Zobrazeno 1 - 10
of 19
pro vyhledávání: '"D. E. Karig"'
Autor:
Hüseyin Kozlu, D. E. Karig
Publikováno v:
Journal of the Geological Society. 147:1023-1034
The Marao region of Turkey includes the Anatolian-Arabian-African triple junction. The African-Arabian margin is marked by left-lateral transtension along the Dead Sea (Kara Su) rift. Motion on the Anatolian-Arabian boundary is partitioned between th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2396825a77bea2afcd4a927f18db483c
https://doi.org/10.1144/gsjgs.147.6.1023
https://doi.org/10.1144/gsjgs.147.6.1023
Autor:
Neil Lundberg, D. E. Karig
Publikováno v:
Journal of Geophysical Research. 95:9099
Deformation in the toe of the Nankai accretionary prism of SW Japan occurs not only by displacement on seismically defined thrust faults but also by diffuse thickening, shortening, and porosity loss. Sediments recovered from this setting are only ver
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::acf4b71581015183f77c5b612008c62e
https://doi.org/10.1029/jb095ib06p09099
https://doi.org/10.1029/jb095ib06p09099
Autor:
D. E. Karig, R. J. Knipe, J. K. Leggett, Jean-Paul Cadet, R. von Huene, Neil Lundberg, C. J. Bray
Publikováno v:
Geological Society, London, Special Publications. 28:593-609
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ebcb3088d8a087a44c441e99b5ff3c9
https://doi.org/10.1144/gsl.sp.1987.028.01.39
https://doi.org/10.1144/gsl.sp.1987.028.01.39
Autor:
R. W. Kay, D. E. Karig
Publikováno v:
Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. 301:233-251
The evolution of the continents and of continental crust is strongly dependent on the trajectory of the sedimentary cover on the descending oceanic lithosphere at arc systems. Although direct calculations of accretion are not reliable, indirect evide
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bfc7dc2b13bc26b2af419ee0bc991674
https://doi.org/10.1098/rsta.1981.0108
https://doi.org/10.1098/rsta.1981.0108
Autor:
D. E. Karig
Publikováno v:
The Journal of Geology. 88:27-39
Observations of high-pressure metamorphic rocks occurring as blocks (knockers) and as thrust sheets intercalated into non-metamorphosed rocks in subduction complexes have led to models of material transport within accretionary prisms having large-sca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a33feb812a739df8331c4e563019c18d
https://doi.org/10.1086/628471
https://doi.org/10.1086/628471
Publikováno v:
Journal of Geophysical Research. 81:6281-6291
Seismic zones beneath consuming plate margins have a flattened upper section, which has been attributed to the growth of the accreted material beneath the inner trench slope. Comparison of well-studied seismic zones shows that the width of this flatt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f835439206c6367c2cd6cf34cc49a4d
https://doi.org/10.1029/jb081i035p06281
https://doi.org/10.1029/jb081i035p06281
Autor:
D. E. Karig
Publikováno v:
Geological Society, London, Special Publications. 10:563-576
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::784072924b8ca2dcd7a60a65a8e74990
https://doi.org/10.1144/gsl.sp.1982.010.01.37
https://doi.org/10.1144/gsl.sp.1982.010.01.37
Autor:
C. J. Bray, D. E. Karig
Publikováno v:
Journal of Geophysical Research: Solid Earth. 90:768-778
Rapid dewatering, largely through loss of porosity, is one of the most striking changes affecting deformed sediments in accretionary prisms. Analysis of porosity from sample and seismic data confirms that porosity in accretionary prisms is significan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af2f8bf41070d83a82990617fa81bd8b
https://doi.org/10.1029/jb090ib01p00768
https://doi.org/10.1029/jb090ib01p00768
