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A Digital Age Map of the Ocean Floor

TLDR
Muller et al. as mentioned in this paper created a digital age grid of the ocean floor with a grid node interval of 6 arc minutes using a selfconsistent set of global isochrons and associated plate reconstruction poles.
Abstract
Author(s): Muller, R. Dietmar; Roest, Walter R; Royer, Jean-Yves; Gahagan, Lisa M; Sclater, John G | Abstract: We have created a digital age grid of the ocean floor with a grid node interval of 6 arc minutes using a self-consistent set of global isochrons and associated plate reconstruction poles. The age at each grid node was determined by linear interpolation between adjacent isochrons in the direction of spreading. Ages for ocean floor between the oldest identified magnetic anomalies and continental crust were interpolated by estimating the ages of passive continental margin segments from geological data and published plate models.

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Late Cretaceous to Miocene sea‐level estimates from the New Jersey and Delaware coastal plain coreholes: an error analysis

TL;DR: In this article, the authors present a method for estimating sea level for the last 108 million years through backstripping of corehole data from the New Jersey and Delaware Coastal Plains.
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The thermal structure of the lithosphere from shear wave velocities

TL;DR: In this paper, the authors combine thermal models of the Pacific lithosphere and pressure and temperature estimates from mantle nodules brought up by kimberlites with three dimensional models of Vs from surface wave tomography to obtain an empirical relation for Vs(P,T), where P is the pressure.
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Measuring the pulse of a plume with the sedimentary record

Nicky White, +1 more
- 01 Jun 1997 - 
TL;DR: In this paper, the authors correlate the timing of these sediment pulses with the time of surface uplift inferred to have been caused by episodic magmatic underplating on the continental shelf of northwestern Europe, suggesting that individual pulses of sedimentation provide a potentially sensitive measure of plume activity.
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Seismic anisotropy of oceanic upper mantle: Shear wave splitting methodologies and observations

TL;DR: In this article, a stacking method was proposed to find the optimum splitting parameters and 95% error region for teleseismic shear-wave phases from a suite of earthquake events.
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