Results 201 to 210 of about 3,877 (262)

Evidence for crustal brines and deep fluid infiltration in an oceanic transform fault. [PDF]

open access: yesSci Adv
Chesley C   +14 more
europepmc   +1 more source

Tectonic and climatic implications of the Aleutian Arc initiation ≥56 million years ago. [PDF]

open access: yesNat Commun
Hoernle K   +13 more
europepmc   +1 more source

Recent increase in N<sub>2</sub>O growth rate (2013-2023) mainly due to increase of nitrogen-fertiliser and manure use in the Northern Tropics and Southern Landmass. [PDF]

open access: yesGeosci Lett
Patra PK   +14 more
europepmc   +1 more source

Lithium isotope evidence for enhanced continental weathering triggering the late Paleozoic greenhouse-to-icehouse climate transition. [PDF]

open access: yesNatl Sci Rev
Zhang F   +10 more
europepmc   +1 more source

Bridging the gap between subduction dynamics and the long-term strength of the Sunda megathrust. [PDF]

open access: yesNat Commun
Capitanio FA   +6 more
europepmc   +1 more source

Slab tearing and segmented subduction termination driven by transform tectonics. [PDF]

open access: yesSci Adv
Shuck B   +14 more
europepmc   +1 more source
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Measurement of the point spread function in the ocean

Applied Optics, 1990
A new instrument to measure the point spread function (PSF) in the ocean is described. This instrument uses a CCD solid state camera to measure the angular radiance field due to a pulsed Lambertian source. In this way the PSF can be measured easily at sea, when precise alignments over ranges >10 m cannot be maintained.
K J, Voss, A L, Chapin
openaire   +2 more sources

Oceanic spreading rate and crustal thickness

Marine Geophysical Researches, 1981
Examination of oceanic seismic refraction results indicates a correlation between total crustal thickness and spreading rate, with slower spreading producing thinner crust. The effect is seen at spreading rates less than about 20 mm yr−1. The crustal thickness and its dependence on spreading rate are predicted by theoretical modelling of flow and ...
I Reid, H R Jackson
exaly   +2 more sources

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