RESOChron Dual Era Testing SystemLaser ablation (U-Th)/He thermochronology can obtain precisely defined, defect free crystal volumes with known surface areas, overcoming the two uncertainties of traditional single particle crystal measurement methods. It can perform rapid and automated U-Th-Pb He analysis on multiple mineral particles, allowing for faster, cheaper, and more conventional application of dual dating in industrial and academic research. This system is a unique instrument that can perform U-Th-Pb He triple dating and trace element characterization of minerals, measuring Pb, U, and Th through ICP-MS to obtain U-Pb ages.

Product advantages:
1. Avoid mineral or gas inclusions during the analysis process;
2. Compared to traditional methods, it has improved accuracy and precision;
3. Provide single particle geochronological age, thermochronological age, and trace element analysis for rapid dating of a large number of mineral particles;
4. No need for alpha correction (able to analyze and measure small mineral particles);
5. No need for dangerous and time-consuming mineral dissolution (HF);
6. Helium content analysis of mineral profiles can be achieved.

RESOchron method:
RESOchron is an integrated, in-situ, computer-controlled microanalysis instrument capable of rapid and automated U-Th-Pb He analysis of multiple mineral particles, measuring the volume of erosion pits through optical interferometry, X-ray computed tomography, or scanning electron microscopy.

RESOChron Dual Era Testing SystemThe main application markets include the fields of oil and mineral exploration. In addition, it has application prospects in academic research (such as structural geology and topographic evolution research) and government earth science institutions that require economical analysis of large samples (such as regional basin analysis, geochemical exploration). Compared with traditional methods, it improves accuracy and precision, does not require alpha correction (which can analyze and measure small mineral particles), and can be used faster, cheaper, and routinely in industrial and academic research to provide single particle geochronological age, thermochronological age, and trace element analysis.