CAMECA

CAMECA offers unique instrumentation for elemental & isotopic microanalysis at the micro, nano and atomic scale. Our SIMS, APT and ECR sources cover numerous applications in geology and geochemistry, environmental microbiology, mining… They have been adopted by top ranking research institutes to track geological processes using stable isotopes, determine the presence and distribution of trace elements, date minerals...

Download your free tutorial on Dynamic Secondary Ion Mass Spectrometry to understand its advantages over alternative surface analysis techniques and how to use it widely.
The IMS 1300‑HR³ brochure features multiple application data in the fields of geochemistry, paleoclimate reconstructions, environmental research and introduces the specifics of Large Geometry SIMS instrumentation
SUCCESS STORY - Our NanoSIMS user at Caltech: Dr Orphan and her team investigate the anabolic activity patterns of marine symbiotic micro-organisms. Findings triggered a surprising new hypothesis!
Download your free tutorial on Dynamic Secondary Ion Mass Spectrometry to understand its advantages over alternative surface analysis techniques and how to use it widely.
The IMS 1300‑HR³ brochure features multiple application data in the fields of geochemistry, paleoclimate reconstructions, environmental research and introduces the specifics of Large Geometry SIMS instrumentation
SUCCESS STORY - Our NanoSIMS user at Caltech: Dr Orphan and her team investigate the anabolic activity patterns of marine symbiotic micro-organisms. Findings triggered a surprising new hypothesis!
The study reveals a laser‑assisted evaporation mechanism improving atom probe analysis of insulating oxides, enabling nanoscale characterization of oxide‑rich mineral phases and expanding geoscience research possibilities.
WEBINAR: “Matrix effects and mineral characterization on LG‑SIMS,” a key challenge in SIMS quantification. Laure Martin (UWA) explains their origins, impact on accuracy, shows practical examples, and shares recommendations to improve user analyses.
BLOG: Discover how Earth’s hydrological cycle began over 4 billion years ago. Using oxygen isotope analysis in ancient zircon grains, researchers reveal early water–rock interactions that shaped our planet and created conditions for life.
The study reveals a laser‑assisted evaporation mechanism improving atom probe analysis of insulating oxides, enabling nanoscale characterization of oxide‑rich mineral phases and expanding geoscience research possibilities.
WEBINAR: “Matrix effects and mineral characterization on LG‑SIMS,” a key challenge in SIMS quantification. Laure Martin (UWA) explains their origins, impact on accuracy, shows practical examples, and shares recommendations to improve user analyses.
BLOG: Discover how Earth’s hydrological cycle began over 4 billion years ago. Using oxygen isotope analysis in ancient zircon grains, researchers reveal early water–rock interactions that shaped our planet and created conditions for life.

Ulrich Ehrke

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Flore Barbier

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