成矿学的过去、现在和将来  

METALLOGENY:PAST,PRESENT,FUTURE A Personal appreciationn

作　　者：Peter Laznicka(University of Manitoba,Winnipeg,MB,Canada) 

出　　处：《地学前缘》1994年第3期9-20,共12页Earth Science Frontiers

摘　　要：成矿学起源于大约１００年前，在地学领域中已赢得了特定的地位。笔者将成矿学细分为经验成矿学、矿床成因论和应用成矿学，系统地论述了三者的关系及其发展简史，并展望了现代电子技术对成矿学研究方法的重大影响。对成矿学研究的现状和困难也做了一些分析。本文强调矿床实际资料的积累、加工、储存（信息库）和全球范围的交流。着重指出：细致描述和用图示记录目前开采矿床的重要性；用全部学识记录和处理岩石和（或）矿石样品的重要性以及利用多种文字的地区性文献（如野外报告或地质图）提供全球性资料的重要性。Metallogeny has originated about 100 years ago and it has earned its place a-mong the geoscientific fields of knowledge. It can be treatedin terms of three end-memberpremises and subdivided into empirical(of gitologie).genetic (or metallogenesis)and ap-plied metallogenies.These are,however,mutually transitional.The tools and techniquesof metallogeny have changed over the years from essentially non-quantitative written es-says and syntheses into highly quantitative,increasingly electronically presented models,yet the fundamental objectives to accumulate,preserve and utilize objective information(“facts”)for the continuous and future use of the professional community have notchanged.Points are made stressing the importance of meticulous descriptive and graphicdocumentation of the presently mined deposits;the importance of rock/ore sample recordand how to manage it in the context of the overall knowledge;and the contribution to ourglobal knowledge made by the multilingual regional literature such as field reports andmaps.As metallogeny depends on information gathered all over the world, colleaguesfrom all nations and all societies have contributed and will contribute to the success of ourprofession in a remarkably even way.

关 键 词：成矿学 经验成矿学 矿床成因论 应用成矿学 

分 类 号：P611[天文地球—矿床学]