World's Best Scientists 2026 revealed!

D-Index & Metrics

Earth Science

D-Index
67
Citations
22226
World Ranking
1191
National Ranking
540

Research.com Recognitions

  • 2016 - Fellow of the American Association for the Advancement of Science (AAAS)
  • 1999 - Fellow of American Geophysical Union (AGU)
  • Fellow of the Geological Society of America
  • Fellow of the Geological Society of America

Overview

What is he best known for?

The fields of study he is best known for:

  • Basalt
  • Igneous rock
  • Plate tectonics

His primary areas of investigation include Mid-ocean ridge, Peridotite, Geochemistry, Mantle and Petrology. His Mid-ocean ridge study incorporates themes from Transform fault and Seafloor spreading. His Peridotite course of study focuses on Abyssal zone and Melt migration, Upwelling, Ultramafic rock and Weathering.

His research investigates the connection with Geochemistry and areas like Ridge which intersect with concerns in Triple junction, Magma and Gabbro. His studies deal with areas such as Mantle convection, Mantle wedge and Transition zone as well as Mantle. Henry J. B. Dick has included themes like Asthenosphere and Geophysics, Crust in his Petrology study.

His most cited work include:

  • Chromian spinel as a petrogenetic indicator in abyssal and alpine-type peridotites and spatially associated lavas (1554 citations)
  • Melting in the oceanic upper mantle: An ion microprobe study of diopsides in abyssal peridotites (1019 citations)
  • An ultraslow-spreading class of ocean ridge (632 citations)

What are the main themes of his work throughout his whole career to date?

His scientific interests lie mostly in Geochemistry, Mid-ocean ridge, Mantle, Basalt and Peridotite. His work focuses on many connections between Geochemistry and other disciplines, such as Lithosphere, that overlap with his field of interest in Shear zone. His Mid-ocean ridge research includes themes of Seafloor spreading and Fracture zone.

His Mantle study integrates concerns from other disciplines, such as Mantle convection, Mantle wedge, Crust, Petrology and Upwelling. In his research on the topic of Basalt, Petrogenesis is strongly related with Ridge. The various areas that Henry J. B. Dick examines in his Peridotite study include Trace element, Metamorphism, Mineralogy, Abyssal zone and Ophiolite.

He most often published in these fields:

  • Geochemistry (53.26%)
  • Mid-ocean ridge (38.04%)
  • Mantle (36.96%)

What were the highlights of his more recent work (between 2000-2017)?

  • Mid-ocean ridge (38.04%)
  • Mantle (36.96%)
  • Geochemistry (53.26%)

In recent papers he was focusing on the following fields of study:

Henry J. B. Dick focuses on Mid-ocean ridge, Mantle, Geochemistry, Peridotite and Seafloor spreading. His Mid-ocean ridge research is multidisciplinary, relying on both Volcano, Fracture zone and Crust. His Mantle research incorporates themes from Abyssal zone and Petrology.

His Lithosphere research extends to Geochemistry, which is thematically connected. Henry J. B. Dick combines subjects such as Ophiolite, Trace element, Mineralogy and Igneous rock with his study of Peridotite. His work is dedicated to discovering how Basalt, Radiogenic nuclide are connected with Isotopes of helium and Petrography and other disciplines.

Between 2000 and 2017, his most popular works were:

  • An ultraslow-spreading class of ocean ridge (632 citations)
  • Coupled major and trace elements as indicators of the extent of melting in mid-ocean-ridge peridotites (421 citations)
  • Magmatic and amagmatic seafloor generation at the ultraslow-spreading Gakkel ridge, Arctic Ocean (303 citations)

In his most recent research, the most cited papers focused on:

  • Basalt
  • Igneous rock
  • Plate tectonics

His primary areas of investigation include Mid-ocean ridge, Geochemistry, Mantle, Basalt and Seafloor spreading. The study incorporates disciplines such as Fracture zone, Petrology, Peridotite and Gabbro in addition to Mid-ocean ridge. His biological study deals with issues like Igneous rock, which deal with fields such as Mineralogy.

In his study, Massif and Lithology is strongly linked to Lithosphere, which falls under the umbrella field of Geochemistry. Henry J. B. Dick is studying Partial melting, which is a component of Mantle. His Ridge research integrates issues from Xenolith and Ophiolite.

Best Publications

  • Chromian spinel as a petrogenetic indicator in abyssal and alpine-type peridotites and spatially associated lavas

    Henry J. B. Dick;Thomas Bullen

  • Melting in the oceanic upper mantle: An ion microprobe study of diopsides in abyssal peridotites

    Kevin T. M. Johnson;Henry J. B. Dick;Nobumichi Shimizu

  • An ultraslow-spreading class of ocean ridge

    Henry J. B. Dick;Jian Lin;Hans Schouten

  • Formation of harzburgite by pervasive melt/rock reaction in the upper mantle

    Peter B. Kelemen;Henry J. B. Dick;James E. Quick

  • Abyssal peridotites, very slow spreading ridges and ocean ridge magmatism

    H. J. B. Dick

  • Coupled major and trace elements as indicators of the extent of melting in mid-ocean-ridge peridotites

    Eric Hellebrand;Jonathan E. Snow;Henry J. B. Dick;Albrecht W. Hofmann

  • A review of melt migration processes in the adiabatically upwelling mantle beneath oceanic spreading ridges

    P. B. Kelemen;G. Hirth;N. Shimizu;M. Spiegelman

  • Mineralogic variability of the uppermost mantle along mid-ocean ridges

    Henry J.B. Dick;Robert L. Fisher;Wilfred B. Bryan

  • A long in situ section of the lower ocean crust: results of {ODP} Leg 176 drilling at the Southwest Indian Ridge

    Henry J.B. Dick;James H. Natland;Jeffrey C. Alt;Wolfgang Bach

  • Magmatic and amagmatic seafloor generation at the ultraslow-spreading Gakkel ridge, Arctic Ocean

    P. J. Michael;C. H. Langmuir;H. J. B. Dick;J. E. Snow

  • Geochemistry, Mineralogy and Petrogenesis of Lavas Erupted along the Southwest Indian Ridge Between the Bouvet Triple Junction and 11 Degrees East

    A. P. Le Roex;H. J. B. Dick;A. J. Erlank;A. M. Reid

  • Pervasive magnesium loss by marine weathering of peridotite

    Jonathan E. Snow;Jonathan E. Snow;Henry J.B. Dick

  • Open system melting and temporal and spatial variation of peridotite and basalt at the Atlantis II Fracture Zone

    Kevin T. M. Johnson;Henry J. B. Dick

  • Late-stage melt evolution and transport in the shallow mantle beneath the East Pacific Rise

    H. J. B. Dick;J. H. Natland

  • Tectonics of ridge-transform intersections at the Kane fracture zone

    J. A. Karson;H. J. B. Dick

  • The fingerprint of seawater circulation in a 500-meter section of ocean crust gabbros

    Stanley R. Hart;Jerzy Blusztajn;Henry J.B. Dick;Peter S. Meyer;Peter S. Meyer

  • A mechanism for magmatic accretion under spreading centres

    John A. Whitehead;Henry J. B. Dick;Hans Schouten

  • Partial melting in the Josephine Peridotite; I, The effect on mineral composition and its consequence for geobarometry and geothermometry

    H. J. B. Dick

  • Lithostratigraphic Evolution of an In-Situ Section of Oceanic Layer 3

    H.J.B. Dick;P.S. Meyer;S. Bloomer;S. Kirby

  • Discovery of abundant hydrothermal venting on the ultraslow-spreading Gakkel ridge in the Arctic Ocean

    H. N. Edmonds;P. J. Michael;E. T. Baker;D. P. Connelly

Frequent Co-Authors

Jonathan E. Snow
Jonathan E. Snow Louisiana State University
Stanley R. Hart
Stanley R. Hart Woods Hole Oceanographic Institution
Peter J. Michael
Peter J. Michael University of Tulsa
Hans Schouten
Hans Schouten Woods Hole Oceanographic Institution
Charles H. Langmuir
Charles H. Langmuir Harvard University
Wolfgang Bach
Wolfgang Bach University of Bremen
Nobumichi Shimizu
Nobumichi Shimizu Woods Hole Oceanographic Institution
Greg Hirth
Greg Hirth Brown University
Edward T. Baker
Edward T. Baker Joint Institute for the Study of the Atmosphere and Ocean
David W. Graham
David W. Graham Oregon State University

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