The mineralogy of a planetary surface can be used to identify the provenance of soil or sediment and reveal the volcanic, metamorphic and/or sedimentological history of a particular region. We have discussed elsewhere the applications and the instrument design of possible X-ray diffraction and X-ray fluorescence (XRD/XRF) devices for the mineralogical characterization of planetary surfaces. In this abstract we evaluate some aspects of sample-detector geometry and sample collection strategies
The power of mineralogical analysis as a descriptive or predictive technique stems from the fact tha...
Sedimentary rocks at Yellowknife Bay (Gale Crater) on Mars include mudstone sampled by the Curiosity...
The Mars Science Laboratory rover Curiosity scooped samples of soil from the Rocknest aeolian bedfo...
An ultra-miniaturised (mass 1.5 kg; volume ~22 × 6 × 12 cm3) instrument which combines X-ray diffrac...
The legacy of planetary X-ray Diffraction (XRD) and X-ray Fluorescence (XRF) began in 1960 when W. P...
To obtain detailed mineralogy information, the Mars Science Laboratory rover Curiosity carries CheMi...
In the context of the exploration of Mars, the availability of an instrument for in-situ mineralogic...
A system is described suitable for remote low power mineralogical analysis of lunar, planetary, or a...
Abstract: In the context of the exploration of Mars, the availability of an instrument for in-situ m...
By employing an integrated x-ray instrument on a future Mars mission, data obtained will greatly aug...
The Mars Science Laboratory Curiosity landed in Gale crater in August 2012 with the goal to identify...
Our joint research effort was aimed at developing techniques for X-ray diffractometry that was being...
X-ray fluorescence (XRF) spectroscopy is a well-established and commonly used technique in obtaining...
In situ analysis of rock chemistry is a fundamental tool for exploration of planets. To meet this ne...
Many planetary surface processes leave evidence as small features in the sub-millimetre scale. Curre...
The power of mineralogical analysis as a descriptive or predictive technique stems from the fact tha...
Sedimentary rocks at Yellowknife Bay (Gale Crater) on Mars include mudstone sampled by the Curiosity...
The Mars Science Laboratory rover Curiosity scooped samples of soil from the Rocknest aeolian bedfo...
An ultra-miniaturised (mass 1.5 kg; volume ~22 × 6 × 12 cm3) instrument which combines X-ray diffrac...
The legacy of planetary X-ray Diffraction (XRD) and X-ray Fluorescence (XRF) began in 1960 when W. P...
To obtain detailed mineralogy information, the Mars Science Laboratory rover Curiosity carries CheMi...
In the context of the exploration of Mars, the availability of an instrument for in-situ mineralogic...
A system is described suitable for remote low power mineralogical analysis of lunar, planetary, or a...
Abstract: In the context of the exploration of Mars, the availability of an instrument for in-situ m...
By employing an integrated x-ray instrument on a future Mars mission, data obtained will greatly aug...
The Mars Science Laboratory Curiosity landed in Gale crater in August 2012 with the goal to identify...
Our joint research effort was aimed at developing techniques for X-ray diffractometry that was being...
X-ray fluorescence (XRF) spectroscopy is a well-established and commonly used technique in obtaining...
In situ analysis of rock chemistry is a fundamental tool for exploration of planets. To meet this ne...
Many planetary surface processes leave evidence as small features in the sub-millimetre scale. Curre...
The power of mineralogical analysis as a descriptive or predictive technique stems from the fact tha...
Sedimentary rocks at Yellowknife Bay (Gale Crater) on Mars include mudstone sampled by the Curiosity...
The Mars Science Laboratory rover Curiosity scooped samples of soil from the Rocknest aeolian bedfo...