scispace - formally typeset
J

John G. Spray

Researcher at University of New Brunswick

Publications -  186
Citations -  6353

John G. Spray is an academic researcher from University of New Brunswick. The author has contributed to research in topics: Impact crater & Impact structure. The author has an hindex of 43, co-authored 175 publications receiving 5670 citations. Previous affiliations of John G. Spray include Centre national de la recherche scientifique.

Papers
More filters
Journal ArticleDOI

Volatile and organic compositions of sedimentary rocks in Yellowknife Bay, Gale crater, Mars.

Douglas W. Ming, +442 more
- 24 Jan 2014 - 
TL;DR: Higher abundances of chlorinated hydrocarbons in the mudstone compared with Rocknest windblown materials previously analyzed by Curiosity suggest that indigenous martian or meteoritic organic carbon sources may be preserved in the Mudstone; however, the carbon source for the chlorinatedHydrocarbons is not definitively of martian origin.
Journal ArticleDOI

Pseudotachylyte controversy: Fact or friction?

TL;DR: In this article, high-speed slip experiments performed on Westerly granite using friction welding apparatus reveal that comminution is an essential precursor to melting by friction, which is not mutually exclusive process.
Journal ArticleDOI

A physical basis for the frictional melting of some rock-forming minerals

TL;DR: In this paper, it was observed that phyllosilicates and amphiboles are preferentially consumed to form the melt phase, whilst quartz and feldspar tend to survive as clasts.
Journal ArticleDOI

Frictional melting processes and products in geological materials: introduction and discussion

TL;DR: The 1990 Geological Society of America Annual Meeting in Dallas, Texas, U.S.A as mentioned in this paper brought together researchers working on various aspects of frictional melting in rock, to provide a forum for the exchange of new ideas and to encourage the production of a thematic set of papers dedicated to the topic.
Journal ArticleDOI

Age constraints on the igneous and metamorphic evolution of the Hellenic-Dinaric ophiolites

TL;DR: In this article, the available age data from Greek and Yugoslavian ophiolites and related rocks are reviewed and, where necessary, have been corrected using the decay constants of Steiger & Jäger (1977).