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Volcanic growth faults and the origin of Pacific abyssal hills

TLDR
Submersible-based investigations show that Pacific abyssal hills are created on the flanks of the East Pacific Rise as horsts and grabens which lengthen with time as mentioned in this paper.
Abstract
The topographic features known as abyssal hills characterize >30% of the ocean floor, and yet their origin has been the subject of vigorous debate for over 40 years. Submersible-based investigations show that Pacific abyssal hills are created on the flanks of the East Pacific Rise as horsts and grabens which lengthen with time. Hills are bounded on one side by ridge-facing scarps produced by normal faulting, and on the other by more gentle slopes produced by volcanic growth faulting.

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A new digital bathymetric model of the world's oceans

TL;DR: The General Bathymetric Chart of the Oceans (GEBCO) as discussed by the authors has been updated with a new digital bathymetric model of the world ocean floor merged with land topography from publicly available digital elevation models.
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Permeability within basaltic oceanic crust

TL;DR: In this paper, a series of focused experiments are required to resolve the wide range of estimated permeability in shallow oceanic basement and to directly couple upper crustal hydrogeology to magmatic, tectonic, and geochemical crustal evolution.
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Modes of seafloor generation at a melt-poor ultraslow-spreading ridge

TL;DR: In this paper, the authors report on extensive off-axis bathymetry, gravity, and magnetic data that provide a 26m.y.d. record of axial tectonic and magmatic processes over a 660km-long and melt-poor portion of the ultralow Southwest Indian Ridge.
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Modes of faulting at mid-ocean ridges

TL;DR: In this article, the authors show that plate unbending with distance from the top of an axial high reproduces the observed dip directions and offsets of faults formed at fast-spreading centres.
References
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Journal ArticleDOI

Mid-Ocean Ridges: Fine Scale Tectonic, Volcanic and Hydrothermal Processes Within the Plate Boundary Zone

TL;DR: In this article, the authors focus on the fine-scale tectonics and geophysics of the active axial zone of mid-ocean ridges with reference to associated volcanic and hydrothermal processes.
Journal ArticleDOI

Stochastic Modeling of Seafloor Morphology: Inversion of Sea Beam Data for Second-Order Statistics

TL;DR: In this article, the seafloor is modeled as a stationary, zero-mean, Gaussian random field completely specified by its two-point covariance function, and the second moments are used as data functionals.
Journal ArticleDOI

Hydrothermal vent distribution along the East Pacific Rise crest (9°09′–54′N) and its relationship to magmatic and tectonic processes on fast-spreading mid-ocean ridges

TL;DR: In this article, the authors used the near bottom ARGO imaging system to visually and acoustically survey the narrow ( < 200 m wide) axial zone of the fast-spreading East Pacific Rise (EPR) along 83 km of its length (9°09′-54′N), and systematically mapped the distribution of hundreds of hydrothermal features relative to other fine-scale volcanic and tectonic features of the ridge crest.
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