Sensitive High Resolution Ion Micro-Probe
The Sensitive High Resolution Ion Micro Probe II is a high precision Secondary Ion Mass Spectrometer (SIMS). Ion microprobes make in situ isotopic and chemical 'surface' analysis of solid targets by bombarding the sample with an ion beam with a diameter of several microns typically employing Kohler focussing. The high mass resolution of SHRIMP is achieved by the use of double-focussing mass spectrometer (simultaneous energy and mass refocussing) with a very large turning radius of Magnet and Electrostatic Analyser. SHRIMP has many applications: zircon dating in copper-uranium-gold-silver deposits, uranium-lead dating of sulphur in the sulphide minerals that form metal ores, the isotopic composition of sulphur in the giant base metal ore bodies.
Oil Exploration.
Exploration of oil is a technically sophisticated and fiercely competitive international business. The cost
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What
is SHRIMP II ?
SHRIMP II
features
Applications
View ANU SHRIMP Research Laboratory
Link - SHRIMP RG Lab at Stanford University
...for further information please contact SHRIMP at ASI
The operating principle of SHRIMP is quite simple. A high-energy (10kV) beam of ions (usually O2-) is focussed onto a small area (<30 µm diameter) on the surface of the target. The ion bombardment erodes (sputters) atoms and molecules from the target, some of which are themselves ionised. These secondary ions are gathered using electrostatic lenses and transfered to a mass spectrometer, by which they are separated according to their relative masses. A limiting factor in the accuracy of all ion probe analyses is the mass spectrometer's ability to distinguish between (resolve) secondary ions of atoms and molecules that are extremely similar in mass (isobars).
In the secondary ion spectra of complex compounds, isobars with fractional mass differences of <3 x 10-4 are common. The high mass resolution of SHRIMP is achieved by the use of double-focussing mass spectrometer (simultaneous energy and mass refocussing) with a very large turning radius (magnet radius 1 m, electrostatic analyser radius 1.27 m) The resulting instrument has a beam line over 7 m long and weighs more than 12 tonnes.
The SHRIMP II Sensitive High Resolution Ion Micro Probe, developed, manufactured, and marketed by Australian Scientific Instruments (ASI), is a fully commercial version of an instrument originally designed for geological research purposes and constructed by the Research School of Earth Sciences (RSES) at the Australian National University (ANU).
The SHRIMP II ion microprobe is a high precision scientific instrument in the broad category of Secondary Ion Mass Spectrometers (SIMS). Ion microprobes make in situ isotopic and chemical 'surface' analysis of solid targets on the scale of a few thousandths of a millimeter by bombarding the sample on a very fine scale, and eliminate the difficult, time-consuming, labour-intensive and potentially hazardous aspects of sample preparation for conventional mass spectrometry.
SHRIMP II, like other ion microprobes, obtains material for analysis by bombarding a sample surface with a finely focused beam of high energy atomic particles (ions). The ion bombardments slowly wear away a small portion of the surface, producing electrically charged atoms and molecules of the sample that can be separated by mass, identified and counted by an attached mass spectrometer.
The quality of the instrument can be assessed by its sensitivity (ability to detect trace elements present in the target at low concentrations) and mass resolution (ability to distinguish between ions of very similar mass). SHRIMP II has the highest sensitivity at high mass resolution of any commercial ion microprobe.
Primary Ion Beam
Sample Stage
Secondary Ion Beam
- 90 degree angle extraction of the secondary beam to minimise instrumental discrimination.
- Large apeture eliminates sample-to-sample memory Low field gradient extraction minimizes inter-element discrimination.
- Triple quadrupole lens matching of secondary beam for maximum transmission.
- Simultaneous collection of secondary and mass analysed beams for maximum precision of analysis.
- Large (1272mm) radius electrostatic analyser.
- Rotatable source slit, width continuously variable from 5µm to 150µm.
- Isotopic mapping of samples accomplished by rastering sample beneath primary beam.
- Elegant, simple integrated ion lens system minimizes beam abberations and simplifies operation.
- High mass dispersion achieved with large (1000mm) radius sector electromagnet.
- Very stable, high speed laminated electromagnet controlled by multiple.
- Hall Effect probes Resolution > 5000 (1% definition) with flat-tops for 80µm source slit and 100µm collector slit.
- Sensitivity better than 18cps/ppm/206Pb/nA 02- under above conditions
Collector
- Rotatable collector slit, width continuously variable from ~5µm to 300µm.
- Ion counting with robust, high gain, high speed electron multiplier, or
- Ion current measurement via Faraday cup and electrometer.
Instrument Control
- Macintosh platform standard.
- Entire vacuum system under microprocessor control.
- Highly intuitive, easy-to-use graphically orientated operation of entire machine.
- Examining stellar nucleosynthesis.
- Calibrating the Palaeozoic time-scale.
- Dating of the Earth's oldest crust.
- Examining the oldest zircons in the solar system.
- Measuring trace elements in diamond inclusions.
- InvestigatingTi isotopic ratios in meteorites.
- Determining Pb isotopic composition of lunar granites.
Mineral Exploration.
SHRIMP zircon dating has led to improved understanding, for example, of the timing and origins of mineralisation of the giant Olympic Dam copper-uranium-gold-silver deposit in South Australia, gold-copper deposits in tennant creek area of the Northern Territory, the gold and nickel deposits of Western Australia and Canada.
The versitility of SHRIMP in fields of other than uranium-lead dating has been illustrated graphically by probing the composition of sulphur at the micro scale in the sulphide minerals that form metal ores. Vital new understanding of the origin of mineral deposits around the world has resulted.
The isotopic composition of sulphur in the giant base metal ore bodies which supply most of the world's copper, zinc, lead and silver is sensitive to whether that sulphur is derived from sediments or from hot fluids originating deep in the Earth. Knowing the source of the sulphur for each ore body helps in determining why metals were deposited and directs the exploration strategy adopted in the search for new ore bodies.
Oil Exploration.
Exploration of oil is a technically sophisticated and fiercely competitive international business. The cost of trial wells, often dry is huge, and millions of dollars are saved if location of oil can be predicted more accurately prior to drilling. The same applies to finding mineral deposits such as gold, copper and nickel ores buried deep underground. The exploration industry therefore relies increasingly on modelling how, where, and when these commodities form and become trapped in rock structures, so as to target drilling in a risk-efficient pattern.
Geologists learn about oil and mineral formation by close study of the crystals that form rocks. One key mineral is zircon, a crystal just a few thousandths of a millimeter in size that contains trace amounts of uranium (typically one hundred parts per million). The time of formation of rocks and mineral deposits can be measured in millions of years from the progress of the uraniums natural and regular radioactive decay to form lead. This gives vital information on when rocks crystallised, when mineral deposits where emplaced, and when traps suitable for oil were being formed.
Zircons have several concentric zones of growth, rather like tree rings, indicating they have crystallised in stages over periods of many millions of years. Conventional methods of dating zircons involve chemically dissolving the crystals in a beaker, and placing the solution in a mass spectrometer for measurement of the amount of lead that has formed from uranium decay. This unavoidably blends all the zones and masks the growth history of the crystal.
The science of dating therefore urgently needed a new type of mass spectrometer capable of probing, and dating, the individual zones of crystals. SHRIMP II was developed in response to this need.
In regards to oil and gas exploration, a clear need exists for accurate calculation of rates of basin substance, sedimentation and sea level change and their correlation with crystal movements. In sediments which carry no fossils to aid dating, such calculations have carried unacceptable levels of error. SHRIMP zircon dating is bring a new level of accuracy to the study of the process that form the sedimentary basins.