Work

Geochemistry, Geophysics, Geosystems

Year: 2018

Type: paratext

Abstract: Giant seafloor depressions are formed by an interaction of bottom currents and pre-existing seafloor topograph Initial seafloor depressions are initiated by slope failure processes

Source: Geochemistry Geophysics Geosystems

DOI: 10.1002/(issn)1525-2027

Authors: Ingale, Vaibhav Vijay, Tepp, Gabrielle, Dziak, Robert P., Parnell‐Turner, Ross

Institutions: Scripps Institution of Oceanography, University of California San Diego, California Institute of Technology, National Oceanic and Atmospheric Administration, NOAA Pacific Marine Environmental Laboratory

Language: English

Topic: Geological formations and processes

Subfield: Earth-Surface Processes

Field: Earth and Planetary Sciences

Domain: Physical Sciences

Open Access status: hybrid

Estimated APC paid: $3,000

Funders: National Science Foundation, Leverhulme Trust, National Oceanic and Atmospheric Administration, University of California, San Diego, Natural Environment Research Council

Awards: G1514894624, Global and regional perspectives of Pleistocene paleoceanography in the western Pacific warm pool based on new sites from IODP Expedition 363, Collaborative Research: Investigating the Role of Mantle Metasomatism and Melt-Rock Interaction During Evolution of Continental Lithosphere Mantle, MCA: Destroying continental plates - unraveling the role of magmatism, Reconstructing Intermediate Water Temperature Response to Pliocene-Pleistocene Climates, Reconstructing Intermediate Water Temperature Response to Pliocene-Pleistocene Climates

OpenAlex ID: W4205573591

Cites: 55

Cited by: 889

Related to: 10