THE EFFECT OF STOCK EXCHANGE REPORTING STANDARDS ON THE COMMUNICATION AND INTERPRETATION OF GEOLOGICAL DATA IN MINERALS EXPLORATION, AND THE BROADER GEOLOGICAL COMMUNITY

 

 

 

Presentation to the Prospectors and Developers Association of Canada Convention

March 2001

 

Clinton Smyth

President

Georeference Online Ltd,

Vancouver, Canada

www.georeferenceonline.com

 

 

 

Introduction                                                                                           

New reporting standards for listed Canadian exploration and mining companies, which are specified in National Instrument 43-101, come at a time when there are a number of other forces promoting standards in the minerals industry.

 

Prominent among these are the need to manage large volumes of data from different sources, and the need to share data more frequently than before, as made possible by the Internet.

 

Nevertheless, Instrument 43-101, with its obvious anti-fraud orientation, may still be seen as yet another administrative chore that cuts into the exploration geologist’s quality scientific time.

 

An alternative perspective, however, and the subject of this presentation, is that 43-101 is a welcome review of how exploration work should be recorded and reported, a review which puts the spotlight on the words and concepts used in geology, and on how they are extrapolated into the world of investment.  In this sense, 43-101 is complementary to all the other promoters of standards in geology.

 

 

National Instrument 43-101

 

National Instrument 43-101 is a law which sets conditions under which public exploration and mining companies are required to publish technical reports.  The content of the reports and the qualifications of their authors are specified by the Instrument.  The purpose of the Instrument is to ensure that securities commissions and investors are informed on technical matters materially affecting the financial status of the listed companies.  The Instrument may be viewed at the following site: http://www.chamberofmines.bc.ca/toolkit/securities/csa_ni43-101start.htm

 

In essence, 43-101 requires listed companies to provide technical audit trails which link their public statements, their work plans and results, and geology as a whole, in a rational way.

 

Computer databases are, in various roles, an increasingly important component of the audit trail required by 43-101.

 

The motivation for 43-101 was set out as follows: 

 

“The CSA believe that incremental costs of compliance with the proposed National Instrument will be outweighed by the very significant benefits provided to investors, namely more reliable and, with the use of standard terminology, more understandable and comparable public information.”

 

While the focus of this motivation was primarily on resource and reserve terminology, it is equally relevant to exploration reporting. Minerals exploration is constantly adding large volumes of data to the global geological data banks. Improved standards of reporting this data will therefore provide significant benefits to geological science in general.

 

The level of detail required by Instrument 43-101 in exploration reports is significant, as shown in Form F1, which is part of the Instrument.

 

Of particular relevance to this paper are the following sections of Form F1, which appear together with their requirements, as specified in the Instrument:

 

 

Section 9: Geological Setting - Include a description of the regional, local and property geology.

Section 10: Deposit Types - Describe the mineral deposit type(s) being investigated or being explored for and the geological model or concepts being applied in the investigation and on the basis of which the exploration program is planned.

Section 11: Mineralization - Describe the mineralized zones encountered on the property, the surrounding rock types and relevant geological controls, detailing length, width, depth and continuity, together with a description of the type, character and distribution of the mineralization

 
 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 


It should be clear that material reported under these headings, by a “Qualified Person” interested in preserving his or her reputation, is likely to be of value in the broader geological context, particularly if using terminology of a recognized standard. 

 

 

Standards

 

Historically, standards have proven difficult and slow to implement.

 

They are usually even more difficult to fund, not least because they often constitute moving targets as different interest groups make their perspectives known.  Further, standardization requirements in the computer era often have to progress from defining terminology (eg: time periods or rock-types) to considering grammars and ontologies [1]. (“Komatiites occur in the Archaean” is a grammatically and ontologically acceptable statement, while “The Archaean occurs in komatiites” is grammatically, but not ontologically, correct.)

 

This is not a new situation, although the communication made possible by the Internet has made it a more pressing one.

 

One attempt to address the problem, as it pertains to rock nomenclature, was “Classification of Rocks” published in 1955 by the Colorado School of Mines [2].  The preface to this classification system, which is still adhered to by the US Forestry Service, and some geologists in Canada, could not be more succinct:

 

 “Geologists owe it to themselves and to workers in other sciences to use standard nomenclature”.  

 

Geological standards are now, however, beginning to emerge in different forms.  Some of them are different because they are mindful of the fact that they are going to be applied, not only in scientific discussion, but also within digital databases.  This can sometimes upset the purists, but has rewards which must be taken into account during the often endless arguments about the best semantics to use.  In today’s environment, any well-defined nomenclature is better than a void left by disagreement.  The British Geological Survey Rock Classification System is a good example of a new, broadly based standard, which is sensitive to the requirements of digital systems [3].

 

Published late in 1999, this is a comprehensive new rock classification system which draws on the best of all previous rock classification schemes, and gives them expression in a way that makes them easier to use within digital databases.  The system recognises four categories of rocks: igneous, sedimentary, metamorphic and surficial cover.  It is documented in detail, and the documentation is freely downloadable on the Internet  from http://www.bgs.ac.uk/bgsrcs/ 

 

Figure 1 shows a visual representation of part of the BGS system.

 

The system’s thorough documentation and its accessibility on the World Wide Web are both crucial characteristics for any nomenclature system that a Qualified Person may wish to refer to as being the standard adhered to when fulfilling 43-101 obligations.

 

It is also very easy to navigate  -  an important “usability” consideration.   With a few mouse clicks it is possible to rapidly traverse the entire system, which includes more than 1200 rock names.

 

 

 

FIGURE 1:  Extract from the British Geological Survey Rock Classification System

 

The system’s hierarchical  design assists with understanding and navigation, but also, very importantly in the GIS field, makes legend matching and map-generalisation much more manageable tasks.

 

In contrast to the above standard, some new standards are very different from anything that most geologists encounter on paper, but are in fact paper representations of the implicit standards that geologists apply in their everyday work.  These are standards of geological grammar and ontology.  They are commonly represented using Entity-Relationship diagrams, and Universal Modeling Language diagrams  -  tools without which it is well-nigh impossible to design geological standards which measure up to the demands of the Internet age.  The North American Data Model (NADM) is one of these [4].

 

The North American Data Model is a joint US/Canadian initiative originally aimed at establishing a standard information model for geological maps, but now including in its scope broader geoscience data modeling issues.  Figure 2 shows one small part of the NADM Entity-Relationship model, and illustrates that the modeling necessary to reach the right ontologies is not simple, particularly when due consideration is given to the broad range of end-users of geological data.

 

FIGURE 2:  Extract from the Entity Relationship diagram of the North American Data Model.

 

Significant progress in standardization can, however, be made while the right ontologies are being hammered out.  In the middle 80’s the USGS published their well-known catalogue of mineral deposit types of the world  -  a list of around 100 of the “highest-level” recognisable mineral deposit types [5].  Each deposit type was characterized using standard vocabulary in the different domains of geological time, associated elements, mineralisation form, host rock, associated minerals, and various other domains.

 

Figure 3 shows a representation of part of their classification, which, again, is hierarchical, easy to navigate, and rewarding to use provided that the user is familiar with the vocabulary used by the USGS compilation.  It does not pay much explicit attention to ontology.  By careful attention to nomenclature, a universally useful database has, nevertheless, been produced.

 

 

FIGURE 3:  Hierarchical representation of data describing mineralisation models.

 

In this context, mention should be made of the FGDC standards for geological mapping which have been in development for a number of years, and which are due for release in mid-2001 [6].  These specifically address only the symbology used on geological maps (such as patterns for rock types and colours for geological time periods).  However, since they were drawn up with considerable input from the North American geological community, and since maps are such an important component of communication in geology, they should be taken into account when developing standards for other parts of the world.

 

Finally, some standards are different in the way that they are delivered  -  in that they are delivered as lookup tables on the Internet for direct inclusion into new databases. 

 

Arguably, Australia is the country most advanced in its use of standards in the earth sciences.  Figure 4 is a view of the Australian Geological Survey Organisation (AGSO) Data Dictionary web page: http://www.agso.gov.au/databases/  .  The page provides, free to users throughout the world, access to internationally relevant lookup tables, under such headings as Time Period, Lithology, Minerals, Structures, Alteration, and others which are more specific to Australia.

 

 

FIGURE 4:  Australian Geological Survey Organisation Lookup Tables World Wide Web page.

 

Crucial to the successful application of such look-up tables, is the fact that each has a custodian.  At the click of a mouse, users may make contact with the custodian.  While AGSO may admit that their lookup tables are not yet perfect  -  this kind of arrangement ensures that they will rapidly evolve to cater for most of their users’ requirements.  To ensure that they are used, the lookup tables are downloadable.

 

It is clear that many of these tables could play an important role in assisting professionals to comply with standards way beyond the shores of Australia.

 

The AGSO example provides a view of standards activity at national level.  Standards do, however, also play an important role at the state level in Australia.  For example, the South Australian Guidelines on Exploration Reporting, released in November 2000 state the following: 

 

“Release of these guidelines marks the commencement of formal requirements for digital data reporting in SA. The Department now requires one hard copy and one digital copy of the technical report until further notice.”

 

They further state:

 

 “The following standard data formats have been developed by a working group comprising representatives from all States and the Territory and in conjunction with industry. These standards which are being adopted Australia wide will provide uniformity in digital data reporting throughout Australia and will improve the efficiency of collection, storage and thus availability of data for future explorers.”

 

 

Many lookup tables similar to those of AGSO exist in Canada.  The British Columbia Geological Survey’s MINFILE system is an example ( http://www.em.gov.bc.ca/mining/geolsurv/minfile/ ).  It is also freely available, but in a somewhat less accessible form than the Australian system described above.  It is a DOS-based system which has to be downloaded in its entirety.  But once inside it, the user finds a number of useful lookup tables, each with a wordlist which can be exported, and which could, in turn, be used to standardize reports prepared under 43-101.  The extent to which these wordlists are under the explicit care of a “custodian” is not clear to the outside user.

 

In regard to statutory exploration reporting in BC at present, provincial geologists translate the partly standardised reports they receive from exploration companies and prospectors into the standardised vocabularies within the MINFILE system.   How much better might it not be to make the standards more easily accessible to those who have to prepare reports, and encourage them to do the standardising, as in the Australian model?

 

One good platform from which to encourage the use of such standards would be in the “Exploration Best Practice Guidelines” recently published by the Canadian Institute of Mining, Metallurgy and Petroleum in support of 43-101 ( http://www.cim.org/definitions/cimdef1.pdf  ).  These guidelines could endorse standard vocabularies such as those found in MINFILE, which could be made available though such initiatives as the Canadian Geoscience Knowledge Network ( http://cgkn.net ).  As in the case of the Australian standards, it is clear that they would have international relevance.

 

 

Benefits of Standards

 

There is almost always a significant resistance to the adoption of new standards, which can be overcome only by delivering advantages to those who adopt the standards.  Three advantages of standardization of geological terminology are presented below:

 

Concurrent overlay of data from different sources

More sophisticated data analysis tools

          More accurate, probably more complex, models of mineralisation

 

Each in its own way is a promoter of standards.

 

Concurrent overlaying of data from different sources, as implemented with XML, is the goal of a current CSIRO project in Perth, Australia ( http://www.ned.dem.csiro.au/xmml/ ).  XML-based real-time integration of mapping data from different sources is scheduled for implementation by the end of 2002.  However, this kind of map integration, to the extent that it incorporates qualitative data, will be ineffective if the maps to be integrated do not use consistent terminology.  Standard terminologies will reward map integrators with rapid, meaningful map integration.

 

As a second example, in the data analysis field, there is a need for tools that can automate certain of the steps in geological data analysis which currently require a geologist, and are consequently never undertaken because they take too long. 

 

Complete interpretation of multi-element geochemical borehole profiles provides a good example.  To automate anomaly recognition, “expected” compositions of lithological units are required to allow software to distinguish “noise” from significant signals such as anomalies.

 

Standardisation of rock nomenclature allows the compilation of such “expected” values, along with many other useful characteristics, which can then be used to implement advanced data analysis techniques such as anomaly recognition -  provided, of course, that the boreholes to be interpreted have also been logged using the same standards of nomenclature.

 

A final, longer term, stock exchange-relevant example of how adherence to standards makes possible better geology, may be found in the representation of mineralisation models on the computer.  It was earlier shown that much can be achieved by the judicious use of simple but comprehensive look-up tables arranged in an hierarchical manner. 

 

The same hierarchical semantics can be used to describe individual mines.  Once completed for many mines using a consistent vocabulary, this representation of geological knowledge provides a powerful environment for exploring the relationships between mineralisation model sub-types, and their expected size or grade distribution.

 

A simple illustration uses location as a distinguishing criterion for sub-type.  In Figure 5, the size distribution curve on the right was published for copper porphyry deposits by the USGS in 1986 [5].  The curve on the left was published in 1993, also by the USGS, for porphyry copper deposits from Alaska and British Columbia, showing a significantly smaller size expectation for Alaska and BC porphyries [7].

 

 

FIGURE 5:  Size distribution curves for global copper porphyry deposits and for copper porphyry deposits from British Columbia and Alaska only.

 

Consequently, with the passing of time, broader adoption of standard descriptive terminology can be expected to lead to more accurate distinctions between mineralisation models and their sub-types, and, consequently, more meaningful size and grade distribution curves.

 

 

Conclusion

 

In summary, it is clear that there are two perspectives to Instrument 43-101.  The first is that, in calling for standards-compliant descriptions of prospects, projects and mines, it should result in better mineralisation–type categorization, and more realistic size and grade expectations which, together with mining economics, fiscal regime, political risk and other factors, can lead to more reliable estimates of the values of the properties being evaluated.

 

The second is that these standards can be expected to lead to better geology allround.

 

 

 

References:

 

[1]  B. Brodaric and M. Gahegan "Geoscience Map Data Models, Open Systems GIS and Semantics," GeoCanada 2000, 2000.

[2]  R. B. Travis "Classification of Rocks," Quarterly of the Colorado School of Mines, Vol 50, No 1, 1955.

[3]  M. R. Gillespie and M. T. Styles "BGS Rock Classification Scheme. Volume 1. Classification of Igneous Rocks," British Geological Survey Report 1999.

[4]  B.R. Johnson, B. Brodaric, G.L. Raines, J.T. Hastings and R. Wahl "Digital Geologic Map Model Version 4.3," US Geological Survey Report 1999.

[5]  D.P. Cox and D.A. Singer "Mineral Deposit Models," US Geological Survey Report 1986.

[6]  Geologic Data Subcommittee of the Federal Geographic Data Committee "Public Review Draft - Digital Cartographic Standard for Geologic Map Symbolization," US Geological Survey Report 2000.

[7]  W.D. Menzie and D.A. Singer "Grade and Tonnage Model of Porphyry Cu Deposits in British Columbia, Canada, and Alaska, U.S.A.," US Geological Survey Open File Report 1993.ref_end