John H. Jones mainly investigates Mineralogy, Martian, Mars Exploration Program, Metal and Meteorite. His studies in Mineralogy integrate themes in fields like Fractional crystallization, Trace element, Chondrite and Analytical chemistry. His Martian research is multidisciplinary, incorporating perspectives in Olivine, Crust, Geochemistry, Basalt and Mantle.
Mars Exploration Program is a subfield of Astrobiology that John H. Jones investigates. His research investigates the connection between Metal and topics such as Thermodynamics that intersect with issues in Nonmetal. His work carried out in the field of Meteorite brings together such families of science as Earth science, Carbonate, Hydrothermal circulation, Atmosphere of Earth and Atmosphere of Mars.
The scientist’s investigation covers issues in Meteorite, Mineralogy, Astrobiology, Mantle and Geochemistry. His work on Olivine as part of general Mineralogy study is frequently connected to Partition coefficient, therefore bridging the gap between diverse disciplines of science and establishing a new relationship between them. The Mars Exploration Program, Atmosphere of Mars and Comet research John H. Jones does as part of his general Astrobiology study is frequently linked to other disciplines of science, such as Hydrogen and Environmental science, therefore creating a link between diverse domains of science.
His study in the fields of Martian under the domain of Mars Exploration Program overlaps with other disciplines such as Sample Analysis at Mars and Rocknest. His research integrates issues of Basalt and Crust in his study of Mantle. His study looks at the relationship between Geochemistry and fields such as Chondrite, as well as how they intersect with chemical problems.
His primary areas of investigation include Astrobiology, Mars Exploration Program, Meteorite, Martian and Atmosphere of Mars. His Astrobiology study which covers Atmosphere that intersects with Carbonate. His work on Planetary geology as part of general Mars Exploration Program research is often related to Sample Analysis at Mars and Rocknest, thus linking different fields of science.
His biological study spans a wide range of topics, including Atmospheric pressure, Geochemistry, Ulvöspinel, Vanadium and Argon. In his research on the topic of Martian, Habitability is strongly related with Earth science. His work deals with themes such as Trace element and Crust, which intersect with Mantle.
His scientific interests lie mostly in Martian, Mars Exploration Program, Astrobiology, Meteorite and Sample Analysis at Mars. The various areas that he examines in his Martian study include Mantle and Crust. His Astrobiology research incorporates themes from Basalt and Earth science.
The study incorporates disciplines such as Geochemistry, Spinel and Vanadium in addition to Meteorite. His Olivine study is concerned with the field of Mineralogy as a whole. His Mineralogy research includes elements of Magnetite, Trace element and Thermodynamics.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
The Sample Analysis at Mars Investigation and Instrument Suite
Paul R. Mahaffy;Christopher R. Webster;Michel Cabane;Pamela G. Conrad.
Space Science Reviews (2012)
Geochemical constraints on core formation in the Earth
John H. Jones;Michael J. Drake.
Volatile and organic compositions of sedimentary rocks in Yellowknife Bay, Gale crater, Mars.
Douglas W. Ming;P. D. Archer;D. P. Glavin;J. L. Eigenbrode.
Oxygen fugacity and geochemical variations in the martian basalts: implications for martian basalt petrogenesis and the oxidation state of the upper mantle of Mars
Christopher D.K Herd;Lars E Borg;John H Jones;James J Papike.
Geochimica et Cosmochimica Acta (2002)
Isotope ratios of H, C, and O in CO2 and H2O of the martian atmosphere.
Chris R. Webster;Paul R. Mahaffy;Gregory J. Flesch;Paul B. Niles.
Experimental investigations of trace element fractionation in iron meteorites, II: The influence of sulfur
John H. Jones;Michael J. Drake.
Geochimica et Cosmochimica Acta (1983)
Experimental Trace Element Partitioning
John H. Jones.
Rock Physics & Phase Relations: A Handbook of Physical Constants (2013)
Experimental partial melting of the Allende (CV) and Murchison (CM) chondrites and the origin of asteroidal basalts
A.J.G. Jurewicz;D.W. Mittlefehldt;J.H. Jones.
Geochimica et Cosmochimica Acta (1993)
A nonmetal interaction model for the segregation of trace metals during solidification of Fe-Ni-S, Fe-Ni-P, and Fe-Ni-S-P alloys
John H. Jones;Daniel J. Malvin.
Metallurgical and Materials Transactions B-process Metallurgy and Materials Processing Science (1990)
The systematics of Cr (super 3+) and Cr (super 2+) partitioning between olivine and liquid in the presence of spinel
Ben Hanson;John H. Jones.
American Mineralogist (1998)
If you think any of the details on this page are incorrect, let us know.
We appreciate your kind effort to assist us to improve this page, it would be helpful providing us with as much detail as possible in the text box below: