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矿床地质  2010 

四川省九龙县黑牛洞韧性剪切带型浸染状铜矿石的特征及其矿床学意义

Keywords: 地质学,大陆被动边缘裂谷,韧性正剪切带,剪切带型浸染状矿石,构造改造矿床,黑牛洞铜矿床

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Abstract:

四川省黑牛洞铜矿赋存于中元古代变质火山_沉积岩中,含矿变质火山-沉积岩可能形成于扬子地台西缘大陆被动边缘裂谷带,经历了至少2次韧性变形,变质达到角闪岩相〔泥质原岩:十字石+铁铝榴石(蓝晶石),变基性火山岩:斜长石+普通角闪石+铁铝榴石〕。一方面,经构造动力作用(韧性剪切变形),原矿石经过改造形成韧性剪切带型浸染状矿石或矿化岩(简称剪切型矿石);另一方面,活化、迁移形成的含矿热液在合适的构造部位淀积成块状、准块状、角砾状和浸染状等矿石,形成以块状、准块状和角砾状硫化物为主的铜矿床。剪切型矿石的特征为:①矿石矿物和脉石矿物与围岩片理的产状基本一致,发育大量剪切条带、石英不对称透镜体和石香肠、不协调褶皱;②矿物晶体或集合体一般呈他形、透镜状;在平行片理的面(∥AB面,⊥C)上,矿石矿物集合体呈浸染状、斑点状和薄片状;在垂直片理走向的面(∥AC面,⊥B)上,则呈细条状、透镜状,甚至无根钩状,发育S∧C组构,与围岩变形特征相同;③石英动态重结晶颗粒、对称透镜体、布丁、条带和S∧C组构发育,矿石矿物集合体条带、对称透镜体、无根褶皱,以及与活化、迁移有关的溶蚀结构十分发育。研究结果表明,黑牛洞矿区发育的剪切型矿石和非剪切型矿石是同一构造过程的不同变形阶段,在不同的成矿作用和不同的地球物理化学条件下的产物。

References

[1]  Boulter C A,Fotios M G and Phillips G N.1987.The golden mile,Kalgoorlie\'a giant gold deposit localized in ductile shear zones by structurally induced infiltration of an auriferous metamorphic fluid[J].Econ.Geol.,82:1661-1678.
[2]  Chen B L,Yang N,Wu G G,Ye D J,Liu X C and Shu B.2002.Analysis of ore-controll ing structure in Ductile shear zone type gold deposits in southern Beishan area,Gansu Province[J].Mineral Deposits,21:149-158(in Chinese with English abstract).
[3]  Chen Z,Liu Y and Hodges K V.1990.The Kangmar dome:A metamorphic core complex in southern Xizeng (Tibet)[J].Science,250:1552-1556.
[4]  Davis G A and Zheng Y D.2002.Metamorphic core complexes:Definition,types and tectouie setting[J].Geological Bulletin of China,21(4-5):185-192(in Chinese with English abstract).
[5]  Du Y J and Tian J Y.1996.Structural control and evolutionary model for Liwu copper deposit[J].Journal of Sichuan Geology,16(3):213-218(in Chinese with English abstract).
[6]  Feng X L,Wang M J,Wen C M,et al.2007.The preliminary study of the exploration potential of the Liwu copper deposit and its surrounding areas,western Sichuan[J].Sedimentary Geology and Tethyan Geology,27(1):9-13(in Chinese with English abstract).
[7]  Fu Z R,Yan D P and Song H L.1997.The structure of the Jianglang metamorphic core complex in the western margin of Yangtza platform and its control on metallization[J].Acta Geologica Sinica,71(2):113-122(in Chinese with English abstract).
[8]  Gates A E.1991.Shear zone control on mineral deposits in the State-line serpentinite,Pennsylvania Piedmont[J].Ore Geology Reviews,6:171-184.
[9]  Gu L X,Yang X Q,Wu C Z,Lu J J,Xiao X J,Zheng Y C,Ni P and Tian Z M.2004.Mechanisms of Cu-Au enrichment in ore mylonites of the Hongtoushan massive sulphide deposit,Liaoning,NE China[J].Earth Science Frontiers,11(2):339-351 (in Chinese with English abstract).
[10]  Gu L X,Zheng Y C,Tang X Q,et al.2007.Copper,gold and silver enrichment in ore mylonites within massive sulphide orebodies at Hongtoushan VHMS deposit,N E China[J].Ore Geology Reviews,30:1-29.
[11]  Guilbert J M and Park C F Jr.2007.The geology of ore deposits[M].U.S.A.:Reissued by Waveland Press Inc.
[12]  Hou L W.1996.Type and origin of the core complexes and the domal deformational-metamorphic bodies in the western margin of Yangtze Craton[J].Journal of Sichuan Geology,16(1):7-11 (in Chinese with English abstract).
[13]  Hu J M,Mang Q R,Shi Y R and Qu H J.2005.SHRIMP U-Pb dating of zircons from granitoid bodies in the Songpan-Genzi terrane and its implications[J].Acta Petrologica Sinica,21 (3):867-880 (in Chinese with English ahstract).
[14]  Hua R M.1989.On the middle proterozoic rifting in China and its control over stratabound copper deposits[J].Geotectonica et Metallogenia,13(2):150-160.
[15]  Hutchinson R W and Albers J P.1992.Metsllogenic evolution of the Cordilleran region of the west United States,the Cordilleran Orogen:Conterminous U S Colorado[M].U.S.A.:The Geological Society of America.629-653.
[16]  Hutchinson R W.1993.A multi-stage,multi-process ganetic hypothesis for greenstonehosted gold lode[J].Ore Geology Reviews,8:349-382.
[17]  Kerrich R.1986.Fluid infiltration into fault zones:Chemical,isotopic,and mechanical effects[A].In:Wang C,ed.Internal structure of fault zones[J].Pure Appl.Geophys.,124 (1/2):225-268.
[18]  Li J Z,Wang M J,Yao P,Zou G F,Tang G L,Li G H,Shen Z W and Zhu X P.2006.Geology and new perspectives of the Heiniudong copper deposit and its surrounding areas in Jiulong,Sichuan[J].Sedimentary Geology and Tethyan Geology,26 (4):69-77 (in Chinese with English abstract).
[19]  Lister G S and Snoke A W.1984.S-C mylonites[J].J.Struct.Geol.,6:617-638.
[20]  Liu Y L.1996.Foreign research progress in ductile shesr-zone gold deposit[J].Gold Geology,2(3):76-80(in Chinese with English abstract).
[21]  更多...
[22]  Ma G T,Wang M J,Yao P,Li J Z,Zhu X P,Chen M H and Liang J.2009.40Ar-39Ar dating of biotite Iron the Heiniudong copper deposit in Jiulong County,Sichuan Province,and its geological significance[J].Acta Geologica Sinica,83(5):671-679(in Chinese with English abstract).
[23]  MaoJ W,Li X F,Li H M,Qu X M,Zhang C Q,Xue C J,Wang Z L,Yu J J,Zhang Z H,Feng C Y and Wang R T.2005.Types and characteristics of endogenetic metallic deposits in orogenic belts in China and their metalloganic processes[J].Acta Gologica Sinica,79(3):343-372(in Chinese with English abstract).
[24]  Marshall B and Gilligan L B.1987.An introduction to remobilization information from ore-bedy geometry and experimental considerstions[J].Ore Geology Reviews,2:87-131.
[25]  Michalski J R,Reynolds S J,Niles P B,et al.2007.Alteration mineralogy in detachment zones:Insights from Swansea,Arizona[J].Geosphere,3(4):184-198.
[26]  Pan X N,Zhao J X,Zhang X Y,et al.1988.Tectonics and rifting in Kangdian region[M].Chongqing:Chongqing Press (in Chinese).
[27]  Ramsay J S.1980.Shear zone geometry[J].Journal of Structural Geolngy,2:83-89.
[28]  Ran C Y,Zhang Z Y and Zhang W H.1994.Kangdian rift cycle,copper ore layers structure,and its evolution[J].Science in China(Series B),24(3):325-330(in Chinese).
[29]  Ran Z C and Li Z G.1984.On the structure control of copper ores in the Kunyang Group[J].Acta Geologica Sinica,4:337-347(in Chinese with English abstract).
[30]  Shen S,Jin M X and Lu Y F.1988.Mineralization law and prospect for main ore deposits in the Xichang Central Yuannan area[M].Chongqing:Chongqing Press.7-22(in Chinese).
[31]  Song H L.1995.An overview of metamorphic core complexes:Characteristics and origin[J].Earth Science Frontiers,2 (1-2):103-111(in Chinese with English abstract).
[32]  Thorne K G,Lentz D R and Hoy D.2008.Characteristics of mineralization at the main zone of the Clarence Stream gold deposit,southwestern New Brunswick,Canada:Evidence for an intrusion-related gold system in the northern Appalachian Orogen[J].Exploration and Mining Geology,17(1-2):13-49.
[33]  Wang J C,Xia B,Lei M B and Tan B F.2003.Structural control of the extensional brittle-ductile shear zone on Woxi W-Sb-Au deposit in western Hunan Province[J].Journal of Jilin University(Earth Sciance Edition),33(2):135-140(in Chinese with English abstract).
[34]  Williams M L and Bauer P W.1995.The copper Hill Cu-Ag-Sb deposit,Picuris Range,New Mexico:Retrograde mineralizatioin a brittleductile trap[J].Econ.Geol.,90:1994-2005.
[35]  Xu Z Q,Hou L W and Wang Z X.1992.Process of making mountains,Songpan-Ganzi Orogen,China[M].Baijing:Geol.Pub.House(in Chinese).
[36]  Yan D P,Song H L and Fu S R.1997.Tectonic evolution of Nyainqentanghla chain since Mesozoic in Tibet[J].Geoscience,11(3):290-297(in Chinese with English abstract).
[37]  Yang Y X,Chou D M,et al.1988.Precambrian stratabound copper deposits in Xichang-central Yunnan region[M].Chongqing:Chongqing Press(in Chinese).
[38]  Yao J D.1990.The cause of forming Liwu copper deposit[J].Journal of Sichuan Geology,10(4):251-257(in Chinese with English abstract).
[39]  Yao P,Wang M J,Li J Z,Ma G T and Zhu X P.2008.Isotopic tracing of the Liwu-type Cu-rich deposits and its ore-forming geological significance[J].Aeta Geoscientica Sinica,29(6):691-696(in Chinese with English abstract).
[40]  Zhang G L,Boulter C A and Liang J C.2001.Brittle origins for disseminated gold mineralization in mylonite:Gaocun gold deposit,Hetai goldfield,Guangdang Province,South China[J].Econ.Geol.,96:49-59.
[41]  Zhang Z B and Gao D B.1997.The knowledge of the genesis of the Shizi mountain Cu deposit,Yimen[J].Yunnan Geology,16:352-358(in Chinese with English abstract).
[42]  Zhu X P,Wang M J,Yao P,Xu J S,Li J Z,Chan M H and Tang G L.2008.Typomorphic characteristics of pyrrhofite as an ore-forming indicator of Heiniudong copper deposit[J].Acta Petrologica Sinica,24(3):562-568(in Chinese with English abstract).
[43]  Davis G A,郑亚东.2002.变质核杂岩的定义、类型及构造背景[J].地质通报,21(4-5):185-192.
[44]  陈柏林,杨农,吴淦国,叶得金,刘晓春,舒斌.2002.甘肃北山南带韧性剪切带型金矿床构造控矿解析[J].矿床地质,21:149-158.
[45]  杜亚军,田竞亚.1996.李伍铜矿床控矿构造地质特征及演化模式探讨[J].四川地质学报,3:213-218.
[46]  冯孝良,汪名杰,文成敏.2007.浅析里伍铜矿外围找矿前景[J].沉积与特提斯地质,27(1):9-13.
[47]  傅昭仁,宋鸿林,颜丹平.1997.扬子地台西缘江浪变质核杂岩结构及对成矿的控制[J].地质学报,71(2):113-122.
[48]  顾连兴,汤晓茜,吴昌志,陆建军,肖新建,郑远川,倪培,田泽满.2004.辽宁红透山块状硫化物矿床矿石糜棱岩铜金富集机制[J].地学前缘,11(2):339-351.
[49]  侯立玮.1996.扬子克拉通西缘弯状变形变质体的类型与成因[J].四川地质学报,16(1):6-11.
[50]  胡健民,孟庆任,石玉若,渠洪杰.2005.松潘.甘孜地体内花岗岩错石SHRIMP U-Pb定年及其构造意义[J].岩石学报,21(3):867-880.
[51]  华仁民.1989.中国中元古代裂谷与层控洞矿床[J].大地构造与成矿学,13(2):150-160.
[52]  李建忠,汪名杰,姚鹏,邹光富,唐高林,李贵鸿,沈战武,祝向平.2006.四川九龙黑牛洞铜矿床地质特征及其外围找矿方向初探[J].沉积与特提斯地质,26(4):69-77.
[53]  刘玉琳.1996.国外韧性剪切带型金矿研究现状[J].黄金地质,2(3):76-80.
[54]  马国桃,汪名杰,姚鹏,李建忠,祝向平,陈敏华,梁鲸.2009.四川省九龙县黑牛洞富铜矿矿床黑云母40Ar-39Ar测年及其地质意义[J].地质学报,83(5):671-679.
[55]  潘杏南,赵济湘,张选阳,等.1988.康滇构造与裂谷作用[M].重庆:重庆出版社.
[56]  冉崇英,张智筠,刘卫华.1994.康滇裂谷旋回与铜矿层楼及其地球化学演化[J].中国科学(D辑),24(3):365-330.
[57]  任主传,李宗光.1984.论昆阳群铜矿的构控性[J].地质学报,4,337-347.
[58]  沈苏,金明霞,陆元法.1988.西昌-滇中地区主要矿产成矿规律及找矿方向[M].重庆:重庆出版社.
[59]  宋鸿林.1995.变质核杂岩研究进展、基本特征及成因探讨[J].地学前缘,2(1-2):103-111.
[60]  汪劲草,夏斌,雷鸣波,谭碧富.2003.伸展型脆-韧性剪切带对沃溪钨锑金矿床的构造控制[J].吉林大学学报(地球科学版),33(2):135-140.
[61]  汪名杰,李建忠,姚鹏,等.2007.四川黑牛洞铜矿床普查地质报告[R].
[62]  吴雪桦.1991.同韧性剪切带复成热液金矿床-排山楼金矿[J].黄金地质科技,28(2):48-49,62.
[63]  许志琴,侯立纬,王宗秀.1992.中国松潘-甘孜造山带的造山过程[M].北京:地质出版社.117-136.
[64]  颜丹平,宋鸿林,傅昭仁.1997.扬子地台西缘江浪变质核杂岩的出露地壳剖面构造地层柱[J].现代地质,11(3):290-297.
[65]  杨应选,仇定茂,等.1988.西昌-滇中前寒武系层控铜矿[M].重庆:重庆出版社.
[66]  姚鹏,汪名杰,李建忠,马国桃,祝向平.2008.里伍式铜矿床同位素示踪及其成矿地质意义[J].地球学报,29(6):691-696.
[67]  姚家栋.1990.试论李伍铜矿床成因[J].四川地质学报,10(4):251-258.
[68]  张志斌,曹德斌.1997.对易门狮子山铜矿床成因的认识[J].云南地质,16(4):352-35
[69]  祝向平,汪名杰,姚鹏,徐金沙,李建忠,陈敏华,唐高林.008.四川黑牛洞铜矿床磁黄铁矿的标型特征及成矿指示意义[J].岩石学报,24(3):562-568.

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