全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
矿床地质  2003 

秦岭—祁连造山带印支-燕山期构造与大型-超大型矿床的形成关系

Keywords: 地质学,秦岭—祁连造山带,印支-燕山期构造,改造富集,大型-超大型矿床,综述

Full-Text   Cite this paper   Add to My Lib

Abstract:

印支-燕山期构造-岩浆热液活动,对秦岭—祁连造山带的区域成矿控制与影响作用十分显著。主要表现在该期北东向构造_岩浆活动不仅控制了金等矿产的形成,而且使先期形成的铜、铅锌等矿产发生了较强烈的改造和富集作用。该期北东向构造带与先期的北西、近东西向构造或含矿层交汇叠加部位,是形成大型_超大型矿床的重要条件。文章对秦岭—祁连造山带印支_燕山期构造_岩浆活动带的发育特征及其对大型_超大型矿床的控制与影响等进行了初步分析与探讨,提出了本区新一轮矿产勘查研究对策与思路。

References

[1]  任富根, 李双保, 丁世应, 等. 1998. 熊耳裂陷印支期成矿作用及其意义[J]. 矿床地质, 17(增刊): 55-58.
[2]  [19]任纪舜, 王作勋, 陈炳蔚, 等. 1999. 从全球看中国大地构造--中国及邻区大地构造图简要说明. 北京: 地质出版社.
[3]  [20]王平安, 陈毓川, 裴荣富. 1998. 秦岭造山带区域矿床成矿系列、构造-成矿旋回与演化[M]. 北京: 地质出版社.
[4]  更多...
[5]  [21]邬介人, 任秉琛, 黄玉春, 等. 1994. 西北海相火山岩地区块状硫化物矿床[M]. 武汉: 中国地质大学出版社.
[6]  [22]殷先明, 任丰寿, 徐家乐, 等. 2000. 甘肃岩金矿床地质[M]. 兰州: 甘肃科学技术出版社.
[7]  [23]张二朋, 牛道韫, 霍有光, 等. 1993. 秦巴及邻区地质-构造特征概论[M]. 北京: 地质出版社.
[8]  [24]朱俊亭, 王忠福, 刘建德, 等. 1992. 秦岭大巴山地区矿产资源和成矿规律--百万分之一秦岭大巴山地区矿产图说明书[M]. 西安: 西安地图出版社.
[9]  [1]Bureau of Geology and Mineral Resources of Gansu Province. 1989. Regional geology of Gansu Province[M]. Beijing: Geol. Pub. House(in Chinese with English abstract).
[10]  [2]Chen Y C, Wang P A and Pei R F. 1998. The metallogenic series and evolution of mineral deposits in the Qinling orogenic belt[J]. Mineral Deposits, 17(Supp..): 93~98(in Chinese).
[11]  [3]Li Y, Q S J, Ma G L, et al. 2001. The study of basic characteristic and formed condition for ultra-larger Sedex deposit in the northern part of China[A]. In: The symposium of 50s for the founding of the Changan University[C]. Beijing: The People\'s Communications Press. 94~98(in Chinese).
[12]  [4]No.6 Geological Party, Bureau of Geology and Mineral Resources of Gansu Province.. 1984. Geology of the copper-nickel sulfide deposit in the Baijiazuizi (Jinchuan), northwest China[M]. Beijing: Geol. Pub. House(in Chinese).
[13]  [5]Qi S J and Li Y. 1993. Lead-zinc metallogenic belt of Devonian system in Qinling mountains[M]. Beijing: Geol. Pub. House(in Chinese).
[14]  [6]Ren F G, Li S B, Ding S Y, et al. 1998. The Indosinian metallization and its significance in the Xionger taphrogeosyncline[J]. Mineral Deposits, 17(Supp.): 55~58(in Chinese).
[15]  [7]Ren J S, Wang Z X, Chen B Y, et al. 1999. Observing China tectonics from the global one: brief synopsis for the tectonic map of China and neighbouring countries[M]. Beijing: Geol. Pub. House(in Chinese).
[16]  [8]Wang P A, Chen Y C and Pei R F. 1998. Regional minerogenetic Series, Tectono-Minerogenic cycles and evolution in the Qinling orogenic belt[M]. Beijing: Geol. Pub. House(in Chinese with English abstract).
[17]  [9]Wu J R, Ren B C, Huang Y C, et al. 1994. Massive sulfide deposits in marine volcanic rock area in northwest China[M]. Wuhan: Press of China University of Geosciences(in Chinese with English abstract).
[18]  [10]Yin X M, Ren F S, Xu J L, et al. 2000. Geology of gold deposits in Gansu Province[M]. Lanzhou: Gansu Sci. & Techn. Pub. House(in Chinese with English abstract).
[19]  [11]Zhang E P, Niu D Y, Hou Y G, et al. 1993. Outline of the geologic-structural characteristic in the Qinling-Dabashan and neighbouring area[M]. Beijing: Geol. Pub. House(in Chinese).
[20]  [12]Zhu J T, Wang Z F, Li J D, et al. 1992. The mineral resources and minerogenetic rule in the Qinling-Dabashan area: Synopsis of the mineral resources map (one millionth) in the Qinling-Dabashan area[M]. Xi\'an: Xi\'an Cartographic Pub. House(in Chinese).
[21]  陈毓川, 王平安, 裴荣富. 1998. 秦岭造山带矿床成矿系列与演化[J]. 矿床地质, 17(增刊): 93-98.
[22]  [14]甘肃省地质矿产局第六地质队. 1984. 白家嘴子硫化铜镍矿床地质[M]. 北京: 地质出版社.
[23]  [15]甘肃省地质矿产局. 1989. 甘肃省区域地质志[M]. 北京: 地质出版社.
[24]  [16]李英, 齐思敬, 马国良, 等. 2001. 中国北方超大型热水沉积硫化矿床基本特征及形成条件研究[A]. 长安大学建校50周年学术论文集[C]. 北京: 人民交通出版社. 94~98.
[25]  [17]祁思敬, 李英. 1993. 秦岭泥盆系铅锌成矿带[M]. 北京: 地质出版社.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133