Rock Characterization for Mineral Exploration

AMICS Automated Mineralogy in Mineral Exploration

目的矿物识别和quantification through characterization of tens to hundreds of samples is difficult with the hand lens or using a petrographic microscope. Automated mineralogy allows the repeatable collection of mineralogical information at the micron, thin section and hand sample scales, providing statistically robust data that includes mineral identification and modal abundance, particle and mineral grain size distributions, mineral texture data, and more. Bruker's automated mineralogy solution is AMICS. This software may be implemented as part of two complementary solutions of direct use in mineral exploration:

Automated Mineralogy for micro-XRF

M4 TORNADO AMICSimplements Bruker's AMICS software directly on theM4 TORNADOandM4 TORNADO PLUSto allow rapid automated mineralogical scanning of minimally prepared samples that may be integrated directly with major and trace element geochemical maps. With the M4 TORNADO series of instruments being robust enough to be deployed to field offices and exploration camps, and requiring no specialist sample preparation equipment, this solution allows real time data feedback to support exploration targeting. UseM4 TORNADO AMICSto support:

Lithotyping and alteration mapping directly on drill core to enhance deposit models and validate interpretations made by visual or geochemical logging tools
Accurate identification and characterization of fine-grained ore and alteration minerals
Selection of samples for more expensive characterization techniques such as SEM-EDS mapping or SEM-based automated mineralogy
Pre-screening of samples for use in prospectivity and fertility workflows (e.g., RIMS), including analysis of stream sediment, soil or till samples without the need for exhaustive sample preparation.

Automated Mineralogy for Scanning Electron Microscope

Where mineral relationships are needed at scales below that resolved by micro-XRF,AMICS for SEMprovides the solution for mineral and rock characterization. Use SEM AMICS:

To quantify abundances of fine-grained alteration and ore minerals to build accurate deposit models
As a fundamental part of your RIMS or alteration footprint programs for local and regional vectoring and targeting
Characterization of mineral deportment aiding an evolving understanding of the target orebody to feed decisions on deposit feasibility, future mill design, and even environmental management of waste and tailings.

Integrate seamlessly with micro-XRF based geochemical and mineral characterization.

通过显微镜o-XRF for Rock Characterization

通过显微镜o-XRF for Rock Characterization in Mineral Exploration

M4 TORNADO elemental map of copper mineralization

Modern explorationists are presented with a myriad of tools to aid targeting, detection and characterization of new ore deposits. Fundamental to the exploration process is robust characterization of rocks – hand samples taken from outcrops, drill chips generated through RC drilling methods, or diamond drill core. While skillful geologists may accurately identify minerals in hand sample and create robust logs that guide sampling for geochemistry and construction of deposit models, new and evolving technologies are providing rapid and repeatable methods for rock characterization.

通过显微镜o-XRF scanning provides rapid visualization of major and trace element geochemistry at the hand-specimen and thin section scale, on minimally prepared samples. Bruker'sM4 TORNADOseries of micro-XRF instruments are rugged, allowing deployment to field sites or offices, and do not require specialist lab personnel to operate or reduce data. Use theM4 TORNADOorM4 TORNADO PLUSto enable:

rapid scanning of rough cut drill core or trays of drill chips to produce major, minor and trace element geochemical maps
quickly evaluate ore and alteration mineralogy and confirm visual logs and direct ongoing logging strategies
verify hyperspectral or other logging technology data by providing direct geochemical data at comparable scales
use geochemical maps to calculate whole rock compositions for entire samples or subdomains within scans for lithotyping and calculation of alteration indices
build data sets rapidly to provide more accurate vectoring during drilling programs, and feed deposit models for regional exploration programs.

通过显微镜o-Characterization

Characterization at the Micron Scale - Mapping by SEM-EDS

EDS elemental map of a metal reach sample

During different stages of exploration needs arise for more detailed investigations of samples that may be beyond field or forward-deployed lab solutions. Micron-scale rock and mineral characterization is commonly needed to understand complex paragenetic relationships, shedding light on the mineralizing processes and event sequences that can be used to build more comprehensive deposit models to guide ongoing exploration.

Rock and mineral characterization driven bySEM-based EDSsolutions provide:

Detailed textural and timing relationships between important ore and gangue minerals
Compositional zoning in ore-related minerals to define ore deposition events
More focused compositional analysis of fine-grained alteration products, to validate other field geochemical techniques and providing confidence in exploration models

Raman and FT-IR

Raman and FT-IR Raman and FT-IR Spectroscopy in Mineral Exploration

Adding to the arsenal of characterization techniques available in the mineral explorationist's toolkit, FTIR and Raman spectroscopy build on elemental scanning techniques to provide addition mineral chemical and structural information. Infrared and Raman spectroscopy allow accurate identification of minerals where elemental signatures are similar but their crystal structures are not. Applications include:

distinguishing specific species of alteration products such as clay, oxide or sulfate minerals, which are important for understanding alteration facies and locations in hypergene, supergene or oxide zones.
Presence of organic materials that can be important exploration indicators in some deposit environments

µXRD

In-Situ Study of Lazulite from Graves Mountain, Georgia, USA

The traditional bulk mineralogy approach is to reduce the sample to a homogenous powder and analyze with a divergent beam (Bragg-Brentano) geometry. Grinding is not always a practical option, due to rarity of a given specimen or the desire to characterize the spatial relationship of multiple phases within an assemblage. Microanalysis techniques offer the ability to analyze the sample in its native state, easing analysis of the individual constituents.