中国及亚洲重要造山带花岗岩浆时空演化及成矿背景对比研究

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Abstract Based on extensive collection of granitoid chronology data and information, a large number of fieldworks had been done in the key areas of the main orogenic belts in Asia, including foreign countries, such as Russia, Mongolia, Kyrgyzstan, South Korea, Japan, and Vietnam. Many high precision zircon U-Pb ages and geochemistry data had been got with a lot of careful analyses in laboratories, and some important magmatic events had been found. Combined with the high quality published data, the geochronological frameworks of granitoids from some key areas were built, and a preliminary summary of the temporal and spatial distribution and tectonic magmatic evolution of the granitoids from the Central Asian Orogenic Belt, Central Orogenic Belt (Qilian-Qinling). Tethys and West Pacific tectonic domain were obtained, providing relevant tectonic background for the mineral resources exploration. Based on above researches, a draft map of Asian granitoids with database has been made, and the tectonic evolution of Asian granitoids has also been published. It provides the basis for discussing the Asian tectonic evolution, especially for the process of continental convergence. This is the first approach to systematical discussion of the Asian granitoid magmatic evolution by Chinese researchers.

Key words： granitoid chronology magmatic evolution metallogenesis orogenic belt Asia

Received: 15 October 2014

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	WANG Tao
	TONG Ying
	WU Cai-lai
	WANG Xiao-xia
	XIE Cai-fu
	ZHANG Hong-rui
	MAO Jian-ren
	ZHANG Lei
	HAN Bao-fu
	GUO Lei
	HONG Da-wei
	WANG Yan-bin
	ZHANG Jian-jun
	LI Shan

Cite this article:

WANG Tao,TONG Ying,WU Cai-lai, et al. Temporal and Spatial Evolution of the Granitoids from the Main Orogenic Belts in Asia and Their Implication for Tectonism and Metallogenesis[J]. , 2014, 1(2): 58-64.

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http://114.242.223.217/EN/ OR http://114.242.223.217/EN/Y2014/V1/I2/58

[1] 王涛,王晓霞,田伟,等.北秦岭古生代花岗岩组合、岩浆时空演变及其对造山作用的启示[J]. 中国科学(D 辑: 地球科学) ,2009, 39(7) : 949-971.
[2] 王涛,童英,李舢,等. 阿尔泰造山带花岗岩时空演变、构造环境及地壳生长意义——以中国阿尔泰为例[J]. 岩石矿物学杂志,2010, 29(6) : 595-618.
[3] Wang Tao, Hong Da-wei, Jahn Bor-ming , et al. Petrogenesis, and setting of Paleozoic synorogenic intrusions from the Altai Mountains, Northwest China: Implications for the tectonic evolution of an Accretionary Orogen[J]. The Journal of Geology,2114:735-751.
[4] Wang Tao, Wang Xiao Xia, Tian Wei, et al. North Qinling Paleozoic granite associations and their variation in space and time: Implications for orogenic processes in the orogens of central China[J]. Sci China Ser D-Earth Sci, 2009, 52(9): 1359-1384.
[5] Wang Xiaoxia, Wang Tao, Bor-ming Jahn, et al. Tectonic significance of Triassic lamprophyres from north Qinling orogen[J]. Geological Magazine, 2007,144 (4) : 837-848.
[6] Wang X X , Wang T,Zhang C L. Neoproterozoic, Paleozoic, and Mesozoic granitoid magmatism in the Qinling Orogen, China: Constraints on orogenic process[J]. Journal of Asian Earth Sciences,2013,72:129-151.
[7] Wu Cailai , Yang Jingsui, Robinson Paul T, et al. Geochemistry, age and tectonic significance of granitic rocks in north Altun,northwest China[J]. Lithos, 2009,113(3/4): 423-436.
[8] Wu Cailai, Joseph L Wooden, Paul T Robinson, et al. Geochemistry and zircon SHRIMP U-Pb dating of granitoids from the west segment of the North Qaidam[J]. Sci China Ser D-Earth Sci, 2009, 52(11): 1771-1790.
[9] Wu Cailai, GaoYuanhong, B Ronald Frost, et al. An early Palaeozoic double-subduction model for the North Qilian oceanic plate: evidence from zircon SHRIMP dating of granites[J]. International Geology Review, 2011, 53 (2) : 157-181.
[10]童英,王涛,洪大卫,等.北疆及邻区石炭—二叠纪花岗岩时空分布特征及其构造意义[J].岩石矿物学杂志,2010, 29(6):619-641.
[11]童英,洪大卫,王涛,等.中蒙边境中段花岗岩时空分布特征及构造和找矿意义[J].地球学报,2010, 31(3):395-412.
[12]Tong Ying, Wang Tao, Jahn Bor-ming, et al. Post-accretionary Permian granitoids in the Chinese Altai orogen: geochronology, petrogenesis and tectonic implications[J]. American Journal of Science, 2014, 314:80-109.
[13]Li Shan, Wang Tao, Wilde S A, et al. Evolution, source and tectonic significance of Early Mesozoic granitoid magmatism in the Central Asian Orogenic Belt (central segment) [J]. Earth-Science Reviews, 2013, 126(10):206-234.
[14]韩宝福,郭召杰,何国琦. “钉合岩体”与新疆北部主要缝合带的形成时限[J]. 岩石学报,2010, 26(8) :2233-2246.
[15]李舢,王涛,童英.中亚造山系中南段早中生代花岗岩时空分布特征及构造环境[J]. 岩石矿物学杂志,2010,29(6) :642-662.
[16]吴才来,郜源红,吴锁平,等.柴北缘大柴旦地区古生代花岗岩锆石 SHRIMP 定年[J].岩石学报, 2007, 23(8): 1861 -1875.
[17]吴才来,郜源红,吴锁平,等.柴北缘西段花岗岩锆石 SHRIMP U-Pb定年及其岩石地球化学特征[J].中国科学(D 辑:地球科学),2008, 38(8) :1-22.
[18]吴才来,徐学义,高前明,等.北祁连早古生代花岗质岩浆作用及构造演化[J]. 岩石学报,2010,26(4) : 1027-1044.
[19]李舢,王涛,洪大卫.中亚造山系中南段早中生代花岗岩类时空分布特征及构造环境[J]. 岩石矿物学杂志,2010,29(6):642-662.
[20]王晓霞,王涛,齐秋菊,等.秦岭晚中生代花岗岩时空分布、成因演变及构造意义[J]. 岩石学报,2011,27(6) : 1573-1593.
[21]Wang Tao, Jahn Bor-Ming, Kovach Victor P, et al. Nd-Sr isotopic mapping of the Chinese Altai and implications for continental growth in the Central Asian Orogenic Belt[J]. Lithos, 2009, 110:359-372.
[22]韩宝福 .中俄阿尔泰山中生代花岗岩与稀有金属矿床的初步对比分析[J]. 岩石学报, 2008, 24(4) :655-660.
[23]Wang Tao, Guo Lei, ZhengYadong, et al. Timing and processes of late Mesozoic mid-lower-crustal extension in continental NE Asia and implications for the tectonic setting of the destruction of the North China Craton: Mainly constrained by zircon U-Pb ages from metamorphic core complexes[J]. Lithos, 2012, 154:315-345.
[24]童英,王涛,洪大卫,等.中国阿尔泰北部山区早泥盆世花岗岩的年龄、成因及构造意义[J].岩石学报,2007, 23(8) :1933-1944.
[25]Tong Ying,Wang Tao,Siebel Wolfgang,et al. Recognition of early Carboniferous alkaline granite in the southern Altai orogen: post-orogenic processes constrained by U-Pb zircon ages,Nd isotopes,and geochemical data [J]. International Journal of Earth Sciences, 2012,101(4):937-950.
[26]Chen Bin, Jahn B M, Tian Wei. Evolution of the Solonker suture zone: Constraints from zircon U-Pb ages,Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subductionand collision-related magmas and forearc sediments[J].Journal of Asian Earth Sciences, 2009, 34:245-257.
[27]Wang Tao, Jahn Borming, Kovach P Victor, et al. Ekaterina. Mesozoic anorogenic granitic magmatism in the Altai Paleozoic accretionary orogen, NW China, and its implications for crustal architecture and growth[J]. American Journal of Science, 2014, 314:1-42.
[28]陈家富,韩宝福,张磊.西准噶尔北部晚古生代两期侵入岩的地球化学、Sr-Nd同位素特征及其地质意义[J].岩石学报,2010, 26(8) :2317-2335.
[29]韩宝福,张臣,赵磊,等.内蒙古西部呼伦陶勒盖地区花岗岩类的初步研究[J]. 岩石矿物学杂志,2010,29(6) :741-749.
[30]Li Shan, Wang Tao, Wilde S A,et al.Geochronology, petrogenesis and tectonic implications of Triassic granitoids from Beishan, NW China[J].Lithos, 2012,123-145.
[31]王涛, 张磊,郭磊, 等. 亚洲中生代花岗岩图初步编制及若干研究进展[J].地球学报,2014,35(6): 1-18.
[32]毛建仁.中国东南部及邻区中新生代岩浆作用与成矿[M].北京:科学出版社,2013.
[33]Wang Tao, Zheng Yadong, Zhang Jinjiang, et al.Pattern and kinematic polarity of late Mesozoic extension in continental NE Asia:Perspectives from metamorphic core complexes[J].Tectonics, 2011, 30 (6):1-27.
[34]Wang Tao, Guo Lei,Zhang Lei, et al.Timing and evolution of late Mesozoic granitoid magmatisms in the Mongol-Okhotsk belt and its adjacent areas, NE Asia: implications for transition from contractional thickened to extensional thinning crust and geodynamic settings[J]. Journal of Asian Earth Sciences, 2015 (accepted).