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Dive into the research topics where Geoffrey H. Howarth is active.

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Featured researches published by Geoffrey H. Howarth.


International Geology Review | 2014

The secondary origin of diamonds: multi-modal radiation tomography of diamondiferous mantle eclogites

Geoffrey H. Howarth; N. V. Sobolev; John F. Pernet-Fisher; Peter H. Barry; Dayakar Penumadu; Stephen B. Puplampu; Richard A. Ketcham; Jessica A. Maisano; Dawn Taylor; L. A. Taylor

Three-dimensional neutron and X-ray tomography reveals the textural and spatial relationship of diamonds and associated minerals in situ, in a unique suite of 17 diamondiferous eclogites. We emphasize the reporting of X-ray imaging on mantle xenoliths, which in combination with neutron imaging enables the clear identification of diamonds and interstitial metasomatic secondary minerals. In particular, neutrons are highly sensitive to hydrogen (H), allowing for the identification of OH- and H2O-bearing metasomatic minerals. The identification of metasomatic minerals allows for the delineation of distinct metasomatic pathways through the eclogite xenoliths. Diamonds are readily identified as the darkest greyscales due to their low attenuation, and are typically surrounded by secondary minerals, never in contact with primary minerals, and always confined within metasomatic pathways. The ubiquitous occurrence of diamonds in association with pathways suggests a potential genetic link. Both octahedral and dodecahedral diamonds are observed within individual xenoliths, suggesting multiple heterogeneous growth and dissolution processes at small scales. The distinct age dichotomy between eclogite xenoliths and metasomatic mineral assemblages implies that the observed textural relationship of diamonds and late-stage metasomatic pathways for this suite of 17 eclogites casts doubt on the theory that eclogitic diamonds formed billions of years ago. Diamonds are interpreted to have formed from multiple growth episodes, with the last of these episodes represented by the metasomatic assemblages observed in this study. This further indicates that eclogitic diamond inclusions may span large time scales from ancient ages (>2 Ga) all the way to the last growth event, perhaps even close to the time of kimberlite emplacement (~360 Ma), which has significant implications for age-dating of diamonds and the study of diamonds as a whole.


Geoscience frontiers | 2013

Two stages of immiscible liquid separation in the formation of Panzhihua-type Fe-Ti-V oxide deposits,SW China

Mei-Fu Zhou; Wei Terry Chen; Christina Yan Wang; Stephen A. Prevec; Patricia Pingping Liu; Geoffrey H. Howarth


Lithos | 2014

Superplume metasomatism: Evidence from Siberian mantle xenoliths

Geoffrey H. Howarth; Peter H. Barry; John F. Pernet-Fisher; Ioannis P. Baziotis; N. P. Pokhilenko; Lyudmila N. Pokhilenko; Robert J. Bodnar; L. A. Taylor; A. M. Agashev


South African Journal of Geology | 2009

CRETACEOUS EROSION IN CENTRAL SOUTH AFRICA: EVIDENCE FROM UPPER-CRUSTAL XENOLITHS IN KIMBERLITE DIATREMES

E.K. Hanson; John M. Moore; Emese M. Bordy; J.S. Marsh; Geoffrey H. Howarth; J.V.A. Robey


Lithos | 2013

Timing of Ti-magnetite crystallisation and silicate disequilibrium in the Panzhihua mafic layered intrusion: Implications for ore-forming processes

Geoffrey H. Howarth; Stephen A. Prevec; Mei-Fu Zhou


Geoscience frontiers | 2013

Assimilation of carbonate country rock by the parent magma of the Panzhihua Fe-Ti-V deposit (SW China): Evidence from stable isotopes

Clément Ganino; Chris Harris; Nicholas T. Arndt; Stephen A. Prevec; Geoffrey H. Howarth


Contributions to Mineralogy and Petrology | 2014

Komsomolskaya diamondiferous eclogites: evidence for oceanic crustal protoliths

John F. Pernet-Fisher; Geoffrey H. Howarth; Yang Liu; Peter H. Barry; Laura Carmody; John W. Valley; Robert J. Bodnar; Zdislav V. Spetsius; L. A. Taylor


Geoscience frontiers | 2013

Hydration vs. oxidation: Modelling implications for Fe–Ti oxide crystallisation in mafic intrusions, with specific reference to the Panzhihua intrusion, SW China

Geoffrey H. Howarth; Stephen A. Prevec


Geochimica et Cosmochimica Acta | 2015

Evidence for the exsolution of Cl-rich fluids in martian magmas: Apatite petrogenesis in the enriched lherzolitic shergottite Northwest Africa 7755

Geoffrey H. Howarth; John F. Pernet-Fisher; Robert J. Bodnar; L. A. Taylor


Geochimica et Cosmochimica Acta | 2013

Trace element, PGE, and Sr-Nd isotope geochemistry of the Panzhihua mafic layered intrusion, SW China: Constraints on ore-forming processes and evolution of parent magma at depth in a plumbing-system

Geoffrey H. Howarth; Stephen A. Prevec

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L. A. Taylor

University of Tennessee

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N. V. Sobolev

Russian Academy of Sciences

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Yang Liu

California Institute of Technology

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