Zobrazeno 1 - 10
of 224
pro vyhledávání: '"Surlyk, Finn"'
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 10, Pp 13-16 (2006)
Externí odkaz:
https://doaj.org/article/beee871ec0ce40bc92110639cd743811
Autor:
Ineson, Jon R., Buchardt, Bjørn, Lassen, Susanne, Rasmussen, Jan A., Schiøler, Poul, Schovsbo, Niels H., Sheldon, Emma, Surlyk, Finn
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 10, Pp 9-12 (2006)
Externí odkaz:
https://doaj.org/article/5bbc5dd73f7242b4b3973407d344cd88
Autor:
Vosgerau, Henrik, Alsen, Peter, Carr, Ian D., Therkelsen, Jens, Stemmerik, Lars, Surlyk, Finn
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 05, Pp 09-18 (2004)
Middle–Late Jurassic rifting in East Greenland was marked by westwards tilting of wide fault blocks bounded by major N–S-trending east-dipping synthetic faults. The syn-rift successions thicken westwards towards the faults and shallow marine sand
Externí odkaz:
https://doaj.org/article/f5c0ac7bca9a4dd68f03c4da11e38301
Autor:
Therkelsen, Jens, Surlyk, Finn
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 05, Pp 19-29 (2004)
A new lithostratigraphic unit, the Bristol Elv Formation, is erected in this paper. It is only known from Traill Ø, East Greenland, where it unconformably overlies Triassic redbeds of the Fleming Fjord Formation and is overlain by lithologically sim
Externí odkaz:
https://doaj.org/article/8d6964a32de544e8b2cb65d7d5d2666a
Autor:
Alsen, Peter, Surlyk, Finn
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 05, Pp 31-49 (2004)
A Middle – lower Upper Jurassic sandstone-dominated succession, more than 550 m thick, with mudstone intercalations in the middle part is exposed in Bjørnedal on Traill Ø, North-East Greenland. A number of ammonite assemblages have been found, ma
Externí odkaz:
https://doaj.org/article/d78f6cfd92524f1d8f37c3ba67a8691d
Autor:
Surlyk, Finn, Donovan, Desmond T.
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 01, Pp 555-583 (2003)
The Jurassic succession of the island of Bornholm in the Baltic Sea includes the Hettangian – lowermost Pliensbachian Rønne Formation, the Lower Pliensbachian Hasle Formation, the Upper Pliensbachian – (?)Lower Aalenian Sorthat Formation and the
Externí odkaz:
https://doaj.org/article/22b46557f4cf401e915f90bb9787543f
Autor:
Surlyk, Finn
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 01, Pp 657-722 (2003)
The Late Palaeozoic – Mesozoic extensional basin complex of East Greenland contains a record of deposition during a period of Rhaetian – Early Bajocian thermal subsidence, the onset of riftingin the Late Bajocian, its growth during the Bathonian
Externí odkaz:
https://doaj.org/article/94f13b630f504d3681a63699627b5041
Autor:
Surlyk, Finn, Frandsen, Nils
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 01, Pp 543-554 (2003)
A Sinemurian mudstone-dominated succession was exposed until recently in the Gantofta quarry in Skåne, southern Sweden. The deposits are placed in the Döshult and Pankarp Members of the Sinemurian–Aalenian Rya Formation. Similar facies of the sam
Externí odkaz:
https://doaj.org/article/3f3ec6b695ae4211b8c2558c6f36bdf0
Autor:
Surlyk, Finn, Ineson, Jon I.
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 01, Pp 009-020 (2003)
The Jurassic succession of Denmark is largely confined to the subsurface with the exception of exposures on the island of Bornholm in the Baltic Sea. In East Greenland, in contrast, the Jurassic is extensively exposed. Comparison of basin evolution i
Externí odkaz:
https://doaj.org/article/6591840be3a74ba5ab952eb53b7ec060
Publikováno v:
Geological Survey of Denmark and Greenland Bulletin, Vol 01, Pp 145-216 (2003)
A complete updated and revised lithostratigraphic scheme for the Jurassic succession of the onshore and offshore Danish areas is presented together with an overview of the geological evolution. The lithostratigraphies of Bornholm, the Danish Basin an
Externí odkaz:
https://doaj.org/article/6f768178677a43fda3285bcdce774bef