Results 41 to 50 of about 187 (140)
Subducting volcaniclastic-rich upper crust supplies fluids for shallow megathrust and slow slip. [PDF]
Gase AC +11 more
europepmc +1 more source
Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events. [PDF]
Matsumoto H +7 more
europepmc +1 more source
Origin and evolution of the Ontong Java Plateau: introduction [PDF]
J. Godfrey Fitton +3 more
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Oceanic and super-deep continental diamonds share a transition zone origin and mantle plume transportation. [PDF]
Doucet LS, Li ZX, Gamal El Dien H.
europepmc +1 more source
Remelting of Ontong Java Plateau Lithosphere
identifier:oai:t2r2.star.titech.ac.jp ...
openaire +1 more source
Volcanic controls on seawater sulfate over the past 120 million years. [PDF]
Laakso TA +3 more
europepmc +1 more source
High mantle seismic P-wave speeds as a signature for gravitational spreading of superplumes. [PDF]
Stern T +4 more
europepmc +1 more source
3. SEISMIC STRATIGRAPHY OF THE ONTONG JAVA PLATEAU 1
The Ontong Java Plateau, a large, deep-water carbonate plateau in the western equatorial Pacific, is an ideal location for studying responses of carbonate sedimentation to the effects of changing paleoceanographic conditions. These carbonate responses are often reflected in the physical properties of the sediment, which in turn control the appearance ...
Mosher, D.C. +16 more
openaire +1 more source

