Prepared by:
Dr. Abdel Monem Soltan
Ph.D.
Ain Shams University, Egypt
Genetic Classification of Ore Deposits
Various geological aspects are employed to classify ore deposits, including:
1.the presence of certain metals or minerals (e.g. silver, haematite);
2.the form of the orebody (vein, bed, etc.);
3.the local geological environment (submarine or terrestrial volcanism);
4.the plate tectonic setting (island arc, continental margin) and
5.other genetic characteristics such as formation temperatures and fluid
chemistry.
However, a stringent genetic classification of mineral deposits is very difficult.
One reason for this is that many ore deposits represent a position in a complex
multi-dimensional space of well defined end members:
1.The formation of Kuroko ore deposits, for example, is an interplay of volcanic,
intrusive, sedimentary and diagenetic processes;
2.The origin of high-grade BIF-haematite ore seems to comprise sedimentation
induced by proliferating marine life, later passage of saline basinal brines and
For Further detailed classification please read:
The “chessboard” classification scheme of mineral deposits: Mineralogy and geolog
. Review Article Earth-Science Reviews, Volume 100, Issues 1–4, June 2010, Pages
1-420
Harald G. Dill
For Further detailed classification please read:
The “chessboard” classification scheme of mineral deposits: Mineralogy and geolog
. Review Article Earth-Science Reviews, Volume 100, Issues 1–4, June 2010, Pages
1-420
Harald G. Dill

Economic geology - Genetic classification of ores

  • 1.
    Prepared by: Dr. AbdelMonem Soltan Ph.D. Ain Shams University, Egypt
  • 2.
    Genetic Classification ofOre Deposits Various geological aspects are employed to classify ore deposits, including: 1.the presence of certain metals or minerals (e.g. silver, haematite); 2.the form of the orebody (vein, bed, etc.); 3.the local geological environment (submarine or terrestrial volcanism); 4.the plate tectonic setting (island arc, continental margin) and 5.other genetic characteristics such as formation temperatures and fluid chemistry. However, a stringent genetic classification of mineral deposits is very difficult. One reason for this is that many ore deposits represent a position in a complex multi-dimensional space of well defined end members: 1.The formation of Kuroko ore deposits, for example, is an interplay of volcanic, intrusive, sedimentary and diagenetic processes; 2.The origin of high-grade BIF-haematite ore seems to comprise sedimentation induced by proliferating marine life, later passage of saline basinal brines and
  • 5.
    For Further detailedclassification please read: The “chessboard” classification scheme of mineral deposits: Mineralogy and geolog . Review Article Earth-Science Reviews, Volume 100, Issues 1–4, June 2010, Pages 1-420 Harald G. Dill
  • 6.
    For Further detailedclassification please read: The “chessboard” classification scheme of mineral deposits: Mineralogy and geolog . Review Article Earth-Science Reviews, Volume 100, Issues 1–4, June 2010, Pages 1-420 Harald G. Dill