D
Daniel L. Orange
Researcher at University of California, Santa Cruz
Publications - 64
Citations - 3634
Daniel L. Orange is an academic researcher from University of California, Santa Cruz. The author has contributed to research in topics: Submarine canyon & Accretionary wedge. The author has an hindex of 33, co-authored 64 publications receiving 3419 citations. Previous affiliations of Daniel L. Orange include Monterey Bay Aquarium Research Institute.
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Journal ArticleDOI
Submarine landslide geomorphology, US continental slope
TL;DR: The morphometric analysis of submarine landslides in four distinctly different tectonic environments on the continental slopes of Oregon, central California, Texas, and New Jersey provides useful insight into submarine process, including sediment transport mechanisms and slope stability as mentioned in this paper.
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Distinguishing sediment waves from slope failure deposits: Field examples, including the 'humboldt slide', and modelling results
Homa J. Lee,James P. M. Syvitski,Gary Parker,Daniel L. Orange,Jacques Locat,Eric W. H. Hutton,Jasim Imran +6 more
TL;DR: A reassessment of these features strongly suggests that numerous turbidity currents, separated by intervals of ambient hemipelagic sedimentation, deposited the wave fields over thousands of years as discussed by the authors.
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Cold-seeps and authigenic carbonate formation in Monterey Bay, California
TL;DR: Authigenic carbonates associated with modern cold seep biological communities and their extinct analogues exhibit a broad range in stable isotope and mineral composition within a limited geographic area of Monterey Bay as mentioned in this paper.
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Biologic and geologic characteristics of cold seeps in Monterey Bay, California
James P. Barry,H. Gary Greene,H. Gary Greene,Daniel L. Orange,C. H. Baxter,Bruce H. Robison,Randall E. Kochevar,James Nybakken,Donald L. R,Cecilia M. G. McHugh +9 more
TL;DR: In this article, cold seep communities discovered at three previously unknown sites between 600 and 1000 m in Monterey Bay, California, are dominated by chemoautotrophic bacteria (Beggiatoa sp.) and vesicomyid clams (5 sp.).
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Fluid venting in the eastern Aleutian Subduction Zone
Erwin Suess,Gerhard Bohrmann,Roland von Huene,Peter Linke,Klaus Wallmann,Stephan Lammers,Heiko Sahling,Gisela Winckler,Richard A. Lutz,Daniel L. Orange +9 more
TL;DR: A biogeochemical approach toward estimating fluid flow rates from individual vents based on oxygen flux measurements and vent fluid analysis indicates a mean value of 5.5 + 0.7 L m -2 d -1 for tectonics-induced water flow as discussed by the authors.