成矿系统及其演化——初步实践到理论思考

翟裕生

Volume 25 Issue 4

Jul. 2000

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Article Navigation > Earth Science > 2000 > 25(4): 333-339

ZHAI Yu-sheng, 2000. METALLOGENIC SYSTEM AND ITS EVOLUTION: FROM PRELIMINARY PRACTICE TO THEORETICAL CONSIDERATION. Earth Science, 25(4): 333-339.

Citation:

ZHAI Yu-sheng, 2000. METALLOGENIC SYSTEM AND ITS EVOLUTION: FROM PRELIMINARY PRACTICE TO THEORETICAL CONSIDERATION. Earth Science, 25(4): 333-339.

ZHAI Yu-sheng, 2000. METALLOGENIC SYSTEM AND ITS EVOLUTION: FROM PRELIMINARY PRACTICE TO THEORETICAL CONSIDERATION. Earth Science, 25(4): 333-339.

Citation:

ZHAI Yu-sheng, 2000. METALLOGENIC SYSTEM AND ITS EVOLUTION: FROM PRELIMINARY PRACTICE TO THEORETICAL CONSIDERATION. Earth Science, 25(4): 333-339.

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METALLOGENIC SYSTEM AND ITS EVOLUTION: FROM PRELIMINARY PRACTICE TO THEORETICAL CONSIDERATION

ZHAI Yu-sheng

Faculty of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2000-03-28
Publish Date: 2000-07-25

Abstract

Abstract

Mineralization system, a natural system with ore forming function often within a certain geological time space zone, includes the geological factors controlling the ore formation and preservation, the ore forming processes and their products, namely the ore deposit series and anomaly series. Based on the combination of the principal trend of metallogenic research with the author's personal study (both practice experience and academic thinking) of mineral deposits, the author considers that the study of the metallogenic system will be an important research field in metallogeny for a certain long period. From the system and history points of view, the author suggests that the metallogenic system and its evolution is one of keys to the metallogenic research. The analysis of the geological and metallogenic characteristics in China shows that the study of the evolution of the metallogenic system is of great importance to the understanding of the metallogenic patterns in China. Furthermore, a metallogenic system model is constructed, and the universal significance of boundary ore formation, transformational ore formation and coupling ore formation is stressed in this paper. Finally, the author proposes that the ore forming products include ore deposit series and anomaly series, and that attention should be paid to the study of the post mineralization changes and preservation. All the mentioned above topics are of great significance both in theory and practice.
- metallogenic system,
- structure,
- type,
- evolution,
- system analysis,
- historical analysis

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References(27)

References

[1]	王鸿祯. 中国地质科学五十年[M]. 北京: 地质出版社, 1999. 前言.
[2]	《中国矿床发现史·黑龙江卷》编委会. 中国矿床发现史·黑龙江卷[M]. 北京: 地质出版社, 1996.19~20.
[3]	翟裕生. 某斜长岩的岩石特征及成因[J]. 地质论评, 1965, 23(5): 359~364. doi: 10.3321/j.issn:0371-5736.1965.05.002
[4]	翟裕生. 侵入接触构造及其控矿作用[A]. 见: 翟裕生, 石准立, 曾庆丰. 矿田构造与成矿[C]. 北京: 地质出版社, 1981.29~44.
[5]	宁芜项目编写小组. 宁芜玢岩铁矿[M]. 北京: 地质出版社, 1978.108~118, 160~162.
[6]	翟裕生. 矿山构造学概论[M]. 北京: 冶金工业出版社, 1984. 序言.
[7]	翟裕生. 矿田矿床构造的研究内容和研究方法[A]. 见: 翟裕生, 石准立, 曾庆丰. 矿田构造与成矿[C]. 北京: 地质出版社, 1981.1~12.
[8]	翟裕生, 熊永良. 关于成矿系列的结构[J]. 地球科学———中国地质大学学报, 1988, 12 (4): 375~380. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX198704009.htm
[9]	翟裕生, 姚书振, 崔彬, 等. 成矿系列研究[M]. 武汉: 中国地质大学出版社, 1996. 1~198.
[10]	翟裕生. 矿床学思维方法的进步[A]. 见: 赵鹏大, 王亨君, 主编. 地质科学思维[C]. 北京: 地震出版社, 1993.74~84.
[11]	翟裕生. 矿床地质学的发展前景和思维方法[J]. 地学前缘, 1994, 1 (3): 1~8. doi: 10.3321/j.issn:1005-2321.1994.03.001
[12]	翟裕生. 古大陆边缘构造演化和成矿系统[A]. 见: 北京大学地质系主编. 北京大学国际地质科学学术研讨会论文集[C]. 北京: 地震出版社, 1998.769~778.
[13]	翟裕生, 邓军, 李晓波. 区域成矿学[M]. 北京: 地质出版社, 1999. 1~287.
[14]	Спижа рский Т Н. Геоло гический слова рь (Том. 2) [M ]. М: Недра, 1973.448.
[15]	Щералов В Н. Разви тие эндогенных флюидных рудооб разующах систем[M ]. Новосибрск: Наука, 1992.47~48.
[16]	Jaques L A, Wyborn L A I, Gallaghe R. The role of geo-graphic information system, empirical modelling and ex-pert systems in metallogenic research [A ]. 12th Aus-tralian Geological Convention, Geological Society of Aus-tralia Abstracts(No. 37)[C]. [s. l. ]: Perth, 1994.196-197.
[17]	於崇文. 成矿作用动力学———理论体系和方法论[J]. 地学前缘, 1994, 1(3): 5 4~82. doi: 10.3321/j.issn:1005-2321.1994.03.006
[18]	於崇文, 岑况, 鲍征宇, 等. 成矿作用动力学[M]. 北京: 地质出版社, 1998.1~23.
[19]	李人澍. 成矿系统分析的理论与实践[M]. 北京: 地质出版社, 1996.19~20.
[20]	翟裕生. 论成矿系统[J]. 地学前缘, 1999, 6(1): 13~27. doi: 10.3321/j.issn:1005-2321.1999.01.002
[21]	翟裕生. 成矿系统与综合地质异常[J]. 现代地质, 1999, 13(1): 1~7. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ901.015.htm
[22]	翟裕生. 论矿床形成后的变化与保存[J]. 地学研究, 1997, (29~30): 267~ 273.
[23]	肖荣阁, 邓军, 彭润民, 等. 华北古陆北缘西段主要成矿系统分析[J]. 地球科学———中国地质大学学报, 2000, 25(4): 362~368.
[24]	翟裕生. 成矿系列研究问题[J]. 现代地质, 1992, 6(3): 301~308. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ199203007.htm
[25]	翟裕生. 地史中成矿演化的趋势和阶段性[J]. 地学前缘, 1997, 4(4): 197~204. doi: 10.3321/j.issn:1005-2321.1997.04.005
[26]	翟裕生. 中国区域成矿若干问题探讨[J]. 矿床地质, 1999, 18(4): 323~332. doi: 10.3969/j.issn.0258-7106.1999.04.005
[27]	翟裕生. 成矿系统的结构框架模型[A]. 见: 中国科学院地球化学研究所等编. 资源环境与可持续发展[C]. 北京: 科学出版社, 1999.77~82.