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哈密地区铜镍金成矿系统和成矿动力学探讨
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摘要
成矿系统是指在一定的时空域中,控制矿床形成和保存的全部地质要素和成矿作用动力过程,以及所形成的矿床系列、异常系列构成的整体,是具有成矿功能的一个自然系统。成矿动力学,是指在一定的地质构造背景下,研究矿床分布规律、形成过程和作用机理的学科。具体而言,是从构造背景、成矿空间、成矿演化、矿质散聚、深部作用和成矿环境等角度探讨挤压、引张和剪切动力作用下的成矿系统、成矿序列、矿化类型、矿化特征和成矿机理。
     通过探讨研究区铜镍金成矿系统及其成矿动力学,可以从整体上了解该地区的成矿作用,各个成矿要素互相的影响,确定成矿构造背景、成矿流体、动力过程和产物等的整体变化过程。使矿床的研究从静态到动态、单个矿床到系列矿床、从定性到定量,从多方面搞清成矿要素的相互影响、整体演化对成矿作用的控制,从而逐步缩小靶区,找出缺位的矿床或类型。
     本文以东天山哈密地区铜镍金矿床为研究对象,以研究区的成矿系统和成矿动力学为研究方向,在系统收集、整理东天山以往区域地质调查、矿床勘探与科学研究资料的基础上,对区内成矿地质、地球物理、地球化学条件进行了综合分析,对金、铜、铜-镍的成矿系统进行了初步的划分探讨,总结了大量前人研究的基础上,在考虑铜镍金矿成矿类型、矿床成因、矿化组合以及赋矿地层和含矿建造的基础上将东天山哈密地区的铜镍金矿床成矿系统主要划分为岩浆岩成矿系统、金成矿系统、铜多金属成矿系统和铜-镍成矿系统几个系统类型,同时又将各个成矿系统划分为几个相应的子系统类型并进行了典型矿床的研究;成矿动力学主要包括构造动力成矿作用、岩浆动力成矿作用、变质动力成矿作用、沉积动力成矿作用,本文主要从构造动力成矿作用这一方面入手对研究区成矿动力学进行了相关的探讨。在以上基础上总结出时-空上东天山哈密地区的金铜镍成矿规律,包括区域构造、区域岩浆、区域地层、区域变质作用与成矿的关系。
Metallogenic system refers to in the certain space-time domain, which control the formation and save all geological elements and mineralization dynamic process of the deposit, and the deposits series, abnormal series composition as a whole,it is a natural system with metallogenic function. Metallogenic dynamics, it is a subject point to in certain geological tectonic background, which study on ore deposit distribution mechanism, the formation process and the disciplines. Specifically, it is a discussion of metallogenic system, metallogenic series, mineralization type, mineralization characteristic and mineralization mechanism in extrusion, tensile and shear force with the metallogenic tectonic background, metallogenic space, metallogenic evolution, mineral scattered gathers, the deep effect and metallogenic environment aspects discuss of
     With he discussion of Metallogenic system and Metallogenic dynamics Copper-Nickel-Gold of Hami,we can understand the mineralization in this region and the influence of different metallogenic element each other,to make sure the overall change of the metallotectonic background, metallogenic fluid, dynamic process and products.To make the research of deposit from static to dynamic,from single deposit to series deposits and from qualitative to quantitative ,and to find out the interaction between metallogenic elemets and the overall evolution of the mineralization controls, thus gradually narrowing target area, find out the deposit or absence types.
     This paper makes Copper-nickel-gold deposits of Hami as the research object,and makes Metallogenic system and Metallogenic dynamics as the research direction,on the basis of systematic collection the previous regional geological survey, ore exploration and scientific research date of East Tianshan, comprehensive analysis the geological,geophysical and geochemical conditions of this ragion.Gave a preliminary classification of the metallogenic system of the Copper-Nickel-Gold deposits.Summarized on the basis of a large number of previous studies, in considering the type, genesis, composition and ore mineralization and ore-bearing formation of Copper-Nickel-Gold deposits,the main metallogenic of Copper-Nickel-Gold deposits of system of Hami region is divided into magmatic system and gold metallogenic system, copper and copper polymetallic metallogenic system and Copper-Nickel metallogenic system, in the same time everyone will also be divided into several different sub-metallogenic system and do some research of the typical deposits. The Metallogenic dynamics include tectonic mineralization, magma motive power mineralization, metamorphic dynamic mineralization, sedimentary dynamic ore-forming processes, in this paper we will disscuss the Metallogenic dynamics in tectonic mineralization aspect. On the basis of the above research ,thia paper gave a summary of the Copper-Nickel-Gold mineralization law of Hami of East Tianshan in time-space, including the relationship between regional tectonics, regional magma, regional strata, regional metamorphism and metallogenic.
引文
[1]朱创业.成矿系统研究现状及发展趋势[J].成都理工学院学报.2000,27(1):50-53.
    [2]翟裕生,邓军,李晓波.区域成矿学[M].北京:地质出版社.1999.
    [3]芮宗瑶,王龙生,王义天.成矿系统的始态、终态及其过程.矿床地质[J].2002.21(2):137-147.
    [4]邓军,杨立强,翟裕生,陈学明.构造-流体-成矿系统及其动力学的理论格架与方法体系[J].地球科学,2000,25(1):71-77.
    [5]李俊.易门铜矿区西矿带喷流沉积成矿与改造期成矿动力学研究[D].昆明理工大学,1999.
    [6]李德威.成矿动力学刍议[J].地球科学—中国地质大学学报,1993,18(4):407-413.
    [7]於祟文,岑祝等.成矿作用动力学[M].地质出版社,1998.
    [8]翟裕生,王建平,邓军,彭润民.成矿系统与矿化网络研究.矿床地质[J].2002,21(1):106-112.
    [9]陈世平.新疆研究区矿产资源成矿规律及评价研究[D].中国地质科学院,2006.
    [10]张良臣、刘德权等编著:中国新疆优势金属矿床成矿规律[M].地质出版社.P446.
    [11]高珍权.东天山铜金多金属成矿学及找矿系统工程学[D].中南大学,2002.
    [12]杨兴科,程宏宾,姬金生,罗桂昌,陶洪祥,东天山金铜成矿背景与成矿系统分析[J].西安工程学院学报.2000,22(2):7-13.
    [13]毛景文,杨建民,韩春明,王志良.东天山铜金多金属矿床成矿系统和成矿地球动力学模型[J].地球科学——中国地质大学学报.2002,27(1):413-423.
    [14]姬金生,薛春纪,曾章仁,等.新疆东天山康古尔塔格金矿带研究[J].地质论评,1997, 43(1): 69-77.
    [15]李华芹,谢才富,常海亮.新疆北部有色贵金属矿床成矿作用年代学[M].北京:地质出版社,1998.
    [16]姬金生,陶洪祥,曾章仁,杨兴科等,东天山康古尔塔格金矿带地质与成矿[M].北京:地质出版社,1994. 204
    [17]张连昌,姬金生.西滩浅成低温热液金矿成矿地质地球化学动力学[J].西安工程学院学报,1999, 21(2):13-18.
    [18]薛春纪,姬金生,曾章仁.东天山康古尔金矿带金矿床基本类型及成矿规律[J].西北地质,1995,16(4): 30-36.
    [19]张连昌,姬金生,曾章仁,等.东天山康古尔金矿成矿物质的同位素地球化学特征[J].现代地质,1998,12(3):380-387.
    [20]丰成友,姬金生,薛春纪,等.东天山西滩浅成低温热液金矿床地质及其成因分析[J].新疆地质,1999,17(1):1-7.
    [21]庄泽道.新疆东天山成矿地质条件与综合信息预测模型研究[D].吉林大学,2005.
    [22]张连昌,秦克章,沈远超,姬金生.东天山康古尔金矿碰撞造山成矿作用的地质地球化学[J],东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001.
    [23]马天林,杨建民,孙丽倩等.土屋铜矿成矿过程与东天山矿产分布[A],东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001,129-131。
    [24]王福同,庄道泽,胡建卫,等.物探在新疆土屋地区铜矿床找矿中的应用[J].中国地质,2001, 28(3):40-46.
    [25]刘德权,唐延龄,周汝洪.新疆斑岩铜矿的成矿条件和远景[J].新疆地质,2001,19(1): 42-48.
    [26]朱裕生.新疆东天山土屋式斑岩铜钼伴生银矿床[J].矿床地质,2002.
    [27]李华芹,陈富文,蔡红等.新疆东部马庄山金矿成矿作用同位素年代学研究[J].地质科学,1999,34(2):251-256.
    [28]李凤鸣,王宗社,侯文斌.东天山小热泉子铜矿床综合找矿模型的建立[J].新疆地质.2002,20(1),38-43.
    [29]徐兴旺.东天山哈密地区镁铁质-超镁铁质岩浆有序侵位与铜镍成矿[R].国家自然科学基金申请书.中国科学院地质与地球物理研究所,2007.
    [30]於祟文,岑祝等.成矿作用动力学[M].地质出版社,1998.
    [31] Cathles,L.M, Floud flocw and genesis of hgdnthenmal ore deposits[J].Econ.Geol., 1981,75th ann.Vol.,424-457.
    [32]於崇文,蒋耀淞.云南个旧矿区锡石一硫化物矿床原生金属分带形成的动力学机制[J].地质学报. 1990,64(3):226-237.
    [33]鲍征宇.垂直裂隙中热热驱动流体对流的发生和稳定性及其热液成矿作用意义[J].地球科学,1992,17卷(增刊):57-67.
    [34] Romeno.L.Neretnieks,l.,Moreno,L. Morement of the redox front at the Osaum Utusmi uranium mine,Pocos de Caldes.Brezil. [J].Geochem.Explor. 1992,45:471-502.
    [35]於祟文,岑祝等.成矿作用动力学[M].地质出版社,1998.
    [36]李俊.易门铜矿区西矿带喷流沉积成矿与改造期成矿动力学研究[D].昆明理工大学,1999.
    [37]周济元,茅燕石,黄志勋,等.东天山古大陆边缘火山地质[M].成都:成都科技大学出版社,1994. 1-280.
    [38]姬金生,杨兴科,苏生瑞.东天山康古尔塔格金矿带成矿条件分析[J].地质找矿论丛,1994, 9(4): 49-56.
    [39]张良臣,吴乃元.天山地质构造及演化史[J].新疆地质,1985, 3(3): 1-14.
    [40]芮宗瑶,王龙生,王义天,等.东天山土屋和延东铜矿时代讨论[J].矿床地质,2002, 21(1): 16-22.
    [41] Chen C, Lu.H, Jia. D, etal. Closing history of the southern Tianshan oceanic basin, western China: anoblique collisional orogeny [J]. Tectonophysics, 1999,302: 23-40.
    [42]陈毓川,王登红,朱裕生,等.中国成矿体系与区域成矿评价[M],北京:地质出版社,2007,1-450.
    [43]娄德波.新疆东天山铜镍矿资源潜力评价方法研究[D].中国地质科学院,2008.
    [44]薛春纪,陈毓川,姬金生等.东天山矿床成矿系列和分布规律[J].东天山铜多金属矿床成矿过程和成矿动力学及找矿预测新技术新方法会议,2001,60-62.
    [45]秦克章,方同辉,王书来等.东天山板块构造分区演化与成矿地质背景研究[J].新疆地质,2002,20(4):302-308.
    [46]冯益民,朱宝清,杨军录,张开春.东天山大地构造及演化-1:50万东天山大地构造图简要说明[J].新疆地质,2002,20(4):309-314.
    [47]秦克章,彭晓明,三金柱等.东天山主要矿床类型成矿区带划分与成矿远景区优选[J].新疆地质,2003,21(2):143-150.
    [48]芮宗瑶,刘玉琳,王龙生等.新疆东天山斑岩型铜矿带及其大地构造格局[J].地质学报, 2002,1:83-94,62(3):257-267.

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