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...

华南印支期产铀和非产铀花岗岩黑云母矿物化学成分差异

, PP. 270-277

Keywords: 印支期花岗岩,黑云母,铀成矿,华南

Full-Text   Cite this paper   Add to My Lib

Abstract:

华南印支期花岗岩与铀成矿关系密切。根据花岗岩赋存铀矿的能力,将华南印支期花岗岩分为产铀花岗岩和非产铀花岗岩。前者以诸广山岩体和大富足岩体为代表,后者以白马山岩体和瓦屋堂岩体为代表。利用黑云母电子探针矿物化学成分来研究产铀与非产铀花岗岩的特征和差异,进一步指导华南印支期花岗岩的铀矿找矿勘探工作。与非产铀花岗岩相比,产铀花岗岩具有如下特征:黑云母蚀变程度强,包裹的副矿物较多;黑云母中SiO2、TiO2、Fe2O3、MgO的含量较低,Al2O3、F、FeO的含量较高;黑云母均为铁叶云母,ⅥAl3+和Fe2+高;花岗岩类型为过铝质花岗岩,来源于泥质地壳;并且花岗岩的氧逸度低、成岩温度低。这些特征是判别华南印支期花岗岩产铀潜力的重要标志。

References

[1]  安芳, 朱永峰.2009.新疆西准噶尔包古图组凝灰岩锆石SHRIMP年龄及其地质意义.岩石学报, 25(6): 1437-1445.
[2]  白文吉, Robinson P, 杨经绥, 周美付, 胡旭峰. 1995. 西准噶尔不同时代蛇绿岩及其构造演化.岩石学报,11(增1): 62-72.
[3]  冯益民. 1985. 西准噶尔优地槽褶皱带沉积建造特征及其多旋回发展. 西北地质科学, 9: 13-19.
[4]  郭丽爽, 刘玉琳, 王政华, 宋达, 许发军, 苏犁. 2010. 西准噶尔包古图地区地层火山岩锆石LA?ICP?MS U?Pb年代学研究. 岩石学报, 26(2): 471-477.
[5]  何国琦, 刘建波, 张越迁, 徐新. 2007. 准噶尔盆地西缘克拉玛依早古生代蛇绿混杂岩带的厘定. 岩石学报, 23(7): 1573-1576.
[6]  贾小辉,王强,唐功建. 2009. A型花岗岩的研究进展及意义.大地构造与成矿学, 33(3):465-480.
[7]  金成伟, 徐永生. 1997. 新疆托里别鲁阿嘎希地区花岗岩类的岩石学和成因. 岩石学报, 13(4): 529-537.
[8]  金成伟, 张秀棋. 1993. 新疆西准噶尔花岗岩类的时代及其成因. 地质科学, 28(1): 28-36.
[9]  晋慧娟, 李育慈. 1998. 准噶尔盆地西北缘石炭纪生物成因的沉积构造研究. 科学通报, 43(17): 1888-1891.
[10]  李华芹, 陈富文, 蔡红. 2000. 新疆西准噶尔地区不同类型金矿床Rb?Sr同位素年代研究. 地质学报, 74(2): 181-192.
[11]  李华芹, 谢才富, 常海亮. 1998. 新疆北部有色贵金属矿床成矿作用年代学. 北京: 地质出版社: 10-27.
[12]  沈远超, 金成伟. 1993. 西准噶尔地区岩浆活动与金矿化作用. 北京: 科学出版社: 113-171.
[13]  宋会侠, 刘玉琳, 屈文俊, 宋彪, 张锐, 成勇. 2007. 新疆包古图斑岩铜矿矿床地质特征. 岩石学报, 23(8): 1981-1988.
[14]  苏玉平, 唐红峰, 侯广顺, 刘丛强. 2006. 新疆西准噶尔达拉布特构造带铝质A型花岗岩的地球化学研究. 地球化学, 35(1): 55-67.
[15]  孙少华, 魏洲龄, 张琴华. 1990. 准噶尔盆地西北缘包古图组的沉积环境. 新疆石油地质. 11(1): 25-31.
[16]  唐功建, 王强, 赵振华, Wyman D A, 陈海红, 贾小辉, 姜子琦. 2009. 西准噶尔包古图成矿斑岩年代学与地球化学:岩石成因与构造、铜金成矿意义. 地球科学――中国地质大学学报, 34(1): 56-74.
[17]  唐红峰,苏玉平,刘丛强,侯广顺,王彦斌. 2007. 新疆北部卡拉麦里斜长花岗岩的锆石U?Pb年龄及其构造意义.大地构造与成矿学,31(1):110-117.
[18]  佟丽莉, 李永军, 张兵, 刘静, 庞振甲, 王军年. 2009. 新疆西准噶尔达尔布特断裂带南包古图组安山岩LA?ICP?MS锆石U?Pb测年及地质时代. 新疆地质, 27(3): 226-230.
[19]  伍建机, 陈斌. 2004. 西准噶尔庙尔沟后碰撞花岗岩微量元素和Nd?Sr同位素特征及成因. 新疆地质, 2(1): 29-36.
[20]  肖文交, 韩春明, 袁超, 陈汉林, 孙敏, 林寿发, 厉子龙, 毛启贵, 张继恩, 孙枢, 李继亮. 2006. 新疆北部石炭纪二叠纪独特的构造成矿作用对古亚洲洋构造域南部大地构造演化的制约. 岩石学报, 22(5): 1062-1076.
[21]  肖序常, 汤耀庆, 冯益民, 朱宝清, 李锦轶, 赵民. 1992. 新疆北部及其邻区大地构造. 北京: 地质出版社.
[22]  尹继元, 袁超, 孙敏, 肖文交, 赵国春, 龙晓平, 耿红燕, 王步云. 2009. 新疆西准噶尔地区赞岐岩(sanukite)的地球化学特征,成因机制及其与铜金矿化的关系. 地球化学, 38(5): 123-132.
[23]  张驰, 黄萱. 1992. 新疆西准噶尔蛇绿岩形成时代和环境探讨. 地质论评, 6: 509-524.
[24]  张立飞, 冼伟胜, 孙敏. 2004. 西准噶尔紫苏花岗岩成因岩石学研究. 新疆地质, 22(1): 36-42.
[25]  张连昌, 万博, 焦学军, 张锐. 2006. 西准包古图含铜斑岩的埃达克岩特征及其地质意义. 中国地质, 33(3): 626-631.
[26]  赵振华, 王强, 雄小林, 牛贺才, 张海祥, 乔玉楼. 2007. 新疆北部的富镁火成岩. 岩石学报, 23(7): 1696-1707.
[27]  周晶, 季建清, 韩宝福, 马芳, 龚俊峰, 徐芹芹, 郭召杰. 2008. 新疆北部基性岩脉40Ar/39Ar年代学研究. 岩石学报, 24(5): 997-1010.
[28]  朱宝清, 王来生, 王连晓. 1987. 西准噶尔西南地区古生代蛇绿岩. 中国地质科学院西安地质矿产研究所所刊, 17: 3-64.
[29]  Anma R, Armstrong R, Orihashi Y, Ike S I, Shin K C, Kon Y, Komiya T, Ota T, Kagashima S I, Shibuya T, Yamamoto S, Veloso E E, Fanning M and Hervé F. 2009. Are the Taitao granites formed due to subduction of the Chile ridge? Lithos, 113: 246-258.
[30]  Ballard J R, Palin J M and Campbell I H. 2002. Relative oxidation states of magmas inferred from Ce(IV)/Ce(III) in zircon: Application to porphyry copper deposits of northern Chile. Contributions to Mineralogy and Petrology Relative, 144: 347?364.
[31]  Bonin B. 2004. Do coeval mafic and felsic magmas in post?collisional to within?plate regimes necessarily imply two contrasting, mantle and crustal, sources? A review. Lithos, 78: 1-24.
[32]  Bornhorst T and Rose J W. 1986. Partitioning of gold in young calc?alkaline volcanic rocks from Guatemala. The Journal of Geology, 94: 412-418.
[33]  Boyle R. 1979. The geochemistry of gold and its deposits. Geoloigcal Survey of Canada Bulletin, 280: 584.
[34]  Buslov M M, Fujiwara Y, Iwata K and Semakov N N. 2004. Late Paleozoic?Early Mesozoic geodynamics of Central Asia. Gondwana Research, 7: 791-808.
[35]  Jian P, Liu D Y, Kr?ner A, Windley B F, Shi Y R, Zhang F Q, Shi G H, Miao L C, Zhang W, Zhang Q, Zhang L Q and Ren J S. 2008. Time scale of an early to mid?Paleozoic orogenic cycle of the long?lived Central Asian Orogenic Belt, Inner Mongolia of China: implications for continental growth. Lithos, 101: 233-259.
[36]  Kwon S T, Tilton G R, Coleman R G and Feng Y. 1989. Istopic studies bearing on the tectonics of the West Junggar region, Xinjiang, China. Tectonics, 8: 719-727.
[37]  Liang H Y, Sun W D, Su W C and Zartman R E. 2009. Porphyry copper?gold mineralization at Yulong, China, promoted by decreasing redox potential during magnetite alteration. Economic Geology, 104: 587-596.
[38]  Maruyama S. 1997. Pacific?type orogeny revisited: Miyashiro?type orogeny proposed. Island Arc, 6(1): 91-120.
[39]  Mungall J. 2002. Roasting the mantle: Slab melting and the genesis of major Au and Au?rich Cu deposits. Geology, 30: 915-918.
[40]  Paquette J L, Ménot R P, Pin C and Orsini J B. 2003. Episodic and short?lived granitic pulses in a post?collisional setting: Evidence from precise U?Pb zircon dating through a crustal cross?section in Corsica. Chemical Geology, 198: 1-20.
[41]  Pearce J A, Harris N B W and Tindle A G. 1984. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology, 25: 956-983.
[42]  Pearce J A. 1996. Sources and settings of granitic rocks. Episodes, 19: 120-125.
[43]  Seltmann R and Porter T M. 2005. The porphyry Cu?Au/Mo deposits of central Eurasia I: Tectonic, geologic and metallogenic setting, and significant deposits//Porter T M. Super Porphyry Copper and Gold Deposits: A global Perspective. PGC Publishing, Adelaide, 2: 467-512.
[44]  Seng?r A M C, Natalin B A and Burtman V S. 1993. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia. Nature, 364: 299?307.
[45]  Shen P, Shen Y C, Liu T B, Meng L, Dai H W and Yang Y H. 2009. Geochemical signature of porphyries in the Baogutu porphyry copper belt, western Junggar, NW China. Gondwana Research, 16: 227-242.
[46]  Sillitoe R. 1997. Characteristics and controls of the largest porphyry copper?gold and epithermal gold deposits in the circum?Pacific region. Australian Journal of Earth Sciences, 44: 373-388.
[47]  Sisson V B and Pavlis T L. 1993. Geologic consequences of plate reorganization?an example from the Eocene southern Alaska fore?arc. Geology, 21(10): 913-916.
[48]  Sisson V B, Pavlis T L, Roeske S M and Thorkelson D J. 2003. Introduction: An overview of ridge?trench interactions in modern and ancient settings//Sisson V B, Roeske S M and Pavlis T L. Geology of a transpressional orogen developed during ridge?trench interaction along the North Pacific margin: Boulder, Colorado. Geological Society of America Special Paper, 371: 1-18.
[49]  Suarez M and De La Cruz R. 2001. Jurassic to Miocene K?Ar dates from eastern central Patagonian Cordillera plutons, Chile (45°-48°S). Geological Magazine, 138(1): 53-66.
[50]  Sun M, Long X P, Cai K D, Jiang Y D,Wang B Y, Yuan C, Zhao G C, Xiao W J and Wu F Y. 2009. Early Paleozoic ridge subduction in the Chinese Altai: Insight from the abrupt change in zircon Hf isotopic compositions. Science in China, Series D, 39: 935-948.
[51]  Tatsumi Y, Shukuno H, Sato K, Shibata T and Yoshikawa M. 2003. The petrology and geochemistry of high?magnesium andesites at the western tip of the Setouchi volcanic belt, SW Japan. Journal of Petrology, 44: 1561-1578.
[52]  Tang G J, Wang Q, Wyman D A, Li Z X, Zhao Z H, Jia X H and Jiang Z Q. 2010. Ridge subduction and crustal growth in the Central Asian Orogenic Belt: Evidence from Late Carboniferous adakites and high?Mg diorites in the western Junggar region, northern Xinjiang (west China). Chemical Geology, doi: 10.1016/j.chemgeo.2010.08.012.
[53]  Thieblemont D, Stein G and Lescuyer J L. 1997. Gisements ’epithermaux et porphyriques: la connexion adakite. Comptes Rendus de l′Acad′emie des Sciences, Serie IIA. Earth and Planetary Science, 325(2): 103-109.
[54]  Tilton G R, Kwon S T and Coleman R G. 1986. Isotopic studies from the West Junggar Mts, NW China. Geol Soc Am Abstr Programs, 18: 773.
[55]  Turner S, Sandiford M and Foden J. 1992. Some geodynamic and compositional constraints on ′post?orogenic′magmatism. Lithos, 20: 931-934.
[56]  Xiao W J, Han C M, Yuan C, Sun M, Lin S F, Chen H L, Li Z L, Li J I and Sun S. 2008. Middle Cambrian to Permian subduction?related accretionary orogenesis of Northern Xinjiang, NW China: Implications for the tectonic evolution of central Asia. Journal of Asian Earth Sciences, 32: 102-117.
[57]  Yakubchuk A. 2004. Architecture and mineral deposit settings of the Altaid orogenic collage: A revised model. Journal of Asian Earth Science, 23: 761-779.
[58]  Zhao J M, Liu G D, Lu Z X, Zhang X K and Zhao G Z. 2003. Lithospheric structure and dynamic processes of the Tianshan orogenic belt and the Junggar basin. Tectonophysics, 376: 199?239.
[59]  Zhou T F, Yuan F, Fan Y, Zhang D Y, Cooke D and Zhao G C. 2008. Granites in the Sawuer region of the west Junggar, Xinjiang Province, China: Geochronological and geochemical characteristics and their geodynamic significance. Lithos, 106: 191-206.
[60]  安芳, 朱永峰. 2007. 新疆西准噶尔哈图金矿蚀变岩型矿体地质和地球化学研究. 矿床地质, 26(6): 621-633.
[61]  高山林, 何治亮, 周祖翼. 2006. 西准噶尔克拉玛依花岗岩体地球化学特征及其意义. 新疆地质, 24(2): 125-130.
[62]  辜平阳, 李永军, 张兵, 佟丽莉, 王军年. 2009. 西准达尔布特蛇绿岩中辉长岩LA?ICP?MS锆石U?Pb测年. 岩石学报, 25(6): 1364-1372.
[63]  韩宝福, 季建清, 宋彪, 陈立辉, 张磊. 2006. 新疆准噶尔晚古生代陆壳垂向生长(Ⅰ)-后碰撞深成岩浆活动的时限. 岩石学报, 22(5): 1077-1086.
[64]  韩宝福. 2007. 后碰撞花岗岩类的多样性及其构造环境判别的复杂性. 地学前缘, 14(3): 64-72.
[65]  何登发, 陈新发, 况军, 袁航, 吴晓智, 杜鹏, 唐勇. 2010. 准噶尔盆地石炭系油气成藏组合特征及勘探前景. 石油学报,31(1):1-11.
[66]  李菊英, 晋慧娟. 1989. 新疆准噶尔盆地西北缘石炭纪浊积岩系中遗迹化石的发现及其意义. 地质科学, 63: 9-15.
[67]  李建峰,夏斌,刘立文,徐力峰,何观生,王洪,张玉泉,杨之青. 2009. 西藏群让蛇绿岩辉长岩SHRIMP锆石U?Pb年龄及地质意义. 大地构造与成矿学, 33(2):294-298.
[68]  李辛子, 韩宝福, 季建清, 李宗怀, 刘志强, 杨斌. 2004. 新疆克拉玛依中基性岩墙群的地质地球化学和K?Ar年代学. 地球化学, 33(6): 574-584.
[69]  李印, 凌明星, 丁兴, 刘健, 韩峰, 孙卫东.2009.中国东部埃达克岩及成矿作用.大地构造与成矿学,33(3):448-464.
[70]  刘红涛, 张旗, 刘建明, 叶杰, 曾庆栋, 于昌明. 2004. 埃达克岩与Cu?Au成矿作用: 有待深入研究的岩浆成矿关系. 岩石学报, 20(2): 205-218.
[71]  刘希军, 许继峰, 王树庆, 侯青叶, 白正华, 雷敏. 2009. 新疆西准噶尔达拉布特蛇绿岩E?MORB型镁铁质岩的地球化学、年代学及其地质意义. 岩石学报, 25: 1373-1389.
[72]  刘玉琳, 郭丽爽, 宋会侠, 宋彪, 张锐, 许发军, 张云孝. 2009. 新疆西准噶尔包古图斑岩铜矿年代学研究. 中国科学(D辑), 39(10): 1466-1472.
[73]  齐进英, 熊义大. 1992. 新疆包古图金矿床特征及其成因. 矿床地质, 11(2): 154-164.
[74]  芮宗瑶, 张立生, 陈振宇, 王龙生, 刘玉琳, 王义天. 2004. 斑岩铜矿的源岩或源区探讨. 岩石学报, 20, 229-238.
[75]  沈晓明,张海祥,马林. 2010. 洋脊俯冲及其在新疆阿尔泰地区存在的可能证据.大地构造与成矿学,34(2):181-195.
[76]  宋春晖, 黄华芳. 1996. 西准噶尔白碱淮北部太勒古拉给深水沉积研究. 兰州大学学报(自然科学版), 32( 3): 132-137.
[77]  涂光炽. 1993. 新疆北部固体地球科学新进展. 北京: 科学出版社: 1-546.
[78]  王福同. 2006. 新疆维吾尔自治区古地理及地质生态图集. 北京: 中国地图出版社.
[79]  吴浩若, 潘正莆. 1991. “构造杂岩”及其地质意义――以西准噶尔为例. 地质科学, (1): 1-8.
[80]  王瑞, 朱永峰. 2007. 西准噶尔宝贝金矿地质与容矿火山岩的锆石SHRIMP年龄. 高校地质学报(董申葆院士九十诞辰纪念专辑), 13(3): 590-602.
[81]  王宗秀, 周高志, 李涛. 2003. 对新疆北部蛇绿岩及相关问题的思考和认识. 岩石学报, 19(4): 683-691.
[82]  熊小林, Adam J, Green T H, 牛贺才, 吴金花, 蔡志勇. 2005. 变质玄武岩部分熔体微量元素特征及埃达克岩熔体产生条件. 中国科学(D辑), 35(9): 837-846.
[83]  徐芹芹, 季建清, 韩宝福, 朱美妃, 储著银, 周晶. 2008. 新疆北部晚古生代以来中基性岩脉的年代学、岩石学、地球化学研究. 岩石学报,24(5): 977-996.
[84]  徐新, 何国琦, 李华芹, 丁天府, 刘兴义, 梅绍武. 2006. 克拉玛依蛇绿混杂岩带的基本特征和锆石SHRIMP年龄信息. 中国地质, 33(3): 470-475.
[85]  杨树德. 1994. 新疆北部的古板块构造. 新疆地质, l2(1): 1-8.
[86]  尹继元, 袁超, 孙敏, 龙晓平, 邱华宁, 王毓婧, 任江波, 关义立. 2011. 新疆哈图早二叠世富镁闪长岩的时代、地球化学特征和可能的成因机制. 岩石学报, 待刊.
[87]  张琴华, 孙少华, 秦清香. 1997. 新疆北部石炭纪岩相古地理、沉积建造及其含矿性. 长沙: 中南工业大学出版社: 1-164.
[88]  张旗, 秦克章, 王元龙, 张福勤, 刘红涛, 王焰. 2004. 加强埃达克岩研究, 开创中国Cu、Au等找矿工作的新局面. 岩石学报, 20(2): 195-204.
[89]  张旗, 王焰, 熊小林, 李承东. 2008. 埃达克岩和花岗岩: 挑战与机遇. 北京:中国大地出版社: 1-344.
[90]  赵振华, 王强, 熊小林, 张海祥, 牛贺才, 许继峰, 白正华, 乔玉楼. 2006. 新疆北部的两类埃达克岩. 岩石学报, 22(5): 1249-1265.
[91]  赵振华.2007.关于岩石微量元素构造环境判别图解使用的有关问题. 大地构造与成矿学, 31(1): 92-103.
[92]  赵振华, 熊小林, 王强, 白正华, 梅厚均. 2004. 新疆西天山莫斯早特石英钠长斑岩铜矿床――一个与埃达克质岩石有关的铜矿实例. 岩石学报,20(2): 249-258.
[93]  Cai K D, Sun M, Yuan C, Zhao G C, Xiao W J, Long X P and Wu F Y. 2010. Geochronological and geochemical study of mafic dykes from the northwest Chinese Altai: Implications for petrogenesis and tectonic evolution. Gondwana Research, doi:10.1016/j.gr.2010.02.010.
[94]  Chen B and Arakawa Y. 2005. Elemental and Nd?Sr isotopic geochemistry of granitoids from the West Junggar foldbelt (NW China), with implications for Phanerozoic continental growth. Geochimica et Cosmochimica Acta, 69: 1307-1320.
[95]  Chen B and Jahn B M. 2004. Genesis of post?collisional granitoids and basement nature of the Junggar terrane, NW China: Nd?Sr isotope and trace element evidence. Journal of Asian Earth Sciences, 23: 691-703.
[96]  Cooke D R, Hollings P and Walshe J L. 2005. Giant porphyry deposits: Characteristics, distribution and tectonic controls. Economic Geology, 100(5): 801-818.
[97]  Choulet F, Chen Y, Wang B, Faure M, Cluzel D, Charvet J, Lin W and Xu B. 2010. Late Paleozoic paleogeographic reconstruction of Western Central Asia based upon paleomagnetic data and its geodynamic implications. Journal of Asian Earth Sciences, doi:10.1016/j.jseaes.2010.07.011.
[98]  Eby G N. 1990. The A?type granitoids: A review of their occurence and chemical characteristics and speculations on their petrogenesis. Lithos, 26: 115-134.
[99]  Gao S, Rudnick R L, Yuan H L, Liu X M, Liu Y S, Xu W L, Ling W L, Ayers J, Wang X C and Wang Q H. 2004. Recycling lower continental crust in the North China craton. Nature, 432: 892-897.
[100]  Geng H Y, Sun M, Yuan C, Xiao W J, Zhao G C, Zhang L F, Wong K and Wu F Y. 2009. Geochemical, Sr?Nd and zircon U?Pb?Hf isotopic studies of Late Carboniferous magmatism in the West Junggar, Xinjiang: Implications for ridge subduction? Chemical Geology, 266: 364-389.
[101]  Guivel C, Lagabrielle Y, Bourgois J, Maury R C, Fourcade S, Martin H and Arnaud N. 1999. New geochemical constraints for the origin of ridge?subduction?related plutonic and volcanic suites from the Chile Triple Junction (Taitao Peninsula and Site 862, LEG ODP141 on the Taitao Ridge). Tectonophysics, 311: 83-111.
[102]  Haeussler P J, Bradley D, Goldfarb R, Snee L and Taylor C. 1995. Link between ridge subduction and gold mineralization in southern Alaska. Geology, 23(11): 995-998.
[103]  Han B F, Wang S G, Jahn B, Hong D W, Kagami H and Sun Y. 1997. Depleted?mantle source for the Ulungur River A?type granites from North Xinjiang, China: Geochemistry and Nd?Sr isotopic evidence, and implications for Phanerozoic crustal growth. Chemical Geology, 138: 135-159.
[104]  Hervé F, Fanning M C, Thomson S N, Pankhurst R J, Anma R, Veloso A and Herrera C. 2003. SHRIMP U?Pb and FT Pliocene agesof near?trench granitesin Taitao Peninsula, southern Chile // IV South American Symposium on Isotope Geology, Bahía, Brasil, Extended Abstracts, 2: 190-193.
[105]  Hollings P, Cooke D and Clark A. 2005. Regional geochemistry of tertiary igneous rocks in central Chile: Implications for the geodynamic environment of giant porphyry copper and epithermal gold mineralization. Economic Geology, 100(5): 887-904.
[106]  Hung C, Chung S, Cole R, Iizuka Y, Chiu H, Chu C and Gallet S. 2007. Zircon U?Pb ages for the McKinley Sequence and associated plutons, central Alaska Range. EOS, Transactions, American Geophysical Union, 88(52).
[107]  Isozaki Y. 1996. Anatomy and genesis of a subduction?related orogen: A new view of geotectonic subdivision and evolution of the Japanese Islands. Island Arc, 5(3): 289-320.
[108]  Jahn B M, Capdevila R, Liu D, Vernon A and Badarch G. 2004. Sources of Phanerozoic granitoids in the transect Bayanhongor?Ulaan Baatar, Mongolia: Geochemical and Nd isotopic evidence, and implications for Phanerozoic crustal growth. Journal of Asian Earth Sciences, 23: 629-653.
[109]  Jahn B M. 2004. The Central Asian orogenic belt and growth of the contitental crust in the Phanerozoic // Malpas, J, Fleteher, C J N, Ali J R and Aitehison J C. Aspects of the Tectonic Evolution of China. Special Publications, London, 226: 73-100.
[110]  Sajona F G and Maury R C. 1998. Association of adakites with gold and copper mineralization in the Philippines. Comptes Rendus de l′Academie des Sciences, Serie II. Sciences de la Terre et des Planetes, 326(1): 27-34.
[111]  Wang B, Chen Y, Zhan S, Shu L S, Faure M, Cluzel D, Charvet J and Laurent?Charvet S. 2007. Primary Carboniferous and Permian paleomagnetic results from the Yili Block (NW China) and their implications on the geodynamic evolution of Chinese Tianshan Belt. Earth and Planetary Science Letters, 263: 288?308.
[112]  Wang Q, Xu J F, Jian P, Bao Z W, Zhao Z H, Li C F, Xiong X L and Ma J L. 2005. Petrogenesis of adakitic porphyries in an extensional tectonic setting, Dexing, south China: Implications for the genesis of porphyry copper mineralization. Journal of Petrology, 47(1): 119-144.
[113]  Wang Q, Wyman D, Xu J, Zhao Z, Jian P, Xiong X, Bao Z, Li C and Bai Z. 2006a. Petrogenesis of Cretaceous adakitic and shoshonitic igneous rocks in the Luzong area, Anhui Province (eastern China): Implications for geodynamics and Cu?Au mineralization. Lithos, 89: 424-446.
[114]  Wang Q, Xu J, Jian P, Bao Z, Zhao Z, Li C, Xiong X and Ma J. 2006b. Petrogenesis of adakitic porphyries in an extensional tectonic setting, Dexing, South China: Implications for the genesis of porphyry copper mineralization. Journal of Petrology, 47: 119-144.
[115]  Windley B F, Alexeiev D, Xiao W J, Kr?ner A and Badarch G. 2007. Tectonic models for accretion of the Central Asian Orogenic Belt. Journal of the Geological Society, 164(1):31-47.
[116]  Windley F B, Kr?ner A, Guo J H, Qu G S, Li Y Y and Zhang C. 2002. Neoproterozoic to Paleozoic geology of the Altai orogen, NW China: New zircon age data and tectonic evolutionl. The Journal of Geology, 110: 719-737.
[117]  Wong K, Sun M, Zhao G C, Yuan C and Xiao W J. 2010. Geochemical and geochronological studies of the Alegedayi Ophiolitic Complex and its implication for the evolution of the Chinese Altai. Gondwana Research, doi:10.1016/j.gr.2010.01.010.
[118]  Xiao W J, Windley B F, Huang B C, Han C M, Yuan C, Chen H L, Sun M, Sun S and Li J L. 2009. End?Permian to mid?Triassic termination of the accretionary processes of the southern Altaids: Implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia. Int J Earth Sci (Geol Rundsch), 98: 1189-1217.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133