Journal articleGeophysical Research Letters · October 28, 2025
Incipient Rift (IR) is the latest in a sequence of short-lived rifts that form ridge-ridge-ridge triple junctions with the East Pacific Rise (EPR) in the Galapagos triple junction region. IR extends ∼65 km southeastward from its intersection with the EPR a ...
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Journal articleEarth and Planetary Science Letters · October 15, 2023
Numerous geochemical studies on mid-ocean ridge basalts have established the presence of both compositional and lithological heterogeneities in the upper mantle. These studies have successfully constrained the composition and age of the chemical heterogene ...
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Journal articleAmerican Mineralogist · May 1, 2023
Trace concentrations of H2O in olivine strongly affect diverse mantle and magmatic processes. H2O in olivine has been difficult to accurately quantify due to challenges in sample preparation and measurement, as well as significant uncertainties in standard ...
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Journal articleGeophysical Research Letters · March 16, 2023
This study analyzes up-to-date gravity data in the Galapagos triple junction region to understand crustal structure and melt distribution beneath the propagating Cocos-Nazca spreading center (CNSC). Application of a standard thermal model to the mantle Bou ...
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Journal articleGeochemistry Geophysics Geosystems · March 1, 2023
A tectonic window into the upper 2,000 m of oceanic crust generated at the superfast spreading (∼142 mm/yr) southern East Pacific Rise exposes a continuous layered structure of basaltic lavas and sheeted dikes over gabbroic rocks. This relatively simple st ...
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Journal articleGlobal Biogeochemical Cycles · November 1, 2022
Direct exploitation and use of arsenic resources has diminished in recent years, but inadvertent mobilizations of As from mineral extractions (metal ores, coal, and phosphate rock) are now as much as ten-fold greater (1,500–5,600 × 109 g/yr) tha ...
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Journal articleGlobal Biogeochemical Cycles · August 2021
AbstractThe total human mobilization of Li from the Earth's crust, >1,000 × 109 g/year, is much larger than Li mobilized by the natural processes of chemical and mechanical weathering (94 and 132 × 1 ...
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Journal articleGlobal Biogeochemical Cycles · December 1, 2020
This review provides a synthesis of what is currently known about the natural and anthropogenic fluxes of fluorine on Earth, offering context for an evaluation of the growing environmental impact of human-induced F mobilization and use. The largest flux of ...
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Journal articleGeochemistry Geophysics Geosystems · June 1, 2020
At the Galapagos triple junction in the equatorial Pacific Ocean, the Cocos-Nazca spreading center does not meet the East Pacific Rise (EPR) but, instead, rifts into 0.4 Myr-old lithosphere on the EPR flank. Westward propagation of Cocos-Nazca spreading fo ...
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Journal articleProceedings of the National Academy of Sciences of the United States of America · December 2017
Synthesizing published data, we provide a quantitative summary of the global biogeochemical cycle of vanadium (V), including both human-derived and natural fluxes. Through mining of V ores (130 × 109 g V/y) and extraction and combustion of fossi ...
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Journal article · January 1, 2016
Mid-ocean ridges display tectonic segmentation defined by discontinuities of the axial zone, and geophysical and geochemical observations suggest segmentation of the underlying magmatic plumbing system. Here, observations of tectonic and magmatic segmentat ...
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Journal articleGeophysical Research Letters · January 1, 2016
It has recently been estimated that serpentinization within continental lithosphere produces H2 at rates comparable to oceanic lithosphere (both are ~1011 mol H2/yr). Here we present a simple model that suggests that H ...
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Journal articleGeochemistry Geophysics Geosystems · November 1, 2012
Early studies of mid-ocean ridge discontinuities, such as transform faults and overlapping spreading centers, suggested a lower magma supply compared to ridge segment centers. This is reflected in bathymetrically deeper ridge axes, decreased hydrothermal a ...
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Journal articleChemical Geology · August 7, 2011
Most geochemical variability in MOR basalts is consistent with low- to moderate-pressure fractional crystallization of various mantle-derived parental melts. However, our geochemical data from MOR high-silica glasses, including new volatile and oxygen isot ...
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Journal articleJournal of Petrology · December 1, 2010
Whereas the majority of eruptions at oceanic spreading centers produce lavas with relatively homogeneous mid-ocean ridge basalt (MORB) compositions, the formation of tholeiitic andesites and dacites at mid-ocean ridges (MORs) is a petrological enigma. Erup ...
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Journal articleEarth and Planetary Science Letters · April 15, 2009
Ever since the discovery that the mid-ocean ridge axis deepens at most axial discontinuities, there has been vigorous debate about whether ridge axis depth and shape reflect magma supply. Here we report evidence, from one of the most thoroughly studied rid ...
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Journal articleJournal of Geophysical Research Solid Earth · March 4, 2009
The northwest trending walls of the Pito Deep Rift (PDR), a tectonic window in the southeast Pacific, expose in situ oceanic crust generated ∼3 Ma at the superfast spreading southern East Pacific Rise (SEPR). Whole rock analyses were performed on over 200 ...
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Journal articleGeology · May 1, 2008
The Galapagos triple junction is a ridge-ridge-ridge triple junction where the Cocos, Nazca, and Pacific plates meet around the Galapagos microplate. Directly north of the large scarps of the Cocos-Nazca Rift, a 250-km-long and 50-km-wide band of northwest ...
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Journal articleGeochemistry Geophysics Geosystems · May 1, 2008
Alteration of sheeted dikes exposed along submarine escarpments at the Pito Deep Rift (NE edge of the Easter microplate) provides constraints on the crustal component of axial hydrothermal systems at fast spreading mid-ocean ridges. Samples from vertical t ...
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Journal articleContributions to Mineralogy and Petrology · November 1, 2007
A suite of samples collected from the uppermost part of the plutonic section of the oceanic crust formed at the southern East Pacific Rise and exposed at the Pito Deep has been examined. These rocks were sampled in situ by ROV and lie beneath a complete up ...
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Journal articleGeochemistry Geophysics Geosystems · November 1, 2005
The northern scarp of the Western Blanco Transform (BT) Fault Zone provides a "tectonic window" into crust generated at an intermediate-rate spreading center, exposing a ∼2000 m vertical section of lavas and dikes. The lava unit was sampled by submersible ...
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Journal articleJournal of Volcanology and Geothermal Research · June 15, 2005
The faulted walls of the Hess Deep Rift in the equatorial Pacific provide one of the few significant tectonic windows into the oceanic crust created at a fast-spreading mid-ocean ridge. The 5000-m-deep rift graben exposes a slightly dismembered section of ...
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Journal articleNature · February 2005
An 'incipient' spreading centre east of (and orthogonal to) the East Pacific Rise at 2 degrees 40' N has been identified as forming a portion of the northern boundary of the Galapagos microplate. This spreading centre was described as a slowly diverging, w ...
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Journal articleJournal of Geophysical Research Solid Earth · April 10, 2003
Differences in composition and phenocryst assemblages between dikes and lavas collected from 1-m.y.-old oceanic crust exposed at the Hess Deep Rift have important implications for density filtering of magmas ascending through the upper crust in mid-ocean r ...
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Journal articleJournal of Geophysical Research: Solid Earth · April 2003
Differences in composition and phenocryst assemblages between dikes and lavas collected from 1‐m.y.‐old oceanic crust exposed at the Hess Deep Rift have important implications for density filtering of magmas ascending through the upper crust in mid ...
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Journal articleJournal of Geophysical Research Solid Earth · October 10, 2002
An investigation of ∼1-m.y.-old dikes and lavas from the north wall of the Hess Deep Rift (2°15′N, 101°30′W) collected during Alvin expeditions provides a detailed view of the evolution of fast spreading oceanic crust. The study area encompasses 25 km of a ...
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Journal articleJournal of Geophysical Research: Solid Earth · October 2002
An investigation of ∼1‐m.y.‐old dikes and lavas from the north wall of the Hess Deep Rift (2°15′N, 101°30′W) collected during Alvin expeditions provides a detailed view of the evolution of fast spreading oceanic crust. Th ...
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Journal articleGeochemistry, Geophysics, Geosystems · January 2002
The uppermost 2 km of the oceanic crust created at the fast spreading (135 mm yr−1, full rate) equatorial East Pacific Rise (EPR) is exposed for tens of kilometers along escarpments bounding the Hess Deep Rift. Mosaics of large ...
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Journal articleEarth and Planetary Science Letters · May 22, 2001
Major- and trace-element analyses of over 50 well-located samples from the third segment south of the Kane Transform Fault are reported. These can be grouped into four age groups based on structural relations and paleomagnetic data. Although no spatial rel ...
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Journal articleGeochemistry Geophysics Geosystems · November 1, 2000
Basaltic glasses from the geophysically well-studied section of the East Pacific Rise (EPR) between 11°45′N to 15deg;00′N range from normal mid-ocean ridge basalts (MORB) to transitional MORB and their major element variations correlate with isotopic and t ...
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Journal articleEarth and Planetary Science Letters · October 17, 2000
Mass spectrometric measurements of 230Th-226Ra, 235U-231Pa and 238U-230Th disequilibria are used to determine eruption ages for four mid-ocean ridge basalts from the median valley of the Mid ...
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Journal articleSpecial Paper of the Geological Society of America · January 1, 2000
The recent discovery of convergent-margin geochemical signatures along the southern Chile Ridge spreading center may have implications for the interpretation of ophiolite provenance. The location of the ridge near a ridge-trench-trench (RTT) triple junctio ...
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Journal articleJournal of Geophysical Research Solid Earth · March 10, 1999
Basalts from the four southernmost segments of the subducting Chile Ridge (numbered 1-4 stepping away from the trench) display large variations in Sr, Nd, Pb, and He isotope and trace element compositions. Klein and Karsten [1995] showed that segments 1 an ...
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Journal articleBiogeochemistry · January 1, 1998
This study examined the accumulation of organic carbon (C) and fractions of soil phosphorus (P) in soils developing in volcanic ash deposited in the 1883 eruption of Krakatau. Organic C has accumulated at rates of 45 to 127 g/m2/yr during 110 ye ...
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Journal articleJournal of Geophysical Research Solid Earth · January 1, 1997
We present major element glass data for 163 rock samples collected from four ridge segments of the southern Chile Ridge between the Chiloe Fracture Zone and the Chile Margin Triple Junction, including the segment currently being subducted at the Chile Tren ...
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Journal articleLithos · January 1, 1996
The southern portion of the Chile Ridge is one of few sites where active subduction of a spreading center and its consequences for ridge axis magmatism can be investigated. New major element, trace element, and isotopic data for lavas recovered from the ri ...
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Journal articleEos · January 1, 1995
Since a large percentage of the mid-ocean ridge system remains uncharted and unsampled, studying the diverse processes involved in the generation of new oceanic crust is an ambitious goal that requires international cooperation. The Ridge InterDisciplinary ...
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Journal articleNature · January 1, 1995
COLLISIONS between active spreading centres and subduction zones have occurred frequently throughout Earth history1. Of the few sites of ridge subduction active today, the southern Chile Ridge has the simplest tectonic history2. We re ...
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Journal articleEos Transactions American Geophysical Union · January 1, 1995
Since a large percentage of the mid‐ocean ridge system remains uncharted and unsampled, studying the diverse processes involved in the generation of new oceanic crust is an ambitious goal that requires international cooperation. The Ridge InterDisciplinary ...
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Journal articleMarine Geophysical Researches · February 1, 1994
Bathmetric highs on the old crust proximal to ridge-transform intersections (RTIs), termed "intersection highs", are common but poorly understood features at offsets of fast to intermediate rate spreading centers. We have combined new reflection seismic, p ...
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Journal articleNature · January 1, 1993
OVER the past several decades, the examination of volcanic rocks recovered from mid-ocean ridges and ocean islands worldwide has led to the identification of large-scale geochemical provinces reflecting compositionally distinct domains in the Earth's mantl ...
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Journal articleJournal of Geophysical Research · January 1, 1991
The ocean basin south of Australia contains the Australian-Antarctic Discordance, an anomalously deep portion of the Southeast Indian Ridge that marks a boundary between isotopic provinces characteristic of the Indian and Pacific oceans. Samples recovered ...
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Journal articleNature · January 1, 1990
KLEIN and Langmuir1 investigated the relationships between the chemistry and water depth of eruption of zero-age mid-ocean-ridge basalts around the world. They showed that the regionally averaged values of the major-element oxides Na2 ...
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Journal articleNature · 1988
Basalts from the Southeast Indian Ridge south of Australia form two geographically and isotopically distinct groups that show affinities with either Indian Ocean or Pacific/Atlantic Ocean isotope compositions. The data raise the possibility that there is a ...
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Journal article · December 1, 1987
Thermal modeling independently predicts the observed relationships among basalt chemistry, ridge depth, and crustal thickness resulting from temperature variations in the mantle. Beneath the shallowest and deepest ridge axes, temperature differences of app ...
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Journal articleJournal of Geophysical Research · 1987
Thermal modeling independently predicts the observed relationships among basalt chemistry, ridge depth, and crustal thickness resulting from temperature variations in the mantle. Beneath the shallowest and deepest ridge axes, temperature differences of app ...
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