Zobrazeno 1 - 6
of 6
pro vyhledávání: '"H. Mark Van Buren"'
Publikováno v:
Deep-Water Turbidite Systems
The open-ocean carbonate slope north of Little Bahama Bank consists of a relatively steep (4°) upper slope between water depths of 200 and 900 m, and a more gentle (1–2°) lower slope between depths of 900 and 1300+ m. The upper slope is dissected
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::09f678f2d17a4ac395f9a08ee90f0f64
https://doi.org/10.1111/j.1365-3091.1984.tb01956.x
https://doi.org/10.1111/j.1365-3091.1984.tb01956.x
Autor:
Henry T. Mullins, H. Mark Van Buren
Publikováno v:
Geo-Marine Letters. 1:225-231
Interpretation of seismic reflection data reveal evidence of a Cenozoic fault (Walkers Cay Fault) north of Little Bahama Bank. This fault strikes N15–30°E, perpendicular to the adjacent bank margin and offsets a late Oligocene reflector by as much
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b460f0f25805493c05d2e19a03c6a522
https://doi.org/10.1007/bf02462438
https://doi.org/10.1007/bf02462438
Publikováno v:
SEPM Journal of Sedimentary Research. 51
Deep-water, ahermatypic coral mounds are present at water depths of 1,000-1,300 m on the lower slope north of Little Bahama Bank. The mounds are patchily distributed over a minimum area of 2,500 km2 and typically display 5-40 m of relief above the su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f34bd3d396369e188e4451ef04fe68f9
https://doi.org/10.1306/212f7dfb-2b24-11d7-8648000102c1865d
https://doi.org/10.1306/212f7dfb-2b24-11d7-8648000102c1865d
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