必须声明标量变量 "@Script_ID"。 新疆阿尔泰大喀拉苏花岗岩年代学、地球化学特征及其构造意义-《地球科学与环境学报》
|本期目录/Table of Contents|

[1]李强,杨富全*,杨成栋.新疆阿尔泰大喀拉苏花岗岩年代学、地球化学特征及其构造意义[J].地球科学与环境学报,2019,41(04):396-413.
 LI Qiang,YANG Fu-quan*,YANG Cheng-dong.Geochronology and Geochemical Characteristics of Dakalasu Granite in Altay of Xinjiang, China and Their Tectonic Significance[J].Journal of Earth Sciences and Environment,2019,41(04):396-413.
点击复制

新疆阿尔泰大喀拉苏花岗岩年代学、地球化学特征及其构造意义(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第41卷
期数:
2019年第04期
页码:
396-413
栏目:
基础地质与矿产地质
出版日期:
2019-07-15

文章信息/Info

Title:
Geochronology and Geochemical Characteristics of Dakalasu Granite in Altay of Xinjiang, China and Their Tectonic Significance
文章编号:
1672-6561(2019)04-0396-18
作者:
李强杨富全*杨成栋
(中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室,北京 100037)
Author(s):
LI Qiang YANG Fu-quan* YANG Cheng-dong
(MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China)
关键词:
花岗岩 地球化学 I-A过渡型 锆石U-Pb年龄 二叠纪 后碰撞 阿尔泰 新疆
Keywords:
Key words:granite geochemistry I-A transitional type zircon U-Pb age Permian post collision Altay Xinjiang
分类号:
P588.12+1; P597
DOI:
-
文献标志码:
A
摘要:
大喀拉苏似斑状黑云母二长花岗岩出露于新疆阿尔泰南缘,是研究阿尔泰二叠纪构造环境的理想对象。采用LA-Q-ICP-MS锆石U-Pb定年获得其加权平均年龄为(261.4±2.1)Ma,属中二叠世。岩石具有高Si(SiO2质量分数为69.03%~70.94%)、富Al(Al2O3为14.18%~14.71%)、富K(Na2O/K2O值为0.70~0.87)的特征,A/CNK值为1.02~1.04,属高钾钙碱性弱过铝质花岗岩,显示I-A过渡型特点。微量元素表现出Rb、Th、Pb、Nd、Sm的相对正异常; Ti、P、Sr和Ba的负异常; 稀土元素显示轻稀土元素强富集、重稀土元素平缓及明显的负Eu异常(0.55~0.82)。岩石的εNd(t)值和两阶段模式年龄分别为2.66~3.01和0.79~0.80 Ga。综合区域地质资料和岩体地球化学特征,认为大喀拉苏黑云母二长花岗岩形成于后造山伸展环境,岩浆来源于地幔和地壳物质的混合,并在岩浆源区经历了分离结晶作用。
Abstract:
Dakalasu porphyritic biotite monzogranite located in the southern Altay is an ideal object to study Permian regional tectonic environment. Zircons yield the weighted mean LA-Q-ICP-MS U-Pb age of(261.4±2.1)Ma for the biotite monzogranite, indicating that it is emplaced in Middle Permian. The rock is high in the contents of SiO2(69.03%-70.94%), Al2O3(14.18%-14.71%)and K(Na2O/K2O is 0.70-0.87)with A/CNK more than 1(1.02-1.04), which are defined as high-K calc-alkaline and weakly peraluminous granite characterized by I-A transitional type. Trace elements of the biotite monzogranites show relative positive anomalies for Rb, Th, Pb, Nd and Sm, and negative anomalies for Ti, P, Sr, Ba. REE shows strong enrichment of LREE, gentle HREE, and obvious negative Eu anomalies(0.55-0.82). The εNd(t)and two-stage model ages of the rock are 2.66-3.10 and 0.79-0.80 Ga, respectively. Combined with regional geological data and geochemistry characteristics presented here, it is suggested that Dakalasu biotite monzogranites form in post-orogenic extensional environment, and are derived from the mixture of crust and mantle materials. The magma experiences separation crystallization in the magma source.

参考文献/References:

[1] SENGOR A M C,NATAL’IN B A,BURTMAN V S.Evolution of the Altaid Tectonic Collage and Paleozoic Crustal Growth in Eurasia[J].Nature,1993,364:299-307.
[2] XIAO W J,WINDLEY B F,BADARCH G,et al.Palaeozoic Accretionary and Convergent Tectonics of the Southern Altaids:Implications for the Growth of Central Asia[J].Journal of the Geological Society,2004,161:339-342.
[3] 王京彬,秦克章,吴志亮,等.阿尔泰山南缘火山喷流沉积型铅锌矿床[M].北京:地质出版社,1998.
WANG Jing-bin,QIN Ke-zhang,WU Zhi-liang,et al.Volcanic Exhalative Sedimentary Lead-zinc Deposits in the South Margin of Altay Mountains,Xinjiang[M].Beijing:Geological Publishing House,1998.
[4] 王登红,陈毓川,徐志刚,等.阿尔泰成矿省的成矿系列及成矿规律[M].北京:原子能出版社,2002.
WANG Deng-hong,CHEN Yu-chuan,XU Zhi-gang,et al.Minerogenetic Series and Regularity of Minerali-zation in the Altai Metallogenetic Province,China[M].Beijing:Atomic Energy Press,2002.
[5] WINDLEY B F,KRONER A,GUO J H,et al.Neoproterozoic to Paleozoic Geology of the Altai Orogen,NW China:New Zircon Age Data and Tectonic Evolution[J].The Journal of Geology,2002,110(6):719-737.
[6] 何国琦,成守德,徐 新,等.中国新疆及邻区大地构造图(1:2 500 000)说明书[M].北京:地质出版社,2004.
HE Guo-qi,CHENG Shou-de,XU Xin,et al.An Introduction to the Explanatory Text of the Map of Tectonics in Xinjiang and Its Neighbouring Areas(1:2 500 000)[M].Beijing:Geological Publishing House,2004.
[7] WANG T,HONG D W,JAHN B M,et al.Timing,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,2006,114(6):735-751.
[8] 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.
TONG Ying,WANG Tao,HONG Da-wei,et al.Ages and Origin of the Early Devonian Granites from the North Part of Chinese Altai Mountains and Its Tectonic Implications[J].Acta Petrologica Sinica,2007,23(8):1933-1944.
[9] MAO J W,PIRAJNO F,ZHANG Z H,et al.A Review of the Cu-Ni Sulphide Deposits in the Chinese Tianshan and Altay Orogens(Xinjiang Autonomous Region,NW China):Principal Characteristics and Ore-forming Processes[J].Journal of Asian Earth Sciences,2008,32(2/3/4):184-203.
[10] XIAO W J,KRONER A,WINDLEY B F.Geodynamic Evolution of Central Asia in the Paleozoic and Meso-zoic[J].International Journal of Earth Sciences,2009,98(6):1185-1188.
[11] 邹天人,曹惠志,吴柏青.新疆阿尔泰造山花岗岩和非造山花岗岩及其判别标志[J].地质学报,1988,62(3):228-245.
ZOU Tian-ren,CAO Hui-zhi,WU Bai-qing.Orogenic and Anorogenic Granitoids in the Altay Mountains of Xinjiang and Their Discrimination Criteria[J].Acta Geologica Sinica,1988,62(3):228-245.
[12] HAN B F,WANG S G,JAHN B M.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[J].Chemical Geology,1997,138(3/4):135-159.
[13] BARBARIN B.A Review of the Relationships Between Granitoid Types,Their Origins and Their Geodynamic Environments[J].Lithos,1999,46(3):605-626.
[14] WANG T,JAHN B M,KOVACH V 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(1/2/3/4):359-372.
[15] 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.
WANG Tao,TONG Ying,LI Shan,et al.Spatial and Temporal Variations of Granitoids in the Altay Orogen and Their Implications for Tectonic Setting and Crustal Growth:Perspectives from Chinese Altay[J].Acta Petrologica et Mineralogica,2010,29(6):595-618.
[16] CAI K D,SUN M,YUAN C,et al.Prolonged Magmatism,Juvenile Nature and Tectonic Evolution of the Chinese Altai,NW China:Evidence from Zircon U-Pb and Hf Isotopic Study of Paleozoic Granitoids[J].Journal of Asian Earth Sciences,2011,42(5):949-968.
[17] LONG L L,GAO J,KLEMD R,et al.Geochemical and Geochronological Studies of Granitoid Rocks from the Western Tianshan Orogen:Implications for Continental Growth in the Southwestern Central Asian Orogenic Belt[J].Lithos,2011,126(3/4):321-340.
[18] 许继峰,陈繁荣,于学元,等.新疆北部阿尔泰地区库尔提蛇绿岩:古弧后盆地系统的产物[J].岩石矿物学杂志,2001,20(3):344-352.
XU Ji-feng,CHEN Fan-rong,YU Xue-yuan,et al.Ku’erti Ophiolite in Altay Area of North Xinjiang:Magmatism of an Ancient Back-arc Basin[J].Acta Petrologica et Mineralogica,2001,20(3):344-352.
[19] 苏慧敏,张东阳,艾 羽,等.阿尔泰南缘中泥盆世北塔山组火山岩中单斜辉石的矿物学研究及其地质意义[J].地质学报,2008,82(11):1602-1612.
SU Hui-min,ZHANG Dong-yang,AI Yu,et al.Mine-ralogy of Clinopyroxene from the Middle Devonian Volcanic Rocks in the South Margin of the Altay Mountains and Its Geological Significances[J].Acta Geologica Sinica,2008,82(11):1602-1612.
[20] CHAI F M,MAO J W,DONG L H,et al.Geochrono-logy of Metarhyolites from the Kangbutiebao Formation in the Kelang Basin,Altay Mountains,Xinjiang:Implications for the Tectonic Evolution and Metallogeny[J].Gondwana Research,2009,16(2):189-200.
[21] ZHANG Z C,ZHOU G,KUSKY T M,et al.Late Paleozoic Volcanic Record of the Eastern Junggar Terrane,Xinjiang,Northwestern China:Major and Trace Element Characteristics,Sr-Nd Isotopic Systematic and Implications for Tectonic Evolution[J].Gondwana Research,2009,16(2):201-215.
[22] 赵战锋,薛春纪,张立武,等.新疆青河玉勒肯哈腊苏铜矿区酸性岩锆石U-Pb法定年及其地质意义[J].矿床地质,2009,28(4):425-433.
ZHAO Zhan-feng,XUE Chun-ji,ZHANG Li-wu,et al.U-Pb Dating of Zircons from Acid Intrusions in Yulekenhalasu Copper Deposit of Qinghe,Xinjiang,and Its Geological Significance[J].Mineral Deposits,2009,28(4):425-433.
[23] YE X T,ZHANG C L,ZOU H B,et al.Devonian Alaskan-type Ultramafic-mafic Intrusions and Silicic Igneous Rocks Along the Southern Altai Orogeny:Implications on the Phanerozoic Continental Growth of the Altai Orogeny of the Central Asian Orogenic Belt[J].Journal of Asian Earth Sciences,2015,113:75-89.
[24] 李 强,柴凤梅,杨富全,等.新疆阿尔泰库卫铜镍硫化物-钒钛铁氧化物复合型矿化镁铁—超镁铁质杂岩体成因[J].岩石学报,2015,31(8):2211-2229.
LI Qiang,CHAI Feng-mei,YANG Fu-quan,et al.Petrogenesis of the Kuwei Ni-Cu Sulfide- and Fe-Ti Oxide-bearing Mafic-ultramafic Intrusions in the Altay Orogenic Belt,Xinjiang,NW China[J].Acta Pe-trologica Sinica,2015,31(8):2211-2229.
[25] 张海祥,牛贺才,SATO H,等.新疆北部晚古生代埃达克岩、富铌玄武岩组合:古亚洲洋板块南向俯冲的证据[J].高校地质学报,2004,10(1):106-113.
ZHANG Hai-xiang,NIU He-cai,SATO H,et al.Late Paleozoic Adakite and Nb-enriched Basalt from Northern Xinjiang:Evidence for the Southward Subduction of the Paleo-Asian Ocean[J].Geological Journal of China Universities,2004,10(1):106-113.
[26] 张招崇,闫升好,陈柏林,等.阿尔泰造山带南缘中泥盆世苦橄岩及其大地构造和岩石学意义[J].地球科学,2005,30(3):289-297.
ZHANG Zhao-chong,YAN Sheng-hao,CHEN Bo-lin,et al.Middle Devonian Picrites of South Margin of Altay Orogenic Belt and Implications for Tectonic Setting and Petrogenesis[J].Earth Science,2005,30(3):289-297.
[27] 张招崇,周 刚,闫升好,等.阿尔泰山南缘晚古生代火山岩的地质地球化学特征及其对构造演化的启示[J].地质学报,2007,81(3):344-358.
ZHANG Zhao-chong,ZHOU Gang,YAN Sheng-hao,et al.Geology and Geochemistry of the Late Paleozoic Volcanic Rocks of the South Margin of the Altai Mountains and Implications for Tectonic Evolution[J].Acta Geologica Sinica,2007,81(3):344-358.
[28] 耿新霞,柴凤梅,杨富全,等.新疆阿尔泰南缘达拉乌兹双峰式火山岩年龄及岩石成因[J].岩石学报,2010,26(10):2967-2980.
GENG Xin-xia,CHAI Feng-mei,YANG Fu-quan,et al.Geochronology and Genesis of the Bimodal Volcanic Rocks in Dalawuzi from the Southern Margin of Altay,Xinjiang[J].Acta Petrologica Sinica,2010,26(10):2967-2980.
[29] 李天德,波里扬斯基.中国和哈萨克斯坦阿尔泰大地构造及地壳演化[J].新疆地质,2001,19(1):27-32.
LI Tian-de,POLIYANGSIJI.Tectonics and Crustal Evolution of Altai in China and Kazakhstan[J].Xinjiang Geology,2001,19(1):27-32.
[30] XIAO W J,HAN C M,YUAN C,et al.Middle Cambrian to Permian Subduction-related Accretionary Orogenesis of Northern Xinjiang,NW China:Implications for the Tectonic Evolution of Central Asia[J].Journal of Asian Earth Sciences,2008,32(2/3/4):102-117.
[31] XIAO W J,WINDLEY B F,HUANG B C,et al.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[J].International Journal of Earth Sciences,2009,98(6):1189-1217.
[32] XIAO W J,SANTOSH M.The Western Central Asian Orogenic Belt:A Window to Accretionary Orogenesis and Continental Growth[J].Gondwana Research,2014,25(4):1429-1444.
[33] TONG Y,WANG T,JAHN B M,et al.Post-accretionary Permian Granitoids in the Chinese Altai Orogen:Geochronology,Petrogenesis and Tectonic Implications[J].American Journal of Science,2014,314(1):80-109.
[34] YUAN C,SUN M,XIAO W J,et al.Accretionary Orogenesis of the Chinese Altai:Insights from Paleozoic Granitoids[J].Chemical Geology,2007,242(1/2):22-39.
[35] WANG W,WEI C,ZHANG Y,et al.Age and Origin of Sillimanite Schist from the Chinese Altai Metamorphic Belt:Implications for Late Palaeozoic Tectonic Evolution of the Central Asian Orogenic Belt[J].International Geology Review,2014,56(2):224-236.
[36] 邹天人,李庆昌.中国新疆稀有及稀土金属矿床[M].北京:地质出版社,2006.
ZOU Tian-ren,LI Qing-chang.Rare and Rare Earth Mineral Deposits in Xinjiang,China[M].Beijing:Geological Publishing House,2006.
[37] 王建国.新疆阿尔泰哈拉苏钽铌铍矿床地质特征[J].新疆有色金属,2008(3):17-18,21.
WANG Jian-guo.Geological Characteristics of the Halasu Ta-Nb-Be Deposit in Altay,Xinjiang[J].Xinjiang Non-ferrous Metal,2008(3):17-18,21.
[38] YANG F Q,MAO J W,LIU F,et al.A Review of the Geological Characteristics and Mineralization History of Iron Deposits in the Altay Orogenic Belt of the Xinjiang,Northwest China[J].Ore Geology Reviews,2013,54:1-16.
[39] LIU Y S,GAO S,HU Z C,et al.Continental and Oceanic Crust Recycling-induced Melt-peridotite Interactions in the Trans-North China Orogen:U-Pb Dating,Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths[J].Journal of Petrology,2010,51(1/2):537-571.
[40] GB/T 14506.28—2010,硅酸盐岩石化学分析方法第28部分:16个主次成分量测定[S].
GB/T 14506.28—2010,Methods for Chemical Analysis of Silicate Rocks,Part 28:Determination of 16 Major and Minor Elements Content[S].
[41] GB/T 14506.2—2010,硅酸盐岩石化学分析方法第2部分:化合水量测定[S].
GB/T 14506.2—2010,Methods for Chemical Analysis of Silicate Rocks,Part 2:Determination of Combined Water Content[S].
[42] NY/T 86—1988,土壤碳酸盐测定法[S].
NY/T 86—1988,Method for Determination of Soil Carbonate[S].
[43] GB/T 14506.14—2010,硅酸盐岩石化学分析方法第14部分:氧化亚铁量测定[S].
GB/T 14506.14—2010,Methods for Chemical Analysis of Silicate Rocks,Part 14:Determination of Ferrous Oxide Content[S].
[44] LY/T 1253—1999,森林土壤矿质全量元素(硅、铁、铝、钛、锰、钙、镁、磷)烧失量的测定[S].
LY/T 1253—1999,Determination of Mineral Total Elements(Silica,Iron,Aluminium,Titanium,Manganese,Calcium,Magneslum,Phosphorus)Ignition Loss in Forest Soil[S].
[45] CLAESSON S,VETRIN V,BAYANOVA T,et al.U-Pb Zircon Age from a Devonian Carbonatite Dyke,Kola Peninsula,Russia:A Record of Geological Evolution from the Archaean to the Palaeozoic[J].Lithos,2000,51(1/2):95-108.
[46] BELOUSOVA E A,GRIFFIN W L,O’REILLY S Y,et al.Igneous Zircon:Trace Element Composition as an Indicator of Source Rock Type[J].Contributions to Mineralogy and Petrology,2002,143(5):602-622.
[47] RUBATTO D.Zircon Trace Element Geochemistry:Partitioning with Garnet and the Link Between U-Pb Ages and Metamorphism[J].Chemical Geology,2002,184(1/2):123-138.
[48] 李 彦,耿新霞,李 强,等.新疆阿尔泰阿勒泰组沉积时代及其形成环境[J].地质科学,2019,54(1):34-61.
LI Yan,GENG Xin-xia,LI Qiang,et al.Constraining the Deposition Time and Sedimentary Environments of the Altay Formation in Altay,Xinjiang[J].Chinese Journal of Geology,2019,54(1):34-61.
[49] 郭旭吉,李 彦,杨成栋.新疆阿尔泰凯勒克赛依铁矿地质特征、锆石LA-MC-ICP-MS U-Pb年龄及其意义[J].现代地质,2017,31(1):11-19.
GUO Xu-ji,LI Yan,YANG Cheng-dong.Kailekesaiyi Iron Deposit in Altay,Xinjiang,and Their Geological Implications[J].Geoscience,2017,31(1):11-19.
[50] RICKWOOD P C.Boundary Lines Within Petrologic Diagrams Which Use Oxides of Major and Minor Elements[J].Lithos,1989,22(4):247-263.
[51] MANIAR P D,PICCOLI P M.Tectonic Discrimination of Granitoids[J].Geological Society of American Bulletin,1989,101(5):635-643.
[52] SUN S S,MCDONOUGH W F.Chemical and Isoto-pic Systematics of Oceanic Basalt:Implication for Mantle Composition and Processes[J].Geological Society,London,Special Publications,1989,42:313-345.
[53] 新疆维吾尔自治区地质局区域地质测量大队第六分队.阿勒泰幅地质图[R].乌鲁木齐:新疆维吾尔自治区地质局,1974.
The Sixth Unit of the Regional Geological Survey Team,Xinjiang Geological Bureau.Altay Geological Map[R].Urumchi:Xinjiang Geological Bureau,1974.
[54] 新疆维吾尔自治区有色地质勘查局七〇六队.克兰盆地区域地质矿产图[R].乌鲁木齐:新疆维吾尔自治区有色地质勘查局,2003.
No.706 Geological Team,Xinjiang Nonferrous Geoexploration Bureau.Regional Geological and Mineral Map of Kelan Basin[R].Urumchi:Xinjiang Nonferrous Geoexploration Bureau,2003.
[55] 新疆维吾尔自治区有色地质矿产勘查研究院.新疆阿勒泰市契别特—沙尔布拉克地区矿产地质调查成果报告[R].乌鲁木齐:新疆维吾尔自治区有色地质矿产勘查研究院,2016.
Xinjiang Nonferrous Geological and Mineral Prospecting Research Institute.Report on Mineral Geology Exploration Results of Qibiete-Sha’erbulake Area in Altay,Xinjiang[R].Urumchi:Xinjiang Nonferrous Geological and Mineral Prospecting Research Institute,2016.
[56] 童 英.阿尔泰造山带晚古生代花岗岩年代学、成因及其地质意义[D].北京:中国地质科学院,2006.
TONG Ying.Geochronology,Origin of the Late Paleozoic Granitoids from the Altai Orogen in China and Their Geological Significance[D].Beijing:Chinese Academy of Geological Sciences,2006.
[57] 周汝洪.新疆同位素地质年代学研究的进展[J].新疆地质,1987(4):5-15.
ZHOU Ru-hong.The Advance on Isotope Geochronology of Xinjiang[J].Xinjiang Geology,1987(4):5-15.
[58] 仝来喜,陈义兵,徐义刚,等.阿尔泰超高温变泥质麻粒岩的锆石U-Pb年龄及其地质意义[J].岩石学报,2013,29(10):3435-3445.
TONG Lai-xi,CHEN Yi-bing,XU Yi-gang,et al.Zircon U-Pb Ages of the Ultrahigh-temperature Metapelitic Granulite from the Altai Orogen,NW China,and Geological Implications[J].Acta Petrologica Sinica,2013,29(10):3435-3445.
[59] 王 伟,魏春景,王 涛,等.中国阿尔泰造山带泥质麻粒岩的确定及地质意义[J].科学通报,2009,54(17):918-923.
WANG Wei,WEI Chun-jing,WANG Tao,et al.Confirmation of Pelitic Granulite in the Altai Orogen and Its Geological Significance[J].Chinese Science Bulletin,2009,54(7):918-923.
[60] 刘 锋,张 超,杨富全.新疆阿尔泰南缘加尔巴斯套铁矿床成矿时代及成矿作用研究[J].矿床地质,2012,31(6):1277-1288.
LIU Feng,ZHANG Chao,YANG Fu-quan.A Study of Chronology and Ore-forming Process of Jialbasto Iron Deposit on Southern Margin of Altay[J].Mineral Deposits,2012,31(6):1277-1288.
[61] 张国锋,李 永,杨富全,等.新疆阿尔泰巴斯铁列克钨多金属矿矿物特征及其地质意义[J].矿床地质,2019,38(1):101-119.
ZHANG Guo-feng,LI Yong,YANG Fu-quan,et al.Mineral Characteristics of Basitielieke W-polymetallic Deposit in Altay of Xinjiang and Their Geological Significance[J].Mineral Deposits,2019,38(1):101-119.
[62] 韩宝福,季建清,宋 彪,等.新疆喀拉通克和黄山东含铜镍矿镁铁—超镁铁杂岩体的SHRIMP锆石U-Pb年龄及其地质意义[J].科学通报,2004,49(22):2324-2328.
HAN Bao-fu,JI Jian-qing,SONG Biao,et al.SHRIMP Zircon U-Pb Ages of Kalatongke and Huangshandong Cu-Ni-bearing Mafic-ultramafic Complexes,Xinjiang,and Geological Implications[J].Chinese Science Bulletin,2004,49(22):2324-2328.
[63] 张 超,刘 锋,杨富全.新疆富蕴县库额尔齐斯铁矿成因机制探讨研究[J].岩矿测试,2013,32(1):157-165.
ZHANG Chao,LIU Feng,YANG Fu-quan.A Discussion on Genetic Mechanism of the Ku’erqis Iron Deposit in Fuyun County,Xinjiang[J].Rock and Mineral Analysis,2013,32(1):157-165.
[64] 韩宝福,季建清,宋 彪,等.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[J].岩石学报,2006,22(5):1077-1086.
HAN Bao-fu,JI Jian-qing,SONG Biao,et al.Late Paleozoic Vertical Growth of Continental Crust Around the Junggar Basin,Xinjiang China(Part I):Timing of Post-collisional Plutonism[J].Acta Petrologica Sinica,2006,22(5):1077-1086.
[65] 刘崴国,韩静波,薛晓峰,等.阿尔泰山南缘二叠纪地壳伸展减薄:侵入岩的证据[J].新疆地质,2011,29(3):270-274.
LIU Wei-guo,HAN Jing-bo,XUE Xiao-feng,et al.Permian Crustal Extensional Thinning in the South Margin of Altay Mountians:Evidence from Intrusive Rocks[J].Xinjiang Geology,2011,29(3):270-274.
[66] BRIGGS S M,YIN A,MANNING C E,et al.Late Paleozoic Tectonic History of the Ertix Fault in the Chinese Altai and Its Implications for the Development of the Central Asian Orogenic System[J].Geological Society of America Bulletin,2007,119(7/8):944-960.
[67] 周 刚,张招崇,王新昆,等.新疆玛因鄂博断裂带中花岗质糜棱岩锆石U-Pb SHRIMP和黑云母40Ar-39Ar年龄及意义[J].地质学报,2007,81(3):359-369.
ZHOU Gang,ZHANG Zhao-chong,WANG Xin-kun,et al.Zircon U-Pb SHRIMP and 40Ar-39Ar Dating of the Granitic Mylonite in the Mayin’ebo Fault Belt of North Xinjiang and Its Geological Significance[J].Acta Geologica Sinica,2007,81(3):359-369.
[68] 周 刚,张招崇,罗世宾,等.新疆阿尔泰山南缘玛因鄂博高温型强过铝花岗岩:年龄、地球化学特征及其地质意义[J].岩石学报,2007,23(8):1909-1920.
ZHOU Gang,ZHANG Zhao-chong,LUO Shi-bin,et al.Confirmation of High Temperature Strongly Peraluminous Mayin’ebo Granites in the South Margin of Altay,Xinjiang:Age,Geochemistry and Tecto-nic Implications[J].Acta Petrologica Sinica,2007,23(8):1909-1920.
[69] 陈立辉,韩宝福.新疆北部乌恰沟地区镁铁质侵入岩的年代学、地球化学和Sr-Nd-Pb同位素组成:对地幔源区特征和深部过程的约束[J].岩石学报,2006,22(5):1201-1214.
CHEN Li-hui,HAN Bao-fu.Geochronology,Geochemistry and Sr-Nd-Pb Isotopic Composition of Mafic Intrusive Rocks in Wuqiagou Area,North Xinjiang:Constraints for Mantle Sources and Deep Processes[J].Acta Petrologica Sinica,2006,22(5):1201-1214.
[70] 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.
TONG Ying,WANG Tao,HONG Da-wei,et al.Spatial and Temporal Distribution of the Carboniferous-Permian Granitoids in Northern Xinjiang and Its Adjacent Areas,and Its Tectonic Significance[J].Acta Petrologica et Mineralogica,2010,29(6):619-641.
[71] 孙桂华,李锦轶,杨天南,等.阿尔泰山脉南部线性花岗岩锆石SHRIMP U-Pb定年及其地质意义[J].中国地质,2009,36(5):976-987.
SUN Gui-hua,LI Jin-yi,YANG Tian-nan,et al.Zircon SHRIMP U-Pb Dating of Two Linear Granite Plutons in Southern Altay Mountains and Its Tectonic Implications[J].Geology in China,2009,36(5):976-987.
[72] 高福平,周 刚,雷永孝,等.新疆阿尔泰山南缘沙尔布拉克一带早二叠世花岗岩的年龄、地球化学特征及地质意义[J].地质通报,2010,29(9):1281-1293.
GAO Fu-ping,ZHOU Gang,LEI Yong-xiao,et al.Early Permian Granite Age and Geochemical Characteristics in Shaerbulake of Xinjiang’s Altay Area and Its Geological Significance[J].Geological Bulletin of China,2010,29(9):1281-1293.
[73] 赵玉梅,彭 戈,赵得龙,等.中国阿尔泰克孜勒花岗岩体LA-ICP-MS锆石U-Pb定年、岩石地球化学特征及其地质意义[J].地质与勘探,2016,52(2):271-282.
ZHAO Yu-mei,PENG Ge,ZHAO De-long,et al.LA-ICP-MS Zircon U-Pb Age and Geochemistry of the Kezile Granitic Pluton in Altay of China and Their Geological Implications[J].Geology and Exploration,2016,52(2):271-282.
[74] MILLER C F,BRADFISH L J.An Inner Cordilleran Belt of Muscovite-bearing Plutons[J].Geology,1980,8(9):412-416.
[75] WOLF M B,LONDON D.Apatite Dissolution into Peraluminous Haplogranitic Melts:An Experimental Study of Solubilities and Mechanisms[J].Geochimica et Cosmochimica Acta,1994,58(19):4127-4145.
[76] CHAPPEDLL B W.Aluminium Saturation in I- and S-type Granites and the Characterization of Fractionated Haplogranites[J].Lithos,1999,46(3):535-551.
[77] WU F Y,JAHN B M,WILDER S A,et al.Highly Fractionated I-type Granites in NE China(I):Geochronology and Petrogenesis[J].Lithos,2003,66(3/4):241-273.
[78] WHALEN J B,CURRIE K L,CHAPPELL B W.A-type Granites:Geochemical Characteristics,Discrimination and Petrogenesis[J].Contributions to Minera-logy and Petrology,1987,95(4):407-419.
[79] 路凤香,桑隆康.岩石学[M].北京:地质出版社,2002.
LU Feng-xiang,SANG Long-kang.Petrology[M].Beijing:Geological Publishing House,2002.
[80] 吴福元,刘小驰,纪伟强,等.高分异花岗岩的识别与研究[J].中国科学:地球科学,2017,47(7):745-765.
WU Fu-yuan,LIU Xiao-chi,JI Wei-qiang,et al.Highly Fractionated Granites:Recognition and Research[J].Science China:Earth Sciences,2017,47(7):745-765.
[81] CHAPPELL B W,WHITE A J R.I- and S-type Granites in the Lachlan Fold Belt[J].Earth and Environmental Science Transactions of the Royal Society of Edinburgh,1992,83(1/2):1-26.
[82] JAHN B M,WU F Y,CAPDEVILA R,et al.Highly Evolved Juvenile Granites with Tetrad REE Patterns:The Woduhe and Baerzhe Granites from the Great Xing’an Mountains in NE China[J].Lithos,2001,59(4):171-198.
[83] MCDONOUGH W F,SUN S S.The Composition of the Earth[J].Chemical Geology,1995,120(3/4):223-253.
[84] TAYLOR S R,MCLENANN S M.The Continental Crust:Its Composition and Evolution[M].Oxford:Blackwell,1985.
[85] DEPAOLO D J,DALEY E E.Neodymium Isotopes in Basalts of the Southwest Basin and Range and Lithospheric Thinning During Continental Extension[J].Chemical Geology,2000,169(1/2):157-185.
[86] WEBSTER J,THOMAS R,FORSTER H J,et al.Geochemical Evolution of the Halogen-enriched Granite Magmas and Mineralizing Fluids of the Zinnwald Tin-tungsten Minning District,Erzgebirge,Germany[J].Mineralium Deposita,2004,39(4):452-472.
[87] BAO B,WESTER J D,ZHANG D H,et al.Compositions of Biotite,Amphibole,Apatite and Silicate Melt Inclusions from the Tongchang Mine,Dexing Porphyry Deposit,SE China:Implications for the Behavior of Halogens in Mineralized Porphyry Systems[J].Ore Geology Reviews,2016,79:443-462.
[88] ZARASKY G P,KORZHINSKAYA V,KOTOVA N.Experimental Studies of Ta2O5 and Columbite-tantalite Solubility in Fluoride Solutions from 300 ℃ to 550 ℃ and 50 to 100 MPa[J].Mineralogy and Petrology,2010,99(3/4):287-300.
[89] BALLOUARD C,POUJOL M,BOULVAIS P,et al.Nb-Ta Fractionation in Peraluminous Granites:A Marker of the Magmatic-hydrothermal Transition[J].Geology,2016,44(7):231-234.
[90] LINNEN R L,KEPPLER H.Columbite Solubility in Granitic Melts:Consequences for the Enrichment and Fractionation of Nb and Ta in the Earth’s Crust[J].Contributions to Mineralogy and Petrology,1997,128(2/3):213-227.
[91] 陈璟元,杨进辉.佛冈高分异I型花岗岩的成因:来自Nb-Ta-Zr-Hf等元素的制约[J].岩石学报,2015,31(3):846-854.
CHEN Jing-yuan,YANG Jin-hui.Petrogenesis of the Fogang Highly Fractionated I-type Granitoids:Constraints from Nb,Ta,Zr and Hf[J].Acta Petrologica Sinica,31(3):846-854.
[92] STEPANOV A,MAVROGENES J A,MEFFRE S,et al.The Key Role of Mica During Igneous Contcentration of Tantalum[J].Contributions to Mineralogy and Petrology,2014,167(6):1009.
[93] PATINO DOUCE A E.Experimental Generation of Hybrid Silicic Melts by Reaction of High Al Basalt with Metamorphic Rocks[J].Journal of Geophysical Research,1995,100:623-639.
[94] PATINO DOUCE A E.What Do Experiments Tell Us About the Relative Contributions of Crust and Mantle to the Origin of Granitic Magmas?[J].Geological Society,London,Special Publications,1999,168:55-75.
[95] 柴凤梅,董连慧,杨富全,等.阿尔泰南缘克朗盆地铁木尔特花岗岩体年龄、地球化学特征及成因[J].岩石学报,2010,26(2):377-386.
CHAI Feng-mei,DONG Lian-hui,YANG Fu-quan,et al.Age,Geochemistry and Petrogenesis of Tiemu’erte Granites in the Kelang Basin at the Southern Mu’argin of Altay,Xinjiang[J].Acta Petrologica Sinica,2010,26(2):377-386.
[96] 陈汉林,杨树锋,厉子龙,等.阿尔泰造山带富蕴基性麻粒岩锆石SHRIMP U-Pb年代学及其构造意义[J].岩石学报,2006,22(5):1351-1358.
CHEN Han-lin,YANG Shu-feng,LI Zi-long,et al.Zircon SHRIMP U-Pb Chronology of Fuyun Basic Granulite and Its Tectonic Significance in Altai Orogenic Belt[J].Acta Petrologica Sinica,2006,22(5):1351-1358.
[97] 张忠利,杨成栋,张 斌,等.新疆阿尔泰克兰盆地泥盆纪花岗岩年代学特征及其地质意义[J].地球科学与环境学报,2019,41(4):414-430.
ZHANG Zhong-li,YANG Cheng-dong,ZHANG Bin,et al.Geochronological Characteristics of Devonian Granitoids in Kelan Basin of Altay,Xinjiang,China and Their Geological Implications[J].Journal of Earth Sciences and Environment,2019,41(4):414-430.
[98] 胡霭琴,韦刚健,邓文峰,等.阿尔泰地区清河县西南片麻岩中锆石SHRIMP U-Pb定年及其地质意义[J].岩石学报,2006,22(1):1-10.
HU Ai-qin,WEI Gang-jian,DENG Wen-feng,et al.SHRIMP Zircon U-Pb Dating and Its Significance for Gneisses from the Southwest Area to Qinghe County in the Altai,China[J].Acta Petrologica Sinica,2006,22(1):1-10.
[99] 韩宝福.后碰撞花岗岩类的多样性及其构造环境判别的复杂性[J].地学前缘,2007,14(3):64-72.
HAN Bao-fu.Diverse Post-collisional Granitoids and Their Tectonic Setting Discrimination[J].Earth Science Frontiers,2007,14(3):64-72.
[100] PEARCE J A,HARRIS N B L,TINDLE A G.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks[J].Journal of Petroloogy,1984,25(4):956-983.

相似文献/References:

[1]赵磊,漆富勇,李江东.江西赣县洋西坑钼矿床地质特征及Re-Os同位素测年[J].地球科学与环境学报,2013,35(04):77.
 ZHAO Lei,QI Fu-yong,LI Jiang-dong.Geological Characteristics and Re-Os Isotopic Dating of Yangxikeng Molybdenum Deposit in Ganxian of Jiangxi[J].Journal of Earth Sciences and Environment,2013,35(04):77.
[2]毕君辉,葛文春,张彦龙,等.佳木斯地块东部二叠纪锦山花岗杂岩体的成因及其地质意义[J].地球科学与环境学报,2014,36(04):16.
 BI Jun-hui,GE Wen-chun,ZHANG Yan-long,et al.Petrogenesis of Permian Jinshan Granitic Complex in the Eastern Jiamusi Massif and Its Geological Implication[J].Journal of Earth Sciences and Environment,2014,36(04):16.
[3]周争艳,杨家喜,徐涛,等.西秦岭天水地区早中生代草川铺花岗岩年代学、地球化学特征及其地质意义[J].地球科学与环境学报,2015,37(02):11.
 ZHOU Zheng-yan,YANG Jia-xi,XU Tao,et al.Geochronological and Geochemical Characteristics of Early Mesozoic Caochuanpu Granitoids in Tianshui Area of West Qinling and Their Geological Significance[J].Journal of Earth Sciences and Environment,2015,37(04):11.
[4]赖绍聪,赵少伟.川西北塔公石英闪长岩地球化学特征和岩石成因[J].地球科学与环境学报,2015,37(03):1.
 LAI Shao-cong,ZHAO Shao-wei.Geochemistry and Petrogenesis of Quartz Diorite in Tagong Area of Northwest Sichuan[J].Journal of Earth Sciences and Environment,2015,37(04):1.
[5]翟明国.大陆动力学的物质演化研究方向与思路[J].地球科学与环境学报,2015,37(04):1.
 ZHAI Ming-guo.New Research Interests and Concept of Material Evolution for Continental Dynamics[J].Journal of Earth Sciences and Environment,2015,37(04):1.
[6]高景刚,梁婷,李文渊,等.新疆额尔齐斯韧性剪切带新生锆石及其年代学意义[J].地球科学与环境学报,2015,37(04):15.
 GAO Jing-gang,LIANG Ting,LI Wen-yuan,et al.Neogenic Zircons in Ertix Ductile Shear Zone of Xinjiang and Their Geochronological Significance[J].Journal of Earth Sciences and Environment,2015,37(04):15.
[7]王超,陈斌,马星华,等.东天山三岔口地区早、晚古生代岩体成因及其对康古尔缝合带演化的意义[J].地球科学与环境学报,2015,37(05):52.
 WANG Chao,CHEN Bin,MA Xing-hua,et al.Petrogenesis of Early and Late Paleozoic Plutons in Sanchakou Area of East Tianshan and Their Implications for Evolution of Kangur Suture Zone[J].Journal of Earth Sciences and Environment,2015,37(04):52.
[8]冯罡,万乐,刘正宏,等.内蒙古巴林右旗晚侏罗世巴彦琥硕花岗岩地球化学特征、锆石U-Pb年龄及Hf同位素组成[J].地球科学与环境学报,2015,37(06):33.
 FENG Gang,WAN Le,LIU Zheng-hong,et al.Geochemical Characteristics, Zircon U-Pb Age and Hf Isotopic Composition of Late Jurassic Bayanhushuo Granites in Balinyou Banner of Inner Mongolia[J].Journal of Earth Sciences and Environment,2015,37(04):33.
[9]叶永钦,叶松鑫,许幼,等.粤北长江铀矿田长排地区花岗岩体地球化学特征及其意义[J].地球科学与环境学报,2015,37(06):101.
 YE Yong-qin,YE Song-xin,XU You,et al.Geochemical Characteristics of Granite Body in Changpai Area of Changjiang Uranium Orefield, the Northern Guangdong and Their Significance[J].Journal of Earth Sciences and Environment,2015,37(04):101.
[10]孙兰兰,杨家喜,周争艳,等.适用于壳幔混合物源成因花岗岩中暗色微粒包体的单斜辉石压力计[J].地球科学与环境学报,2016,38(01):34.
 SUN Lan-lan,YANG Jia-xi,ZHOU Zheng-yan,et al.Clinopyroxene Geobarometer Applied to Mafic Microgranular Enclaves in Granite Originated from Crust-mantle Mixed Source[J].Journal of Earth Sciences and Environment,2016,38(04):34.

备注/Memo

备注/Memo:
收稿日期:2019-03-24; 修回日期:2019-06-01投稿网址:http://jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41702100); 中国地质科学院基本科研业务费专项资金项目(K1701); 新疆维吾尔自治区阿勒泰地区资源补偿奖励资金项目
作者简介:李强(1987-),男,河北唐山人,助理研究员,理学博士,E-mail:liqiangcags@163.com。
*通讯作者:杨富全(1968-),男,河北张家口人,研究员,博士研究生导师,理学博士,E-mail:fuquanyang@163.com。
更新日期/Last Update: 2019-07-11