Zobrazeno 1 - 10
of 972
pro vyhledávání: '"M. Gahagan"'
Autor:
Cazden, Courtney B.
Publikováno v:
Language in Society, 1973 Apr 01. 2(1), 147-151.
Externí odkaz:
https://www.jstor.org/stable/4166711
Publikováno v:
Marine Geophysical Research. 40:1-16
The passive margin and ocean crust of the Enderby Basin, East Antarctica preserves a record of the breakup of East Gondwana. Using a suite of public domain geophysical data, we have examined and described the crustal morphology of the basin. Based on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eeca0f0581149603f798fadd104317dd
https://doi.org/10.1007/s11001-018-9356-5
https://doi.org/10.1007/s11001-018-9356-5
Publikováno v:
Gondwana Research. 34:16-28
The oldest portions of the Indian Ocean formed via the breakup of Gondwana and the subsequent fragmentation of East Gondwana. We present a constrained plate model for this early Indian Ocean development for the time period from Gondwana Breakup until
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::032b0158e4afd7517199d003b218ebb8
https://doi.org/10.1016/j.gr.2016.02.010
https://doi.org/10.1016/j.gr.2016.02.010
Autor:
Gold, Natalie1,2 (AUTHOR) natalie.gold@veriangroup.com, Cornel, Pieter1 (AUTHOR), Zhuo, Shi1 (AUTHOR), Thornton, Katie1 (AUTHOR), Riddle, Rupert1 (AUTHOR), McPhedran, Robert3 (AUTHOR)
Publikováno v:
International Journal of Market Research. Sep2024, Vol. 66 Issue 5, p650-673. 24p.
Publikováno v:
Annual Review of Earth and Planetary Sciences. 41:767-793
The Scotia arc is the eastward-closing loop of mountains and locally emergent submarine ridges extending from the southernmost Andes through the active South Sandwich volcanic arc to the Antarctic Peninsula. Its origins lie in the Jurassic initial fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e53b8fbd6387ffac149e9fd2225a24e3
https://doi.org/10.1146/annurev-earth-050212-124155
https://doi.org/10.1146/annurev-earth-050212-124155
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f0da372cfab9f73513011490248a46c
https://doi.org/10.1130/abs/2016am-279366
https://doi.org/10.1130/abs/2016am-279366
Publikováno v:
Geological Society, London, Memoirs. 35:61-77
The Palaeozoic motion of the future Arctic continents is presented in the animation found in the accompanying CD-ROM. The animation shows snapshots of the motion of the tectonic blocks from 550 to 250 Ma in 3 million year steps. The locations of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::029ed543758565884141ea4809caefa3
https://doi.org/10.1144/m35.5
https://doi.org/10.1144/m35.5
Autor:
Nigel H. Trewin, Malcolm J. Hole, Lawrence A. Lawver, Juan Rafael Franzese, David MacDonald, Luis Antonio Spalletti, Lisa M. Gahagan, Ian W. D. Dalziel, I. Gomez-Perez, C. G. C. Thomas, Douglas A. Paton
Publikováno v:
Marine and Petroleum Geology. 20:287-308
This work provides new palinspastic palaeofacies reconstructions of SW Gondwana incorporating rotation of a Falkland/Malvinas microplate. We discuss the implications of this for the tectonic evolution of the southern South Atlantic and hence for the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c97aaf4129b69bd1113d8561ceac7354
https://doi.org/10.1016/s0264-8172(03)00045-x
https://doi.org/10.1016/s0264-8172(03)00045-x
Publikováno v:
The Journal of Geology. 108:499-513
The Llano Orogenic Belt along the present southern margin of Laurentia, regarded as continuation of the Grenvillian Orogen along the eastern Laurentian margin and exposed in basement uplifts in central and western Texas, records an ∼300‐m.yr. his
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31638763afc1bf45657d60732a101c14
https://doi.org/10.1086/314418
https://doi.org/10.1086/314418
Publikováno v:
Journal of Geophysical Research: Solid Earth. 102:3211-3214
We have created a digital age grid of the ocean floor with a grid node interval of 6 arc min using a self-consistent set of global isochrons and associated plate reconstruction poles. The age at each grid node was determined by linear interpolation b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c80856f69c9a13ee91b73d72af72cb0a
https://doi.org/10.1029/96jb01781
https://doi.org/10.1029/96jb01781