Exploration drilling turns the unknown into the known. This “core” activity is perhaps one of the most valuable assets in the mineral exploration workflow. Core extracted during diamond drilling is typically described by skilled geologists and along with geotechnical characterization is subjected to additional geochemical and mineral analysis.
Bruker is pioneering new technologies and methods to extract more useful and scalable information from core, aiding geologists on the ground and in the exploration office. As a critical link to the subsurface, core analysis is the best opportunity to characterize the products of mineralization and alteration, from the ore body scale to the sub-grain scale, allowing development of refined ore system process models. Non-destructive and minimally destructive tools can characterize elemental concentration, mineralogy, and texture to construct 3D subsurface deposit models and constrain predictive exploration strategies.
Non-destructive elemental and mineral logging of core provides objective high-resolution analytical data to identify sweet spots, mineralization, and alteration. Bruker portable and handheld analyzers are used to collect depth-registered geochemical and mineralogic data in the field or the core shack. The high-resolution nature of this data means that even small prospective zones of mineralization or alteration can be identified without dilution, improving distal identification of ore systems. Field collection of data provides near-instantaneous geochemistry that can be used for:
Visualization of the spatial distribution of major, minor and trace elements in core feeds an understanding of the processes of mineralization and alteration. Micro-XRF provides large-sample geochemical mapping at resolutions less than <20µm that can contextualize features within a geologic process framework. The addition of automated mineralogy to micro-XRF is an emerging field that promises to add the new dimension of rapid and repeatable petrologic characterization. For core analysis Bruker’s M4 TORNADO series of instruments can be set for rapid data collection on-site or in the core shack:
Geology happens over a large scale. Small inclusions and thin veins can be measured to determine a rock's scientific value or which mining-relevant elements are present. It is however the bigger picture of gradual changes in minerology over meters, if not kilometers, that tells the tale of the rock’s formation and geological history.
Differences in the elemental composition of drill cores and other geological samples can be used to determine information about a samples value, geological history and the processes by which it was formed.
Elemental mapping allows for the identification of different types of minerals within a sample as well as the location and measurement of phenomena such as veins, which can be used to establish the sample's value and the different geological conditions that the sample experienced over its lifetime.
Micro-XRF allows for the high-resolution elemental mapping of drill cores and geological samples. The use of the M6 JETSTREAM, which has a sampling area of 800 x 600 mm², facilitates the non-destructive analysis of many pieces of drill cores at once or for the full scanning of large samples - allowing geologists to access rich information about a samples composition or history without having to destroy or damage it.
The following Lab Report describes the use of the M6 JETSTREAM for the compositional analysis of a large granite sample from the Vredefort Dome, a 300km wide impact crater in South Africa.
Many mineralization processes leave a record at the micron scale. Scanning electron microscopy (SEM) characterization is the most accurate method available to visualize and analyze processes at this scale. Bruker’s automated mineralogy and large area elemental mapping solutions by automated EDS X-ray mapping with backscatter election (BSE) imaging, provides detailed analysis at resolutions down to ~1 µm. Click here to learn more about rock characterization for exploration with microanalysis.
Traditional mineral analysis of rocks views a 3D world in 2D. Analysis of thin sections and core slabs in optical microscopes, SEMs and micro-XRF all require extrapolation from a single plane to understand a 3D object. High-resolution 3D X-ray Microscopy studies on core allow for non-destructive observations of the third dimension. Bruker’s SKYSCAN series of X-ray microscopes works with other methods to produce detailed information on the shape, size and inter-relationships of geologic features. When combined with automated mineralogy from SEM or micro-XRF the possibility opens to develop fully comprehensive models of ore distribution at the micron-scale, better defining mineralization processes and predict comminution and other processing behaviors.