Results 111 to 120 of about 126,680 (250)
Miocene deep-water agglutinated foraminifera from the Lomonosov Ridge and the opening of the Fram Strait [PDF]
Deep-water agglutinated Foraminifera (DWAF) were recovered from Miocene to Pliocene sediments in 103 samples from IODP Hole M0002A on the Lomonosov Ridge.
Kaminski, M.A., Kender, S., Silye, L.
core
The carbon isotopic signature of the upper mantle is heterogeneous
Knowledge of the carbon isotopic (δ13C) signature of the mantle source region of mid–ocean ridge basalts, is key to understanding carbon cycling on a planetary scale.
Yves Moussallam +5 more
doaj +1 more source
Modeling the effects of tidal loading on mid‐ocean ridge hydrothermal systems [PDF]
T. J. Crone, William S. D. Wilcock
openalex +1 more source
Unbending connects sea level to faulting at fast-spreading mid-ocean ridges
Richard F. Katz, Peter Huybers
openalex +1 more source
The significance of plagioclase textures in mid-ocean ridge basalt (Gakkel Ridge, Arctic Ocean). [PDF]
Bennett EN, Lissenberg CJ, Cashman KV.
europepmc +1 more source
Consequences of a crystal mush-dominated magma plumbing system: a mid-ocean ridge perspective. [PDF]
Lissenberg CJ, MacLeod CJ, Bennett EN.
europepmc +1 more source
Magmatic Processes Associated with Oceanic Crustal Accretion at Slow-spreading Ridges: Evidence from Plagioclase in Mid-ocean Ridge Basalts from the South China Sea [PDF]
Fan Yang +3 more
openalex +1 more source

