African Mineral and Energy Resources Classification and Management System (AMREC) is a continental system for management of Africa’s mineral and energy resources.

The AMREC is based on United Nations Framework Classification for Resources (UNFC) Principles, Generic Specifications and Guidelines and is aligned to Africa Mining Vision (AMV) and the Sustainable Development Goals (SDGs). Adapting to national or local needs, the AMREC provides the specifications and guidelines required for sustainable development of Africa’s mineral and energy resources.

The Kazakhstan Public Reporting Code for Exploration Results, Mineral Resources and Mineral Reserves (hereinafter - the KAZRC Code) was developed by the Kazakhstan Association of Public Reporting for Exploration Results, Mineral Resources and Mineral Reserves (hereinafter - the KAZRC Association) with the support of the Committee of Geology and Subsoil Use of the Ministry of Investments and Development of the Republic of Kazakhstan and the members of the KAZRC Association.

Казахстанский Кодекс публичной отчетности о результатах геологоразведочных работ, Минеральных Ресурсах и Минеральных Запасах (далее – Кодекс KAZRC) разработан Казахстанской Ассоциацией Публичной Отчетности о Результатах Геологоразведочных Работ, Минеральных Ресурсах и Минеральных Запасах (далее – Ассоциация KAZRC) при поддержке Комитета геологии и недропользования Министерства по инвестициям и развитию Республики Казахстан и членов Ассоциации KAZRC.

Казахстанский Кодекс публичной отчетности о результатах геологоразведочных работ, Минеральных Ресурсах и Минеральных Запасах (далее – Кодекс KAZRC) разработан Казахстанской Ассоциацией Публичной Отчетности о Результатах Геологоразведочных Работ, Минеральных Ресурсах и Минеральных Запасах (далее – Ассоциация KAZRC) при поддержке Комитета геологии и недропользования Министерства по инвестициям и развитию Республики Казахстан и членов Ассоциации KAZRC.

In contrast to the recognized man/machine system of industry, the production process of mineral resources brings about a man/machine/nature system. The dynamic evolution of this system is characterized by a steady increase in the level of human labour. This also means that labour becomes increasingly complex and complicated due to the interaction with increased automation and mechanization.

The Pan European Reserves and Resources Reporting Committee (PERC) Code for Reporting of Exploration Results, Mineral Resources and Mineral Reserves (further referred to as ‘the Code’) sets out minimum standards, recommendations and guidelines for Public Reporting of Exploration Results, Mineral Resources and Mineral Reserves in the United Kingdom, Ireland and Europe. The history of development of this code is summarised in Appendix 4.  This 2008 edition supersedes all previous editions of The Reporting Code and the IMM Reporting Code. <...>

A brief history

1991: IMM code, broadly similar to JORC
2001: “The Reporting Code” sponsored by professional bodies IMM, GSL, IGI, and EFG, and aligned with CRIRSCO
2006: Reserves committee re-formed as PERC
2008: Updated PERC Code issued

The International Template for Reporting of Exploration Results, Mineral Resources and Mineral Reserves integrates the minimum standards being adopted in national reporting codes worldwide with recommendations and interpretive guidelines for the Public Reporting of Exploration Results, Mineral Resources and Mineral Reserves. The definitions in this edition of the International Reporting Template are either identical to, or not materially different from those definitions used in the countries represented on the CRIRSCO committee <...>

Nickel, copper, and cobalt resources in undiscovered Ni-Cu deposits associated with Palaeoproterozoic synorogenic intrusions and Archaean and Palaeoproterozoic komatiitic volcanic rocks have been estimated down to the depth of one kilometre in the bedrock of Finland using the three-part quantitative assessment method. Grade-tonnage models were constructed for Finnish synorogenic intrusive deposits and komatiitic deposits using data from known Fennoscandian deposits. Twenty-six permissive tracts were delineated for synorogenic intrusive deposits, 30 for komatiitic deposits, and 15 for Talvivaaratype Ni-Zn-Cu-Co deposits.