U.S. Geological Survey

Revising U.S. Geological Survey Mineral-Resource Assessment Methods

Background

As a result of public controversy over recommendations related to the wilderness preservation system, the U.S. Geological Survey (USGS) conducted a series of reviews of its mineral-resource assessment methods. The first review panel recommended several short- and long-term modifications to improve future mineral-resource assessments (Harris and Rieber, 1993). Implementation of some of these recommendations requires the development of new tools to augment USGS assessment procedures. The second panel identified the need to improve the classification of known mineral deposits according to USGS deposit models and to improve the delineation of areas that are favorable for the occurrence of particular mineral-deposit types (Barton and others, 1995).

The panels' major recommendations, however, were to develop two new tools as a first priority -- empirical rate-of-occurrence models for important mineral-deposit types (which aid in the subjective assessment of the number of undiscovered deposits in a given area) and economic cost filters.

New Tools and Methods

The principal elements in a mineral-resource assessment are shown in figure 1. On the left are earth science data on which a mineral-resource assessment is based -- a map of land tracts that may contain particular types of mineral deposits (that is, delineated tracts permissive for a particular mineral), estimates of undiscovered deposits by type, and grade-tonnage models. Resource, economic, and policy analysis tools are shown in the center of the figure, and various assessment results are portrayed on the right. Maps of delineated tracts have traditionally been made by integrating various kinds of geoscience data using descriptive mineral-deposit models. Current research is directed to developing neural network (an empirical data-driven procedure) representations of mineral-deposit models from which maps of delineated tracts can be generated. Figure 2 depicts the basic elements of the neural network representation process. The input (on the left of the figure) includes deposit and occurrence data; geochemical, geophysical, and geologic data; and historical data. These data are integrated empirically (in the center of the figure), and the output (on the right of the figure) is a map of delineated mineral-resource tracts. Figure 3 is a map of delineated tracts permissive for the occurrence of pluton-related deposits. The map was drawn by using neural network representations of mineral-deposit models. The red dots represent deposits classified by the neural model as being pluton related. By placing a 5-kilometer buffer around these deposits, a new map of tracts can be generated automatically.
Elements of a mineral-resource assesment
Figure 1. Elements of a mineral-resource assessment.

Neural network integration
Figure 2. Neural network integration of various kinds of earth science data used to delineate mineral-resource tracts.
Tracts permissive for pluton-related deposits in Nevada
Figure 3. Tracts permissive for pluton-related deposits in Nevada. This map was created by using a neural network representation of a mineral-deposit model.

Target-recognition map
Figure 4. Example of a target-recognition map. The map shows areas with enhanced probability for occurrence within a larger permissive area created by a strike-slip fault system associated with a collisional orogen.

Estimating the Number of Undiscovered Deposits

One of the two major recommendations made by the review panels was to develop improved methods for estimating the number of undiscovered deposits. There are two principal ways to accomplish this task. The first is to develop empirical rate-of-occurrence models for well-explored regions. Previous work presented empirical rate-of-occurrence models for low-sulfide quartz veins, bedded barite, diamond kimberlite pipe, and volcanogenic manganese-type deposits (Bliss and Menzie, 1993). Additional work has resulted in preliminary empirical rate-of-occurrence models for Cyprus and kuroko types of massive sulfide deposits and vein, skarn, replacement, and greisen types of tin deposits. The second is to develop procedures for recognizing mineralized targets. Figure 4, which shows the locations of several types of mineralized targets within a large permissive tract, was created by using target-recognition procedures. In this example, target recognition was based upon an understanding of the interaction of hydrothermal systems and structures that are associated with a collisional orogen.

Using Economic Cost Filters

The second recommendation by the review panels was to develop economic cost filters to facilitate the translation of physical resources into societally meaningful measures of those resources. Economic filters define the boundary in grade-tonnage space between deposits that are estimated to be economically producible at a stated rate of return and those that are not. These filters are based on the application of simplified models of mining and milling to deposits used to construct grade-tonnage models. Economic filters are used to estimate the part of the undiscovered mineral resources that may be of interest at stated conditions of price, rate of return, and location. Figure 5 shows the application of an economic cost filter to grade-tonnage data from a collection of porphyry copper deposits. Deposits shown as "Eľ" in this figure are estimated to be economic at a 10-percent internal rate of return (a 10-percent economic cost filter).
Application of economic cost filter
Figure 5. Application of an economic cost filter for porphyry copper deposits in Alaska and in British Columbia and the Yukon Territory, Canada. Deposits shown as "E" are estimated to be economic at a 10-percent internal rate of return; that is, a 10-percent economic cost filter.

Additional Methods

A geographic information system (GIS) can be used to integrate mineral-resource information to delineate areas that are permissive for the occurrence of undiscovered mineral deposits by a variety of weighting procedures. GIS can also be used to compute automatically the base rate of mineral-deposit occurrence within permissive terranes; for example, podiform chromite and Cyprus-type massive sulfide deposits within ophiolite terranes.

References Cited

Barton, P.B., and others, 1995, Recommendations for assessments of undiscovered mineral resources: U.S. Geological Survey Open-File Report 95-82, 139 p.

Bliss, J.D., and Menzie, W.D., 1993, Spatial mineral deposit models and the prediction of undiscovered mineral deposits, in Kirkham, R.V., Sinclair, W.D., Thorpe, R.I., and Duke, J.M., eds., Mineral deposit modeling: Geological Association of Canada Special Paper 40, p. 693-706.

Harris, D.P., and Rieber, Michael, 1993, Evaluation of the United States Geological Survey's three-step assessment methodology: U.S. Geological Survey Open-File Report 93-258-A, 675 p.

For more information, please contact:
Lawrence J. Drew
U.S. Geological Survey
954 National Center
Reston, VA 20192

E-mail: ldrew@usgs.gov


U.S. Department of the Interior
U.S. Geological Survey
                                                  USGS Information Handout
July 1998

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Last revised 8-28-98