Zobrazeno 1 - 10
of 16
pro vyhledávání: '"M. R. Dobson"'
Publikováno v:
Geological Society, London, Special Publications. 129:43-66
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::69feb55682cff93453ecca8389beea76
https://doi.org/10.1144/gsl.sp.1998.129.01.04
https://doi.org/10.1144/gsl.sp.1998.129.01.04
Autor:
R. J. Whittington, M. R. Dobson
Publikováno v:
Geological Society, London, Special Publications. 62:291-311
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6b8e8e16d89ad36ae1bd31c1c3bfe25
https://doi.org/10.1144/gsl.sp.1992.062.01.23
https://doi.org/10.1144/gsl.sp.1992.062.01.23
Publikováno v:
Basin Research. 3:99-117
Shell-Agip 35/13–1 well drilled 2445 m of Tertiary sediments in the Main Porcupine Basin situated offshore west of Ireland. Early Tertiary sediments and microfossils indicate a major cycle from deep-sea to marginal marine and terrestrial palaeoenvi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b06f7169cf64abb83126dc31aedb07f
https://doi.org/10.1111/j.1365-2117.1991.tb00142.x
https://doi.org/10.1111/j.1365-2117.1991.tb00142.x
Autor:
I. R. Westlake, M. R. Dobson
Publikováno v:
Atlas of Deep Water Environments ISBN: 9789401045391
Flysch, of Aptian to Turonian age, crops out south of the Yarlung-Zangbo (Brahmaputra) river, in southern Tibet between the Gangdise batholith to the north and the Xigaze ophiolite to the south; the latter is part of the Indus suture zone that can be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8fab36d62d6577f394c9e414a9c302a6
https://doi.org/10.1007/978-94-011-1234-5_12
https://doi.org/10.1007/978-94-011-1234-5_12
Publikováno v:
Geo-Marine Letters. 2:23-30
Transgressive Upper Cretaceous Chalk terminates (between SW Wales and SE Ireland) at approximately latitude 52°N as thinly bedded marginal facies; while the Tertiary sequences, previously considered to extend uninterrupted into both the South Celtic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3951510ddd1659620e4262b00308230b
https://doi.org/10.1007/bf02462796
https://doi.org/10.1007/bf02462796
Publikováno v:
Journal of the Geological Society. 132:611-621
Dredged carbonates from the margins of Rockall Trough mostly represent hard grounds made up of outer shelf benthonic skeletal assemblages and pelagic ooze. Chertification and occasional iron impregnation either as a crust or dominant association, are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42c41d4b7ee873c6108aebc6f619ecb3
https://doi.org/10.1144/gsjgs.132.6.0611
https://doi.org/10.1144/gsjgs.132.6.0611
Autor:
M. P. Tate, M. R. Dobson
Publikováno v:
Geological Society, London, Special Publications. 39:309-334
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::338e2747f774d3b6db18eb414f0a5050
https://doi.org/10.1144/gsl.sp.1988.039.01.28
https://doi.org/10.1144/gsl.sp.1988.039.01.28
Autor:
M. R. Dobson, R. J. Whittington
Publikováno v:
Journal of the Geological Society. 136:243-249
A gravity low immediately E of Dublin is interpreted as an Upper Palaeozoic to Cenozoic basin on the basis of seismic reflection profiles and direct sampling evidence. Maximum thickness of the sediment fill may exceed 4 km. It is considered to consis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bddfcb49fdc3414abb2a012425bbea52
https://doi.org/10.1144/gsjgs.136.2.0243
https://doi.org/10.1144/gsjgs.136.2.0243
Autor:
M. R. Dobson, D. C. Pendlebury
Publikováno v:
Scottish Journal of Geology. 11:315-332
Synopsis A bathymetric, sediment and macrofaunal analysis has been made of the eastern Malin Sea off the west coast of Scotand using shallow seismic, side-scan sonar, and the results from 53 bottom samples. The distributions of the sediment types and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4e3ec6cb3a8605c84d475081799d7655
https://doi.org/10.1144/sjg11040315
https://doi.org/10.1144/sjg11040315
Publikováno v:
Scottish Journal of Geology. 15:217-230
Synopsis Marine studies in the Firth of Lorne have revealed the presence of heterogeneous basement and a constricted yet complex sedimentary basin. A total of forty three dive, dredge and borehole samples has allowed both the basement, which consists
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9d8fab041b8ca9647363794cb70e2773
https://doi.org/10.1144/sjg15030217
https://doi.org/10.1144/sjg15030217