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Craig Manning

· Distinguished Professor & Associate Dean for Academic Personnel

University of California, Los Angeles · Earth and Space Sciences

Active 1974–2025

h-index75
Citations18.0k
Papers45645 last 5y
Funding$1.9M

Academic metrics are sourced from OpenAlex and public funding records; values may differ from Google Scholar.

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About

Craig Manning is a Distinguished Professor and Associate Dean for Academic Personnel at UCLA's Department of Earth, Planetary, and Space Sciences (EPSS). His role involves academic leadership within the department, contributing to the development and administration of academic programs and policies. Manning's work is associated with research in earth, planetary, and space sciences, and he is actively involved in departmental activities, including seminars, research groups, and community updates. His contact information includes a phone number and email at UCLA EPSS, and he is engaged in supporting inclusive excellence and academic resources within the department.

Research topics

  • Geology
  • Geochemistry
  • Seismology
  • Geophysics
  • Petrology
  • Chemistry
  • Materials science
  • Environmental chemistry
  • Organic chemistry
  • Metallurgy

Selected publications

  • Subduction-Zone Fluids

    Elements · 2020 · 90 citations

    1st authorCorresponding

    Fluids are essential to the physical and chemical processes in subduction zones. Two types of subduction-zone fluids can be distinguished. First, shallow fluids, which are relatively dilute and water rich and that have properties that vary between subduction zones depending on the local thermal regime. Second, deep fluids, which possess higher proportions of dissolved silicate, salts and non-polar gases relative to water content, and have properties that are broadly similar in most subduction sy…

  • Listvenite Formation During Mass Transfer into the Leading Edge of the Mantle Wedge: Initial Results from Oman Drilling Project Hole BT1B

    Journal of Geophysical Research Solid Earth · 2022-01-13 · 41 citations

    articleOpen access

    Abstract This paper provides an overview of research on core from Oman Drilling Project Hole BT1B and the surrounding area, plus new data and calculations, constraining processes in the Tethyan subduction zone beneath the Samail ophiolite. The area is underlain by gently dipping, broadly folded layers of allochthonous Hawasina pelagic sediments, the metamorphic sole of the Samail ophiolite, and Banded Unit peridotites at the base of the Samail mantle section. Despite reactivation of some faults…

  • Brittle Deformation of Carbonated Peridotite—Insights From Listvenites of the Samail Ophiolite (Oman Drilling Project Hole BT1B)

    Journal of Geophysical Research Solid Earth · 2020 · 40 citations

    Abstract Hole BT1B of the Oman Drilling Project provides a continuous sampling from listvenite into the metamorphic sole that preserves the deformation, hydration, and carbonation processes of oceanic mantle peridotite at the base of the Samail ophiolite, Oman. We present evidence of multistage brittle deformation in listvenites and serpentinites based on field observations, visual core logging and petrography. About 10 vol% of listvenite and serpentinite in Hole BT1B is composed of cataclasite…

  • Hydrothermal Properties of Geologic Fluids

    Elements · 2020-12-01 · 38 citations

    articleSenior author

    Aqueous fluids are critical agents in the geochemical evolution of Earth’s interior. Fluid circulation and fluid–rock reactions in the Earth take place at temperatures ranging from ambient to magmatic, at pressures from ambient to extreme, and involve fluids that range from nearly pure H2O through to complex, multicomponent solutions. Consequently, the physical and chemical properties of hydrothermal fluids vary widely as functions of geologic setting; this variation strongly impacts fluid-drive…

  • Subducted organic matter buffered by marine carbonate rules the carbon isotopic signature of arc emissions

    Nature Communications · 2022 · 36 citations

    isotopic signature with the fluid-rock ratios and the redox state in force in its subarc source.

Recent grants

Frequent coauthors

  • Robert C. Newton

    Planetary Science Institute

    66 shared
  • P. B. Kelemen

    50 shared
  • C. J. MacLeod

    50 shared
  • An Yin

    44 shared
  • Peter Tropper

    40 shared
  • A. R. Makhluf

    University of California, Los Angeles

    38 shared
  • T. Mark Harrison

    University of California, Los Angeles

    31 shared
  • Edward Young

    Planetary Science Institute

    29 shared

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