Zobrazeno 1 - 5
of 5
pro vyhledávání: '"J R Ineson"'
Autor:
U Gregersen, P C Knutz, G K Pedersen, H Nøhr-Hansen, J R Ineson, L M Larsen, J R Hopper, J A Bojesen-Koefoed, G Dam, T Funck, J Hovikoski
The stratigraphy and the geological evolution of the West Greenland margin from the Labrador Sea to Baffin Bay in both the onshore and offshore areas are described. The primary data sets include seismic reflection surveys, wells, and outcrops. In add
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d132ec53ade6198be4afbf842affd87
https://doi.org/10.4095/321849
https://doi.org/10.4095/321849
Autor:
J. R. Ineson
Publikováno v:
Geological Society, London, Petroleum Geology Conference Series. 4:175-183
The Upper Hauterivian to Lower Albian strata of the Danish Central Trough comprise a varied succession of pelagic coccolith chalks, argillaceous chalks and marlstones with subordinate claystones. Where well developed, such as in the recently released
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::076478bf99e15ae089c52858f074aead
https://doi.org/10.1144/0040175
https://doi.org/10.1144/0040175
Autor:
J. R. Ineson
Publikováno v:
Sedimentology. 32:659-670
Isolated exotic blocks of late Jurassic age occur within an undeformed succession of marine Lower Cretaceous back-arc basin deposits on the west coast of James Ross Island, Antarctica. These flat, tabular slabs range up to 200 × 800 m in cross-secti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a16f7a2203727901b35d1ba4fb516a14
https://doi.org/10.1111/j.1365-3091.1985.tb00480.x
https://doi.org/10.1111/j.1365-3091.1985.tb00480.x
Publikováno v:
Geological Society, London, Special Publications. 16:219-229
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5bdb689fa172a2822a07761e64ca0573
https://doi.org/10.1144/gsl.sp.1984.016.01.17
https://doi.org/10.1144/gsl.sp.1984.016.01.17
Autor:
J. R. Ineson
Publikováno v:
Sedimentology. 36:793-819
The Cretaceous of west James Ross Island, Antarctica represents the proximal fill of a late Mesozoic back-arc basin that was probably initiated by oblique extension during the early development of the Weddell Sea. The succession records sedimentation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b0dc88c1829b67fe5a48a40b3c31a27
https://doi.org/10.1111/j.1365-3091.1989.tb01747.x
https://doi.org/10.1111/j.1365-3091.1989.tb01747.x