Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Ken J. Woolfe"'
Publikováno v:
Australian Journal of Earth Sciences. 51:665-683
The Great Barrier Reef represents the largest modern example of a mixed siliciclastic–carbonate system. The Burdekin River is the largest source of terrigenous sediment to the lagoon and is therefore an ideal location to investigate regional patter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::236056854a73d64251db00c24deb44c7
https://doi.org/10.1111/j.1400-0952.2004.01083.x
https://doi.org/10.1111/j.1400-0952.2004.01083.x
Publikováno v:
International Journal of Coal Geology. 51:215-235
Selected Tertiary coals from the Zeya–Buryea Basin, Far Eastern Russia, were investigated for aspects of their coal type, rank, depositional environment and post-depositional history. The coals have been examined in outcrop (lithotype logging), mic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9876435f0c79fa6c6cd51cb05895897f
https://doi.org/10.1016/s0166-5162(02)00100-3
https://doi.org/10.1016/s0166-5162(02)00100-3
Publikováno v:
Sedimentology. 49:603-621
Thick sequences of sediment surround the Whitsunday Islands on the middle shelf of the Great Barrier Reef (GBR) Platform. Much of this sediment is siliciclastic material deposited since the sea-level highstand at around 6·5 ka. This raises a mass ba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c67012e1fb6af9abc6ef32b2d1e2775
https://doi.org/10.1046/j.1365-3091.2002.00464.x
https://doi.org/10.1046/j.1365-3091.2002.00464.x
Publikováno v:
Sedimentology. 48:811-835
The Great Barrier Reef (GBR) shelf contains a range of coral reefs on the highly turbid shallow inner shelf, where interaction occurs with terrigenous sediments. The modern hydrodynamic and sedimentation regimes at Paluma Shoals, a shore-attached ‘
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07122bd202dad60f36b48fd967390e03
https://doi.org/10.1046/j.1365-3091.2001.00396.x
https://doi.org/10.1046/j.1365-3091.2001.00396.x
Publikováno v:
Computers & Geosciences. 27:597-600
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa869cea0011dc5cf49b303fed2633ac
https://doi.org/10.1016/s0098-3004(00)00147-3
https://doi.org/10.1016/s0098-3004(00)00147-3
Publikováno v:
Journal of the Geological Society. 158:427-438
A zone of active seabed erosion has been identified in the northwestern Rockall Trough using seismic reflection profiles and cores. The region from George Bligh Bank to Rockall Bank has been subject to vigorous bottom-current activity, for at least t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::30fa17a19cab2de842b18525b2085ae1
https://doi.org/10.1144/jgs.158.3.427
https://doi.org/10.1144/jgs.158.3.427
Publikováno v:
Computers & Geosciences. 27:351-355
Regional palaeocurrent datasets frequently are stored in multiple files, whereby each file contains observations from a specific location, formation and suite of sedimentary structures. Interpretative analysis of such data often involves the graphica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6cf1be02e2694f49f3b7f2bfd2ae3e22
https://doi.org/10.1016/s0098-3004(00)00107-2
https://doi.org/10.1016/s0098-3004(00)00107-2
Autor:
Peter Barrett, Jaap J.M. van der Meer, Sandra Passchier, Fabio Florindo, Christopher R. Fielding, C Percy Strong, Leonardo Sagnotti, Alistair Dunn, Stuart Henrys, C. Bücker, P.N. Webb, Andrew P. Roberts, David K. Watkins, Tim R Naish, Gary S. Wilson, William C. McIntosh, Reed P. Scherer, M. J. Hannah, Frank Niessen, C. Atkins, M. Claps, Franco M Talarico, Fred Davey, Thomas Wonik, David M. Harwood, Steven M Bohaty, Lawrence A. Krissek, Ken J. Woolfe, M. Lavelle, Gavin B. Dunbar, Ross D. Powell, Giuliana Villa, Kenneth L. Verosub
Publikováno v:
ResearcherID
Nature, 413, 719-723. Nature Publishing Group
Nature, 413, 719-723. Nature Publishing Group
Between 34 and 15 million years (Myr) ago, when planetary temperatures were 3–4 °C warmer than at present and atmospheric CO2 concentrations were twice as high as today1, the Antarctic ice sheets may have been unstable2, 3, 4, 5, 6, 7. Oxygen isot
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::27d3280f96c8118cf3ecfed1b3ee79c7
https://dare.uva.nl/personal/pure/en/publications/orbitally-induces-oscillations-in-the-east-antarctic-ice-sheet-at-the-oligocenemiocene-boundary(0a1ae030-2c73-42c7-a8f4-148b0c1072fc).html
https://dare.uva.nl/personal/pure/en/publications/orbitally-induces-oscillations-in-the-east-antarctic-ice-sheet-at-the-oligocenemiocene-boundary(0a1ae030-2c73-42c7-a8f4-148b0c1072fc).html
Publikováno v:
Sedimentary Geology. 136:59-69
A simple model is developed to infer flood-tide dispersal of silt during fair-weather conditions from spatial grain size variation of mixed carbonate/siliciclastic silt on the bed of Nara Inlet, a 3 km long shallow, tropical embayment on the mid-shel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95a01a7b55e2ba6ecf2326609d61b798
https://doi.org/10.1016/s0037-0738(00)00086-5
https://doi.org/10.1016/s0037-0738(00)00086-5
Publikováno v:
Australian Journal of Earth Sciences. 47:689-694
In broad terms, fluvial systems can be considered as comprising two basic geomorphologic features, a channel and its floodplain (overbank), each of which may accumulate sediment or undergo erosion. The sedimentary relationships between channels and f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dc6fe9c562d05be41f12c4adcecf14e0
https://doi.org/10.1046/j.1440-0952.2000.00801.x
https://doi.org/10.1046/j.1440-0952.2000.00801.x