Engineering topics

Mathew, K. J.

Publications and source records attributed to Mathew, K. J..

7 records

NASA NTRS2004

Signatures in Martian Volatiles and the Magma Sources of NC Meteorites

We report nitrogen and xenon isotopic signatures in Yamato nakhlites and use the data to assess properties of the magma source of NC meteorites in planet Mars. The Chassigny meteorite was investigated by Floran et al, who classified it as a cumulate dunite with hydrous amphibole-bearing melt inclusions with no preferred orientation of the olivines. Their inferred composition of the parent magma, which was based on electron microprobe analyses, has been questioned. The trace and minor elements in minerals were analyzed in nakhlites and in Chassigny and the authors conclude that nakhlites may represent samples from different horizons of the same lithologic unit, but that Chassigny was not co-magmatic with the nakhlites.

Marti, K.↗

NASA NTRS2004

Calibration of the Galactic Cosmic Ray Flux

We report first Xe data on the cross-calibration of I-129-Xe-129(sub n) ages with conventional CRE ages, a method which is expected to provide information on the long-term constancy of the galactic cosmic ray (GCR) flux. We studied isotopic signatures of Xe released in stepwise heating, decomposition and melting of troilites in the Cape York iron meteorite to identify isotopic shifts in Xe-129 and Xe-131 due to neutron capture in Te-128 and Te-130. We also resolve components due to extinct 129I, spallation and fission Xe. There has recently been much speculation on the constancy of GCR over long time scales, as may be inferred from iron meteorites. If GCRs originate from supernova events, this provides the basis for postulating increased fluxes at locations with higher than average densities of supernovae, specifically in OB-associations. The solar system at present appears to be inside a local bubble between spiral arms and may experience an increased GCR flux.

Mathew, K. J.↗

NASA NTRS2003

Xe-126 Excesses: Monoisotopic Anomalies in Regolith Samples?

We present new Xe isotopic signatures of Pesyanoe regolith samples which document excesses of 126Xe and we explore the possibility that it formed by low-energy reactions on transient Te-rich coatings.

Mathew, K. J.↗

NASA NTRS2003

Martian Xenology: Indigenous, Radiogenic and Fission Components

We identify Martian interior, radiogenic and fission components in recently recovered shergottites, which further constrain the differentiation and evolution of the mantle.

Marti, K.↗

NASA NTRS2002

Near-Earth Asteroid Origin for the Farmington Meteorite

We report nitrogen and xenon isotopic signatures in separated metal and non-magnetic phases of a catastrophically degassed L5 chondrite and discuss implications for the collisional event and the impactor. Additional information is contained in the original extended abstract.

Marti, K.↗

NASA NTRS2002

Fission Xenon on Mars

Fission Xe components due to Pu-244 decay in the early history of Mars have been identified in nakhlites; as in the case of ALH84001 and Chassigny the fission gas was assimilated into indigenous solar-type Xe. Additional information is contained in the original extended abstract.

Mathew, K. J.↗

NASA NTRS2000

Nitrogen Isotopic Signatures: Tracers of Relationships Among Meteorite Groups

We report N data of H- and L-chondritic metal separates, which show tight clustering and overlap the signatures of the IIE(Y) and IVA(-6) subgroups of iron meteorites.

Mathew, K. J.↗