Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Katherine L. Maier"'
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Observations from the modern seafloor that suggest turbidity currents tend to erode as they lose channel-levee confinement, rather than decelerating and depositing their sediment load, has driven investigations into sediment gravity flow behaviour at
Externí odkaz:
https://doaj.org/article/a809607c23334784aee94b99b101df1b
Autor:
Charles K. Paull, Peter J. Talling, Katherine L. Maier, Daniel Parsons, Jingping Xu, David W. Caress, Roberto Gwiazda, Eve M. Lundsten, Krystle Anderson, James P. Barry, Mark Chaffey, Tom O’Reilly, Kurt J. Rosenberger, Jenny A. Gales, Brian Kieft, Mary McGann, Steve M. Simmons, Mike McCann, Esther J. Sumner, Michael A. Clare, Matthieu J. Cartigny
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
The structure of turbidity currents has remained unresolved mainly due to lack of observations. Here the authors present data from a high-resolution monitoring array deployed for 18 months over Monterey Bay, that suggests turbidity currents are drive
Externí odkaz:
https://doaj.org/article/c89a013470984ee8871bebcd73c8c6c1
Autor:
Katherine L. Maier, Jennifer A. Gales, Charles K. Paull, Kurt Rosenberger, Peter J. Talling, Stephen M. Simmons, Roberto Gwiazda, Mary McGann, Matthieu J. B. Cartigny, Eve Lundsten, Krystle Anderson, Michael A. Clare, Jingping Xu, Daniel Parsons, James P. Barry, Monica Wolfson-Schwehr, Nora M. Nieminski, Esther J. Sumner
Publikováno v:
Frontiers in Earth Science, Vol 7 (2019)
Submarine canyons are conduits for episodic and powerful sediment density flows (commonly called turbidity currents) that move globally significant amounts of terrestrial sediment and organic carbon into the deep sea, forming some of the largest sedi
Externí odkaz:
https://doaj.org/article/6d2e0e1523cd46d7b77b5e0966277f3b
Publikováno v:
New Zealand Journal of Geology and Geophysics. 66:42-58
Autor:
Andrea Fildani, Charles K. Paull, Jacob A. Covault, Katherine L. Maier, David W. Caress, Svetlana Kostic
Publikováno v:
Sedimentology. 68:1378-1399
Autor:
R. Gwiazda, C. K. Paull, B. Kieft, D. Klimov, R. Herlien, E. Lundsten, M. McCann, Matthieu J. Cartigny, A. Hamilton, J. Xu, Katherine L. Maier, D. R. Parsons, Peter J. Talling
Publikováno v:
Journal of Geophysical Research: Earth Surface, 2022, Vol.127(2) [Peer Reviewed Journal]
The near-bed section of submarine gravity flows travels at the highest and most destructive speeds making direct measurements of this region of the flow difficult. Here results are presented from “boulder-like” Benthic Event Detectors (BEDs) that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0f620b23bada8e13ea0e42078e6f883a
https://doi.org/10.1029/2021JF006437
https://doi.org/10.1029/2021JF006437
Autor:
Maureen A.L. Walton, Daniel S. Brothers, James E. Conrad, Katherine L. Maier, Emily C. Roland, Jared W. Kluesner, Peter Dartnell
Publikováno v:
Geosphere. 16:1312-1335
Catalina Basin, located within the southern California Inner Continental Borderland (ICB), United States, is traversed by two active submerged fault systems that are part of the broader North America–Pacific plate boundary: the San Clemente fault (
Autor:
K. Anderson, N. Nieminski, Andrea Fildani, David W. Caress, Benjamin E. Erwin, Charles K. Paull, Roberto Gwiazda, Eve Lundsten, Katherine L. Maier
Publikováno v:
Journal of Sedimentary Research. 90:468-479
New high-resolution datasets across La Jolla submarine fan, offshore California, illuminate low-relief, down-dip widening conduits emanating from a deep-sea channel that deposited a combination of laterally extensive sand strata seemingly crisscrosse
Autor:
Monterey Cce Team, Katherine L. Maier, Daniel R. Parsons, Stephen M. Simmons, Mary McGann, Kurt J. Rosenberger, Eve Lundsten, Michael A. Clare, Matthieu J.B. Cartigny, Charles K. Paull, Roberto Gwiazda, Lewis Bailey, Jingping Xu, Ivan D. Haigh, Peter J. Talling
Publikováno v:
Earth and Planetary Science Letters, 2021, Vol.562, pp.116845 [Peer Reviewed Journal]
Turbidity currents dominate sediment transfer into the deep ocean, and can damage critical seabed infrastructure. It is commonly inferred that powerful turbidity currents are triggered by major external events, such as storms, river floods, or earthq
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c7b1e52fb104c7f9cb8079af71d2b7ec
https://eprints.soton.ac.uk/468558/
https://eprints.soton.ac.uk/468558/
Publikováno v:
Marine Geology. 404:24-40
The Monterey submarine canyon, incised across the continental shelf in Monterey Bay, California, provides a record of the link between onshore tectonism, fluvial transport, and deep-marine deposition. High-resolution seismic-reflection imaging in Mon