收稿日期: 1994-02-01
修回日期: 1994-03-28
网络出版日期: 1995-02-01
基金资助
国家自然科学基金项目“斑岩铜矿床成矿作用的构造地球化学动力学研究”（编号：49303042）资助.
A SUMMARY OF RESEARCHES ON PORPHYRY COPPER DEPOSITS
Received date: 1994-02-01
Revised date: 1994-03-28
Online published: 1995-02-01
高合明 . 斑岩铜矿床研究综述[J]. 地球科学进展, 1995 , 10(1) : 40 -46 . DOI: 10.11867/j.issn.1001-8166.1995.01.0040
The main achievements of the genetic relationships between porphyry copper deposits and plate tectonics, tectonic unit, regional structure, long and deep regional fracture and hot point in the mantle are summarized. The most important characteristics of zoning of alteration and mineralization and the primary features of distribution and dips of veins in porphyry copper deposits as well as genetic views for the veins are synthesized. The significant investigations about physico-chemical coditions of rock-forming and ore-forming processes, the sources of ore-forming matter, the major genetic patterns for the deposits and some important aspects which should be studied in detail by complex sciences are show in this article.
Key words： Vein; Genetic pattern.; Porphyry copper deposit; Alteration; Mineralization
[1] 芮宗瑶等.中国斑岩铜(钼)矿床.北京:地质出版社，1984. 340.
[2] Sillitoe R H. A plate tectonic model for the origin of porphyry copper deposits. Econ Geol,1972,67:184-197.
[3] Livingston D E. A plate tectonic hypothesis for the genesis of porphyry copper deposits of the southern Basin and Range Province. Earth Planet Sci Letters,1973,20:171-179.
[4] 克里夫佐夫 A И,米加切夫 И Ф,波波夫 B C[苏].世界斑岩铜矿床.王肇芬，赵俊磊，王璞译.北京:地质出版社，1986. 265.
[5] Lowell J D. Regional characteristics of porphyry copper deposits of the Southwest.Econ Geol,1974,69:60-617.
[6] Hollister V F. Regional characteristics of porphyry copper deposits of South America. Soc Mining Engineers AIME Trans,1974,255:45-53.
[7] 冶金工业部地质研究所著.中国斑岩铜矿.北京:科学出版社，1984.
[8] Lowell J D and Guilbert J M. Lateral and vertical alteration-mineralization zoning in porphyry ore deposits. Econ Geol,1970,65:373-408.
[9] Hollister V F. Geology of the porphyry copper deposits of the Western Hemisphere. New York:Soc Mining Engineers AIME,1978,219.
[10] Sillitoe V F. The tops and bottoms of porphyry copper deposits. Econ Geol,1973,68:799-815.
[11] Titley S R and Beane R E. Porphyry copper deposits. Econ Geol 75th Annu,1981. 799-815.
[12] Titley S R ed. Advances in geology of the porphyry copper deposits of southwestern North America. Tueson: Univ Arizona Press ,1982.
[13] Hemley J J. Some mineralogical equilibria in the system K2O-Al2O3-SiO2-H2O. Am J Sci,1959,257:241-270.
[14] 朱训等.德兴斑岩铜矿.北京:地质出版社,1983. 336.
[15] 高合明.德兴斑岩铜矿床蚀变、矿化、脉体和裂隙的成因统一性研究.见:1992年中国科学院地球化学研究所矿床开放研究室年报.北京:地震出版社，1993. 191-197.
[16] Koide J and Bhattachar Ji S. Formation of fractures around magmatic in trusions and their role in ore localisation. Econ Geol,1975,70:781-799.
[17] Knapp R B and Kinght J E. Differential thermal expansion of pore fluid:fracture propagation and microear thquake production in hot pluton environments. J Geophys Res,1977,82:2515-2522.
[18] Candela P A and Holland H D. A mass transfer model for copper and molybdenum in magmatic hydrothermal fluid system: the origin of porphyry-type ore Deposits. Econ Geol,1986,. 81:1-19.
[19] Фoмиyёв В-Л等[苏]，铜—铝矿床分带性的形成机制.国外地质，1990, (1) :36-38.
/
| 〈 |
|
〉 |
甘公网安备62010202000687
