiment was performed on the Lofoten passive continental margin, which was formed by the continental break-up between Greenland and northern Norway at 58 Ma. The geological units of the outer Lofoten margi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e4260878b719ffd0953d5f82e3c0b52
https://doi.org/10.1111/j.1365-246x.1995.tb06447.x
https://doi.org/10.1111/j.1365-246x.1995.tb06447.x
Autor:
Takaya Iwasaki, T. Kanazawa, Hideki Shimamura, Shuichi Kodaira, Markvard A. Sellevoll, Rolf Mjelde, H. B. Hirschleber
Publikováno v:
Journal of Physics of the Earth. 43:729-745
This study presents a 500-km-long crustal transect across the Lofoten volcanic passive continental margin, N. Norway, by compiling the results of two successive Ocean Bottom Seismographic (OBS) experiments performed in 1988. The OBS profiles were acq
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eb013a8aaadac7caf858070818ec8fd2
https://doi.org/10.4294/jpe1952.43.729
https://doi.org/10.4294/jpe1952.43.729
Autor:
Markvard A. Sellevoll, Hideki Shimamura, Takaya Iwasaki, Knut J. F. Hansch, T. Kanazawa, H. B. Hirschleber, Andreas Goldschmidt-Rokita
Publikováno v:
Marine Geophysical Researches. 16:201-224
The Cenozoic margins of the Norwegian-Greenland Sea offer ideal conditions for passive margin studies. A series of structural elements, first observed on these margins, led to the concept of volcanic passive margins. Questions still remain about the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::306296bd62a49bf09c82c5a086081645
https://doi.org/10.1007/bf01237514
https://doi.org/10.1007/bf01237514
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
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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During the Volcanic Island Clastic Apron Project (VICAP), south of the Canary Islands, a total of 700 line-km multichannel seismic profiles were acquired. Two prominent reflectors (A and C) were observed alternately: A is the top of the volcanic apro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5ada47965a8049830e2854d4f4ed654e
http://hdl.handle.net/10261/171652
http://hdl.handle.net/10261/171652
Autor:
Rolf Mjelde, Hideki Shimamura, Markvard A. Sellevoll, Shuichi Kodaira, Eivind Berg, H. B. Hirschleber
Publikováno v:
Proceedings.
The continental break-up between Norway and Greenland occurred in late Paleocene / early Eocene, and was associated with an intensive volcanisim along the margin. At a passive continental margin the whole process of crustal evolution is generally ret
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4cf20af2c0448a42a49b60d41b0db60e
https://doi.org/10.3997/2214-4609.201409544
https://doi.org/10.3997/2214-4609.201409544
Publikováno v:
Tectonophysics. 128:209-228
During the Meteor 66 cruise in the offshore areas surrounding Jutland in November 1983, seismic reflection and refraction measurements were made. A streamer, Ocean Bottom Seismographs, and land stations were deployed, which enabled both vertical-inci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::559329cfa43a2ec0581e254fa5f72ea2
https://doi.org/10.1016/0040-1951(86)90294-5
https://doi.org/10.1016/0040-1951(86)90294-5