HIP - Heidelberg Ion Probe
What is HIP?
The Heidelberg Ion Probe (HIP) laboratory is dedicated to providing isotopic analysis of geochemically and cosmochemically important solids at high spatial resolution and sensitivity. The HIP laboratory features a CAMECA ims 1280-HR ion microprobe and peripheral instrumentation for pre- and post-analysis investigation of samples. The lab is hosted in the Institute of Earth Sciences of the Heidelberg University. Instrument acquisition was funded through DFG which also oversees its operation.
History of Acquisition
The Heidelberg Ion Probe was applied for within the DFG special priority program SPP 1385 "The First 10 Million Years of the Solar System" (coordinators: Klaus Mezger, Bern, and M. Trieloff, Heidelberg).
The compelling advantages of applying for such an instrument by the SPP were
- the intrinsically urgent need for this key technology imposed by heterogeneous and ultra-small extraterrestrial samples, last but not least with respect to future sample return missions
- the fact that the SPP of which most members are not only cosmochemists but also geoscientists was the suitable scientific nucleus and field, from which a national SIMS center can emerge
In December 2014 the CAMECA 1280-HR ion probe was inaugurated by K. Remes (Deutsche Forschungsgemeinschaft - German Research Foundation) and B. Eitel, Rector of Heidelberg University. A. W. Hofmann, former director of the Max-Planck-Institut für Chemie, gave a talk about the applications of ion probes in cosmo- and geochemistry.
Merislava Anguelova presents HIP results at the GeoBremen meeting of the Deutsche Mineralogische Gesellschaft (DMG) and the Deutsche Geologische Gesellschaft - Geologische Vereinigung (Talk: „Petrology and geochronology of mylonitic high-pressure granulites from the Variscan Schwarzwald, SW Germany“)
Presentation of HIP results during the workshop „Petrochronology: Methods and Applications - RiMG Shortcourse“, European Geosciences Union, Vienna
Presentation of HIP results during the „Radiogenic and Non-traditional Isotope Short Course“, Goethe University Frankfurt
|2016/10||HIP data contribute to new study on magma storage in arc volcanoes published in Proceedings of National Academy of Science (Barboni et al. 2016: Link http://www.pnas.org/content/early/2016/10/27/1616129113.short)|
|2016/09||New geochronology results for Suvasvesi Impact Structures in Finland presented at the 79th Annual Meeting of the Meteoritical Society in Berlin (Schwarz et al. 2016: Link http://www.hou.usra.edu/meetings/metsoc2016/pdf/6297.pdf)|
|2016/02||Completion of the first two Master's theses using HIP data
Gunilla Breutmann: "U-Pb Geochronology on shocked Impact Zircons using High Resolution Secondary Ion Mass Spectrometry"
Jens Barosch: "40K-40Ca Dating of Muscovite"
Congratulations to you two!
|2016/01||First HIP ion probe publication accepted
Winfried H. Schwarz, Mario Trieloff, Klemens Bollinger, Niklas Gantert, Vera A. Fernandes, Hans-Peter Meyer, Hal Povenmire, Elmar K. Jessberger, Massimo Guglielmino, Christian Koeberl (accepted): Coeval ages of Australasian, Central American and Western Canadian tektites reveal multiple impacts 790 ka ago. Geochimica et Cosmochimica Acta.
|2015/11/11||First HIP ion probe results presented at Paneth Colloquium in Nördlingen|