Zobrazeno 1 - 10
of 75
pro vyhledávání: '"David H. Elliot"'
Publikováno v:
Annals of Glaciology, Vol 64, Pp 181-186 (2023)
Over the last two decades, anomalous warming events have been observed in coastal Antarctic regions. While these events have been documented in the Ross Sea sector, the Antarctic interior is believed to have been buffered from warming. In this work,
Externí odkaz:
https://doaj.org/article/c593bdc284aa4035be341c18e790fef1
Autor:
David H. Elliot
Publikováno v:
New Zealand Journal of Geology and Geophysics. :1-16
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bad4d211b651185de6a05f953cad37db
https://doi.org/10.1080/00288306.2022.2114505
https://doi.org/10.1080/00288306.2022.2114505
Autor:
David H. Elliot, James W. Collinson
Publikováno v:
Antarctic Science. 34:172-179
The geology of the Schroeder Hill region near the head of the Shackleton Glacier, central Transantarctic Mountains, consists of Triassic Fremouw Formation and overlying Falla Formation strata intruded by Jurassic Ferrar Dolerite sills. At ‘Alfie’
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c68d29fd92cf86a2e2c1aeb7676bd36
https://doi.org/10.1017/s0954102022000013
https://doi.org/10.1017/s0954102022000013
Autor:
David H. Elliot
Publikováno v:
New Zealand Journal of Geology and Geophysics. 65:407-421
Eight landslides, seven certain and one possible, have been identified in the central Transantarctic Mountains and one at Carapace Nunatak, south Victoria Land. Four consist of Kirkpatrick Basalt l...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5c6bc830dca43adf3fa629f22bf146b3
https://doi.org/10.1080/00288306.2021.1929349
https://doi.org/10.1080/00288306.2021.1929349
Autor:
John L. Isbell, David H. Elliot
Publikováno v:
New Zealand Journal of Geology and Geophysics. 65:315-335
The Permian Mackellar Formation in the central Transantarctic Mountains is a fine-grained siliciclastic succession, which was deposited in a marine to brackish inland sea (Mackellar Sea) along the ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ecbb3a57387e2733e57edee7c2e4037e
https://doi.org/10.1080/00288306.2020.1868538
https://doi.org/10.1080/00288306.2020.1868538
Publikováno v:
Geological Society, London, Memoirs. 55:75-91
Preserved rocks in the Jurassic Ferrar Large Igneous Province consist mainly of intrusions, and extrusive rocks, the topic of this chapter, comprise the remaining small component. They crop out in a limited number of areas in the Transantarctic Mount
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6c70fac9f6a0ee4faa5847dd4259751
https://doi.org/10.1144/m55-2018-44
https://doi.org/10.1144/m55-2018-44
Autor:
David H. Elliot, Thomas Fleming
Publikováno v:
Geological Society, London, Memoirs. 55:93-119
The Lower Jurassic Ferrar Large Igneous Province consists predominantly of intrusive rocks, which crop out over a distance of 3500 km. In comparison, extrusive rocks are more restricted geographically. Geochemically, the province is divided into the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1a775ddd5d05136ef70674dc1b34738b
https://doi.org/10.1144/m55-2018-39
https://doi.org/10.1144/m55-2018-39
Autor:
W. B. Lyons, Byron J. Adams, Christopher B. Gardner, Melisa A. Diaz, David H. Elliot, Mike Cloutier
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::24a3364e4b01d9284923689e272a5499
https://doi.org/10.1130/abs/2020am-359713
https://doi.org/10.1130/abs/2020am-359713
Autor:
Thomas Fleming, David H. Elliot
Publikováno v:
Geological Society, London, Special Publications. 463:41-58
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c2bbf03f4997d2034ec8fc37bee6754
https://doi.org/10.1144/sp463.1
https://doi.org/10.1144/sp463.1
Permian–Triassic strata in the Transantarctic Mountains and West Antarctica carry a significant detrital component derived from a contemporaneous magmatic belt along the Gondwana margin. Hf- and O-isotope characteristics were determined for near-co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::84c42de5969a0062357d79eea540e1e1
