Zobrazeno 1 - 8
of 8
pro vyhledávání: '"R. E. Marzen"'
Autor:
R. E. Marzen, D. J. Shillington, D. Lizarralde, J. H. Knapp, D. M. Heffner, J. K. Davis, S. H. Harder
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
The Central Atlantic Magmatic Province is the most aerially extensive magmatic event in Earth’s history, yet few constraints exist on the volumes of intrusions at depth. Here, the authors find limited intrusive volumes beneath the South Georgia Rif
Externí odkaz:
https://doaj.org/article/0187946bb48c46d591dadf58879a1a26
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:6625-6652
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research-Solid Earth
Autor:
Daniel Lizarralde, S. H. Harder, R. E. Marzen, D. M. Heffner, D. J. Shillington, J. H. Knapp, J. K. Davis
Publikováno v:
Nature Communications
Nature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
Nature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
The Central Atlantic Magmatic Province (CAMP) is the most aerially extensive magmatic event in Earth’s history, but many questions remain about its origin, volume, and distribution. Despite many observations of CAMP magmatism near Earth’s surface
Publikováno v:
Quaternary Science Reviews. 149:109-121
Microfaunal and geochemical proxies from marine sediment records from central Arctic Ocean (CAO) submarine ridges suggest a close relationship over the last 550 thousand years (kyr) between orbital-scale climatic oscillations, sea-ice cover, marine b
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Lauren H. DeNinno, E. K. Caverly, Richard Z. Poore, R. E. Marzen, Thomas M. Cronin, Leonid Polyak, A. R. Brenner, Julio Rodríguez-Lázaro
Publikováno v:
Marine Micropaleontology. 111:118-133
The stratigraphic distributions of ostracodes and selected calcareous benthic and planktic foraminiferal species were studied in sediment cores from ~ 700 to 2700 m water depth on the Northwind, Mendeleev, and Lomonosov Ridges in the western Arctic O
Publikováno v:
Paleoceanography. 29:765-777
Pre-twentieth century sea level (SL) variability remains poorly understood due to limits of tide gauge records, low temporal resolution of tidal marsh records, and regional anomalies caused by dynamic ocean processes, notably multidecadal changes in