必须声明标量变量 "@Script_ID"。 北秦岭晚三叠世关山岩体地球化学特征及成因机制-《地球科学与环境学报》
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[1]杨航,赖绍聪*,张志华,等.北秦岭晚三叠世关山岩体地球化学特征及成因机制[J].地球科学与环境学报,2019,41(02):170-184.
 YANG Hang,LAI Shao-cong*,ZHANG Zhi-hua,et al.Geochemical Characteristics and Forming Mechanism of Late Triassic Guanshan Pluton in North Qinling, China[J].Journal of Earth Sciences and Environment,2019,41(02):170-184.
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《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02期
页码:
170-184
栏目:
基础地质与矿产地质
出版日期:
2019-03-15

文章信息/Info

Title:
Geochemical Characteristics and Forming Mechanism of Late Triassic Guanshan Pluton in North Qinling, China
文章编号:
1672-6561(2019)02-0170-15
作者:
杨航12赖绍聪12*张志华12秦江锋12
(1.西北大学 大陆动力学国家重点实验室,陕西 西安 710069; 2.西北大学 地质学系,陕西 西安 710069)
Author(s):
YANG Hang12 LAI Shao-cong12* ZHANG Zhi-hua12 QIN Jiang-feng12
(1. State Key Laboratory of Continental Dynamics, Northwest University, Xi’an 710069, Shaanxi, China; 2. Department of Geology, Northwest University, Xi’an 710069, Shaanxi, China)
关键词:
地球化学 锆石U-Pb年龄 Lu-Hf同位素 埃达克岩 花岗岩 同碰撞岩浆作用 北秦岭
Keywords:
geochemistry zircon U-Pb age Lu-Hf isotope adakite granite syn-collisional magmatism North Qinling
分类号:
P597
DOI:
-
文献标志码:
A
摘要:
关山地区位于北秦岭与北祁连造山带的结合部位,目前有关关山岩体的岩石成因存在争议。锆石U-Pb定年结果表明关山岩体二长花岗岩的加权平均年龄为(236.3±4.0)Ma(样本数为6个,平均标准权重偏差为2.6)。地球化学特征显示岩石具有高Si(SiO2 含量(质量分数,下同)高于69%)、富碱(K2O含量高于3.84%,Na2O含量高于4.18%)、Mg#值较高(50.4~51.0)的特征,轻稀土元素较富集,重稀土元素亏损且相对平坦,Eu呈微弱负异常(0.75~0.82),岩石富集Sr、Rb、Ba,亏损Y、Yb等,Sr/Y值为37.5~60.7,具有埃达克岩的性质。锆石Lu-Hf同位素(除去捕获锆石)分析结果表明,二长花岗岩5颗锆石具有负ε<sub>Hf(t)值(-21.59~-4.49),对应的二阶段Hf模式年龄为1 538~2 622 Ma,1颗锆石为正ε<sub>Hf(t)值(0.19),对应的二阶段Hf模式年龄为1 245 Ma,指示关山岩体来源于新元古代地壳物质。岩石具有高SiO2、Al2O3含量,相比于地幔明显较低MgO以及Cr、Ni等元素含量,指示关山岩体来源于地壳物质的熔融,岩石较高Mg#值说明其源区可能有地幔组分的加入。岩相学、地球化学、同位素特征和区域地质资料综合显示,关山岩体二长花岗岩形成于碰撞挤压环境,是下地壳增厚环境下脱水部分熔融的产物,其中伴随有地幔组分的加入。
Abstract:
Guanshan area is located in the junction of North Qinling and North Qilian orogenic belt, and it has a lot of controversy about the genesis of Guanshan pluton at present. The zircon U-Pb dating results show that the monzogranite of Guanshan pluton is formed in(236.3±4.0)Ma(the number of sample is 6, MSWD is 2.6). Late Triassic Guanshan monzogranite in North Qinling displays the characteristics of high Si(the content of SiO2 is more than 69%)and alkali-rich(the content of K2O is more than 3.84%, that of Na2O is more than 4.18%), Mg# is on the high side(50.4-51.0), LREE is enriched, HREE is depleted and flat, Eu has a non-obvious negative anomaly(0.75-0.82). The rock is enriched in Sr, Rb, Ba, and depleted in Y, Yb and other elements, the ratio of Sr/Y is 37.5-60.7, indicating that the rock has the propertieswith adakite. Zircon Lu-Hf isotope displays that 5 grains of the monzogranite have negative εHf(t)(-21.59--4.49)with corresponding two-stage Hf pattern ages of 1 538-2 622 Ma, and 1 grain has positive εHf(t)(0.19)with two-stage Hf pattern age of 1 245 Ma, indicating that Guanshan pluton is derived from the melting of Neoproterzoic crustal material. The rock has high SiO2 and Al2O3 contents, low MgO, Cr and Ni contents, indicating the pluton derives from the melting of crustal material. Compared with the standard value of the crust, the higher Mg# indicates the addition of the mantle component in the source of Guanshan pluton. The petrography, geochemistry, isotopic characteristics and regional geological data comprehensively show that the monzogranite of Guanshan pluton is formed under the tectonic setting of collisional compression, and the lower crust is thickened, dehydrated and melted with the addition of mantle components.

参考文献/References:


[1] 赖绍聪,张国伟,杨瑞瑛.南秦岭巴山弧两河—饶峰—五里坝岛弧岩浆带的厘定及其大地构造意义[J].中国科学:D辑,地球科学,2000,30(增1):53-63.
LAI Shao-cong,ZHANG Guo-wei,YANG Rui-ying.Identification of the Island-arc Magmatic Zone in the Lianghe-Raofeng-Wuliba Area,South Qinling and Its Tectonic Significance[J].Science in China:Series D,Earth Sciences,2000,30(S1):53-63.
[2] MAO J W,XIE G Q,BIERLEIN F,et al.Tectonic Implications from Re-Os Dating of Mesozoic Molybdenum Deposits in the East Qinling-Dabie Orogenic Belt[J].Geochimica et Cosmochimica Acta,2008,72(18):4607-4626.
[3] GAN B P,LAI S C,QIN J F,et al.Neoproterozoic Alkaline Intrusive Complex in the Northwestern Yang-tze Block,Micang Mountains Region,South China:Petrogenesis and Tectonic Significance[J].International Geology Review,2016,59(3):311-332.
[4] QIN J F,LAI S C,LI Y F.Multi-stage Granitic Magmatism During Exhumation of Subducted Continental Lithosphere:Evidence from the Wulong Pluton,South Qinling[J].Gondwana Research,2013,24(3/4):1108-1126.
[5] 赖绍聪,张国伟,裴先治.南秦岭勉略结合带琵琶寺洋壳蛇绿岩的厘定及其大地构造意义[J].地质通报,2002,21(8):465-470.
LAI Shao-cong,ZHANG Guo-wei,PEI Xian-zhi.Geochemistry of the Pipasi Ophiolite in the Mianlue Suture Zone,South Qinling,and Its Tectonic Significance[J].Geological Bulletin of China,2002,21(8):465-470.
[6] 赖绍聪,杨瑞瑛,张国伟.南秦岭西乡群孙家河组火山岩形成构造背景及其大地构造意义的讨论[J].地质科学,2001,36(3):295-303.
LAI Shao-cong,YANG Rui-ying,ZHANG Guo-wei.Tectonic Setting and Implication of the Sunjiahe Volcanic Rocks,Xixiang Group,in South Qinling[J].Chinese Journal of Geology,2001,36(3):295-303.
[7] 李 桐,巨银娟,赖绍聪,等.北秦岭—祁连结合带扫帚滩辉长岩年代学、地球化学特征及其地质意义[J].地球化学,2017,46(3):219-230.
LI Tong,JU Yin-juan,LAI Shao-cong,et al.Geochemistry and Chronology of the Early-Paleozoic Gabbro from the Saozhoutan Area in the North Qinling-Qilian Junction Zone:Its Petrogenesis and Geodynamic Implications[J].Geochemistry,2017,46(3):219-230.
[8] 张志华,赖绍聪,秦江锋.北秦岭太白山晚中生代正长花岗岩成因及其地质意义[J].岩石学报,2014,30(11):3242-3254.
ZHANG Zhi-hua,LAI Shao-cong,QIN Jiang-feng.Petrogenesis and Its Geological Significance of the Late Mesozoic Syengranite from the Taibai Mountain,North Qinling[J].Acta Petrologica Sinica,2014,30(11):3242-3254.
[9] 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.
WANG Xiao-xia,WANG Tao,QI Qiu-ju,et al.Temporal-spatial Variations,Origin and Their Tectonic Significance of the Late Mesozoic Granites in the Qinling,Central China[J].Acta Petrologica Sinica,2011,27(6):1573-1593.
[10] 张 旗,王 焰,刘红涛,等.中国埃达克岩的时空分布及其形成背景,附:国内关于埃达克岩的争论[J].地学前缘,2003,10(4):385-400.
ZHANG Qi,WANG Yan,LIU Hong-tao,et al.On the Space Time Distribution and Geodynamic Environments of Adakites in China,Annex:Controversies over Differing Opinions for Adakites in China[J].Earth Science Frontiers,2003,10(4):385-400.
[11] 张宏飞,王 婧,徐旺春,等.俯冲陆壳部分熔融形成埃达克质岩浆[J].高校地质学报,2007,13(2):224-234.
ZHANG Hong-fei,WANG Jing,XU Wang-chun,et al.Derivation of Adakitic Magma by Partial Melting of Subducted Continental Crust[J].Geological Journal of China Universities,2007,13(2):224-234.
[12] 殷龙飞,刘坤鹏,于宏伟.北秦岭成矿带西段关山岩体地球化学特征与铀成矿[J].西部资源,2016(4):14-16.
YIN Long-fei,LIU Kun-peng,YU Hong-wei.Geochemical Characteristics and Uranium Mineralization of Guanshan Rock Mass in the Western Part of Northern Qinling Metallogenic Belt[J].Western Resources,2016(4):14-16.
[13] 张成立,王 涛,王晓霞.秦岭造山带早中生代花岗岩成因及其构造环境[J].高校地质学报,2008,14(3):304-316.
ZHANG Cheng-li,WANG Tao,WANG Xiao-xia.Origin and Tectonic Setting of the Early Mesozoic Granitoids in Qinling Orogenic Belt[J].Geological Journal of China Universities,2008,14(3):304-316.
[14] 徐学义.西秦岭北缘花岗质岩浆作用及构造演化[J].岩石学报,2014,30(2):371-389.
XU Xue-yi.Granitoid Magmatism and Tectonic Evolution in Northern Edge of the Wstern Qinling Terrane[J].Acta Petrologica Sinica,2014,30(2):371-389.
[15] JIANG Y H,JIN G D,LIAO S Y,et al.Geochemical and Sr-Nd-Hf Isotopic Constraints on the Origin of Late Triassic Granitoids from the Qinling Orogen, Central China:Implications for a Continental Arc to Continent-continent Collision[J].Lithos,2010,117(1/2/3/4):183-197.
[16] 刘树文,杨朋涛,李秋根,等.秦岭中段印支期花岗质岩浆作用与造山过程[J].吉林大学学报(地球科学版),2011,41(6):1928-1943.
LIU Shu-wen,YANG Peng-tao,LI Qiu-gen,et al.Indosinian Granitoids and Orogenic Processes in the Middle Segment of the Qinling Orogen[J].Journal of Jilin University(Earth Science Edition),2011,41(6):1928-1943.
[17] 张国伟,张本仁.秦岭造山带与大陆动力学[M].北京:科学出版社,2001.
ZHANG Guo-wei,ZHANG Ben-ren.Qinling Orogenic Belt and Continental Dynamics[M].Beijing:Science Press,2001.
[18] DONG Y P,ZHANG X N,LIU X M,et al.Propagation Tectonics and Multiple Accretionary Processes of the Qinling Orogen[J].Journal of Asian Earth Sciences,2015,104:84-98.
[19] 杨 阳.秦岭造山带中段花岗岩的时空格架、源区物质及其对地壳深部物质组成的示踪[D].北京:中国地质科学院,2017.
YANG Yang.Spatial-temporal Distribution and Sources of Granitoids in the Middle Qinling Orogenic Belt,Central China:Implications for the Nature of Deep Crustal Basement[D].Beijing:Chinese Academy of Geological Sciences,2017.
[20] 王银川,裴先治,李佐臣,等.祁连造山带东端张家川地区长宁驿中元古代花岗质片麻岩LA-ICP-MS锆石U-Pb年龄及其构造意义[J].地质通报,2012,31(10):1576-1587.
WANG Yin-chuan,PEI Xian-zhi,LI Zuo-chen,et al.LA-ICP-MS Zircon U-Pb Dating of the Mesoproterozoic Granitic Gneisses at Changningyi of Zhangjiachuan Area on the Eastern Edge of the Qilian Orogenic Belt[J].Geological Bulletin of China,2012,31(10):1576-1587.
[21] 何艳红,孙 勇,陈 亮,等.陇山杂岩的LA-ICP-MS锆石U-Pb年龄及其地质意义[J].岩石学报,2005,21(1):125-134.
HE Yan-hong,SUN Yong,CHEN Liang,et al.Zircon U-Pb Chronology of Longshan Complex by LA-ICP-MS and Its Geological Significance[J].Acta Petrolo-gica Sinica,2005,21(1):125-134.
[22] 裴先治,李佐臣,李瑞保,等.祁连造山带东段早古生代葫芦河群变质碎屑岩中碎屑锆石LA-ICP-MS U-Pb年龄:源区特征和沉积时代的限定[J].地学前缘,2012,19(5):205-224.
PEI Xian-zhi,LI Zuo-chen,LI Rui-bao,et al.LA-ICP-MS U-Pb Age from the Meta-detrital Rocks of the Early Palaeozoic Huluhe Group in Eastern Part of Qilian Orogenic Belt:Constraints of Material Source and Sedimentary Age[J].Earth Science Frontiers,2012,19(5):205-224.
[23] ZHANG H F,ZHANG B R,HARRIS N,et al.U-Pb Zircon SHRIMP Ages,Geochemical and Sr-Nd-Pb Isotopic Compositions of Intrusive Rocks from the Longshan-Tianshui Area in the Southeast Corner of the Qilian Orogenic Belt,China:Constraints on Petrogenesis and Tectonic Affinity[J].Journal of Asian Earth Sciences,2006,27(6):751-764.
[24] 刘 晔,柳小明,胡兆初,等.ICP-MS测定地质样品中37个元素的准确度和长期稳定性分析[J].岩石学报,2007,23(5):1203-1210.
LIU Ye,LIU Xiao-ming,HU Zhao-chu,et al.Evaluation of Accuracy and Long-term Stability Determination of 37 Trace Elements in Geological Samples by ICP-MS[J].Acta Petrologica Sinica,2007,23(5):1203-1210.
[25] YUAN H,GAO S,LIU X,et al.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-inductively Coupled Plasma-mass Spectro-metry[J].Geostandards and Geoanalytical Research,2010,28(3):353-370.
[26] 王春林,孟明亮,鲁孝军,等.内蒙古多伦晚中生代中酸性火山岩岩石地球化学特征及构造环境分析[J].地质与勘探,2018,54(5):988-1000.
WANG Chun-lin,MENG Ming-liang,LU Xiao-jun,et al.Geochemical Characteristics of Intermediate-acid Volcanic Rocks Late Mesozoic and the Tectonic Environment in the Duolun Area,Inner Mongolia[J].Geology and Exploration,2018,54(5):988-1000.
[27] 王洪亮,肖绍文,徐学义,等.北秦岭西段吕梁期构造岩浆事件的年代学及其构造意义[J].地质通报,2008,27(10):1728-1738.
WANG Hong-liang,XIAO Shao-wen,XU Xue-yi,et al.Geochronology and Significance of the Early Meso-Proterozoic Tectono-magmatic Event in the Western Segment of the North Qinling Mountains[J].Geolo-gical Bulletin of China,2008,27(10):1728-1738.
[28] 秦江锋.秦岭造山带晚三叠世花岗岩类成因机制及深部动力学背景[D].西安:西北大学,2010.
QIN Jiang-feng.Petrogenesis and Geodynamic Implications of the Late-Triassic Granitoids from the Qinling Orogenic Belt[D].Xi’an:Northwest University, 2010.
[29] 赖绍聪,秦江锋,朱韧之,等.扬子地块西缘天全新元古代过铝质花岗岩类成因机制及其构造动力学背景[J].岩石学报,2015,31(8):2245-2258.
LAI Shao-cong,QIN Jiang-feng,ZHU Ren-zhi,et al.Petrogenesis and Tectonic Implication of the Neopro-terozoic Peraluminous Granitoids from the Tianshui Area,Western Yangtze Block[J].Acta Petrologica Sinica,2015,31(8):2245-2258.
[30] 葛小月,李献华,陈志刚,等.中国东部燕山期高Sr低Y型中酸性火成岩的地球化学特征及成因:对中国东部地壳厚度的制约[J].科学通报,2002,47(6):474-480.
GE Xiao-yue,LI Xian-hua,CHEN Zhi-gang,et al.Geo-chemical Characteristics and Petrogenesis of High-Sr Low-Y Medium-acid Igneous Rocks in Yanshanian Epoch in Eastern China:Constraints on the Thickness of Crust in Eastern China[J].Chinese Science Bulletin,2002,47(6):474-480.
[31] 张 财.西藏拉萨地块北部永珠地区岩浆岩年代学与地球化学[D].北京:中国地质大学,2016.
ZHANG Cai.Geochronology and Geochemistry of Magmatic Rock in Yongzhu at North Lhasa Block,Tibet[D].Beijing:China University of Geosciences,2016.
[32] 张 旗,许继峰,王 焰,等.埃达克岩的多样性[J].地质通报,2004,23(9/10):959-965.
ZHANG Qi,XU Ji-feng,WANG Yan,et al.Diversity of Adakite[J].Geological Bulletin of China,2004,23(9/10):959-965.
[33] SUN S S,MCDONOUGH W F.Chemical and Isoto-pic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society,London,Special Publications,1989,42:313-345.
[34] 秦江锋,赖绍聪,李永飞.扬子板块北缘碧口地区阳坝花岗闪长岩体成因研究及其地质意义[J].岩石学报,2005,21(3):157-170.
QIN Jiang-feng,LAI Shao-cong,LI Yong-fei.Petrogenesis and Geological Significance of Yangba Granodiorites from Bikou Area,Northern Margin of Yangtze Plate[J].Acta Petrologica Sinica,2005,21(3):157-170.
[35] 王晓霞,王 涛,卢欣祥.北秦岭中生代沙河湾岩体环斑结构特征及有关问题的讨论[J].地球学报,2002,23(1):30-36.
WANG Xiao-xia,WANG Tao,LU Xin-xiang.Characteristics of Rapakivi Texture in Mesozoic Shahewan Granite of North Qinling Mountains and Some Related Problems[J].Acta Geoscientica Sinica,2002,23(1):30-36.
[36] DEFANT M J,DRUMMOND M S.Derivation of
Some Modern Arc Magmas by Melting of Young Subducted Lithosphere[J].Nature,1990,347:662-665.
[37] DEFANT J,KEPEZHINSKAS P,XU J F,et al.Adakites:Some Variations on a Theme[J].Acta Petrologica Sinica,2002,18(2):129-142.
[38] THIEBLEMONT D,STEIN G,LESCUYER J L.Epi-thermal and Porphyry Deposits:The Adakite Connection[J].Comptes Rendus de l’Academie des Sciences:Series IIA,Earth and Planetary Science,1997,325(2):103-109.
[39] OYARZUN R,MARQUEZ A,LILLO J,et al.Giant Versus Small Porphyry Copper Deposits of Cenozoic Age in Northern Chile:Adakitic Versus Normal Cal-calkaline Magmatism[J].Mineralium Deposita,2001,36(8):794-798.
[40] BELLON H,YUMUL JR G P.Miocene to Quaternary Adakites and Related Rocks in Western Philippine Arc Sequences[J].Comptes Rendus de l’Academie des Sciences:Series IIA,Earth and Planetary Science,2001,333(6):343-350.
[41] WANG Q,WYMAN D A,ZHAO Z H,et al.Petrogenesis of Carboniferous Adakites and Nb-enriched Arc Basalts in the Alataw Area,Northern Tianshan Range(Western China):Implications for Phanerozoic Crustal Growth in the Central Asia Orogenic Belt[J].Chemical Geology,2007,236(1):42-64.
[42] 张 旗,王 焰,刘 伟,等.埃达克岩的特征及其意义[J].地质通报,2002,21(7):431-435.
ZHANG Qi,WANG Yan,LIU Wei,et al.Adakite: Its Characteristics and Implications[J].Geological Bulletin of China,2002,21(7):431-435.
[43] MARTIN H,SMITHIES R H,RAPP R,et al.An Overview of Adakite,Tonalite-trondhjemite-granodiorite(TTG),and Sanukitoid:Relationships and Some Implications for Crustal Evolution[J].Lithos,2005,79(1):1-24.
[44] 肖 龙.富钾埃达克岩:加厚下地壳变质基性岩脱水熔融的产物[C]∥中国地质学会.2004年全国岩石学与地球动力学研讨会论文集.北京:地质出版社,2004:283.
XIAO Long.Potassium-rich Adakite:Dehydration and Melting Products of Thickened Lower Crust Metamorphic Rocks[C]∥Geological Society of China.Proceedings of the National Petrology and Geodynamics Symposium Conference Proceedings in 2004.Beijing:Geological Publishing House,2004:283.
[45] ATHERTON M P,PETFORD N.Generation of Sodium-rich Magmas from Newly Underplated Basaltic Crust[J].Nature,1993,362:144-146.
[46] MARTIN H.Adakitic Magmas:Modern Analogues of Archaean Granitoids[J].Lithos,1999,46(3):411-429.
[47] XU J F,SHINJO R,DEFANT M J,et al.Origin of Mesozoic Adakitic Intrusive Rocks in the Ningzhen Area of East China:Partial Melting of Delaminated Lower Continental Crust?[J].Geology,2002,30(12):1111-1114.
[48] GAO S,RUDNICK R L,YUAN H L,et al.Recycling Lower Continental Crust in the North China Craton[J].Nature,2004,432:892-897.
[49] WANG Q,XU J F,JIAN P,et al.Petrogenesis of Adakitic Porphyries in an Extensional Tectonic Setting,Dexing,South China:Implications for the Genesis of Porphyry Copper Mineralization[J].Journal of Petrology,2006,47(1):119-144.
[50] CHUNG S L,LIU D,JI J,et al.Adakites from Continental Collision Zones:Melting of Thickened Lower Crust Beneath Southern Tibet[J].Geology,2003,31(11):1021-1024.
[51] HOU Z Q,GAO Y F,QU X M,et al.Origin of Adakitic Intrusives Generated During Mid-Miocene East-west Extension in Southern Tibet[J].Earth and Planetary Science Letters,2004,220(1/2):139-155.
[52] WANG Q,MCDERMOTT F,XU J F,et al.Cenozoic K-rich Adakitic Volcanic Rocks in the Hohxil Area,Northern Tibet:Lower-crustal Melting in an Intracontinental Setting[J].Geology,2005,33(6):465-468.
[53] ROBERTS M P,CLEMENS J D.Origin of High-potassium,Calc-alkaline,I-type Granitoids[J].Geology,1993,21(9):825.
[54] HOFMANN A W.Mantle Geochemistry:The Message from Oceanic Volcanism[J].Nature,1997,385:219-229.
[55] 许立权,邓晋福,陈志勇,等.内蒙古达茂旗北部奥陶纪埃达克岩类的识别及其意义[J].现代地质,2003,17(4):428-434.
XU Li-quan,DENG Jin-fu,CHEN Zhi-yong,et al.The Identification of Ordovician Adakites and Its Significance in Northern Damao,Inner Mongolia[J].Geo-science,2003,17(4):428-434.
[56] 方博文,张 贺,叶日胜,等.南秦岭老城花岗岩成因:锆石U-Pb年龄和Sr-Nd同位素的制约[J].地球科学与环境学报,2017,39(5):633-651.
FANG Bo-wen,ZHANG He,YE Ri-sheng,et al.Petrogenesis of Laocheng Granite in South Qinling:Constraints from Zircon U-Pb Age and Sr-Nd Isotopic Composition[J].Journal of Earth Sciences and Environment,2017,39(5):633-651.
[57] 张国伟,孟庆任,于在平,等.秦岭造山带的造山过程及其动力学特征[J].中国科学:D辑,地球科学,1996,26(3):193-200.
ZHANG Guo-wei,MENG Qing-ren,YU Zai-ping,et al.The Orogenic Process and Dynamic Characteristics of the Qinling Orogenic Belt[J].Science in China:Series D,Earth Sciences,1996,26(3):193-200.
[58] 林 鑫,刘 浩,梁利鹏,等.北秦岭及周缘花岗岩地球化学特征与构造环境分析[J].矿物岩石,2016,36(4):74-85.
LIN Xin,LIU Hao,LIANG Li-peng,et al.Research of Geochemistry of Granitoids in the Northern Qinling Orogen and Their Tectonic Setting[J].Journal of Mineralogy and Petrology,2016,36(4):74-85.
[59] 张成立,罗静兰,李 淼,等.东秦岭西坝花岗岩体及其脉岩的地球化学特征[J].西北大学学报(自然科学版),2002,32(4):384-388.
ZHANG Cheng-li,LUO Jing-lan,LI Miao,et al.Geochemical Characteristics and Geological Significance of Xiba Granite,Porphyry and Porphyrite in East Qinling[J].Journal of Northwest University(Natural Science Edition),2002,32(4):384-388.
[60] AMES L,ZHOU G,XIONG B.Geochronology and
Geochemistry of Ultrahigh-pressure Metamorphism with Implications for Collision of Sino-Korea Cratons,Central China[J].Tectonics,1996,15(2):472-489.
[61] HACKER B R,RATSCHBACHER L,WEBB L,et al.U/Pb Zircon Ages Constrain the Architecture of the Ultrahigh-pressure Qinling-Dabie Orogen,China[J].Earth and Planetary Science Letters,1998,161(1/2/3/4):215-230.
[62] AYERS J C,DUNKLE S,GAO S,et al.Constraints on Timing of Peak and Retrograde Metamorphism in the Dabie Shan Ultrahigh-pressure Metamorphic Belt,East-central China,Using U-Th-Pb Dating of Zircon and Monazite[J].Chemical Geology,2002,186(3):315-331.
[63] 张宏飞,欧阳建平,凌文黎,等.南秦岭宁陕地区花岗岩类Pb、Sr、Nd同位素组成及其深部地质信息[J].岩石矿物学杂志,1997,16(1):22-32.
ZHANG Hong-fei,OUYANG Jian-ping,LING Wen-li,et al.Pb,Sr and Nd Isotope Composition of Ning-shan Granitoids,South Qinling and Their Deep Geological Information[J].Acta Petrologica et Mineralo-gica,1997,16(1):22-32.
[64] 张宏飞,靳兰兰,张 利,等.西秦岭花岗岩类地球化学和Pb-Sr-Nd同位素组成对基底性质及其构造属性的限制[J].中国科学:D辑,地球科学,2005,35(10):10-22.
ZHANG Hong-fei,JIN Lan-lan,ZHANG Li,et al.Geochemical and Pb-Sr-Nd Isotopic Compositions of Granitoids from Western Qinling Belt:Constraints on Basement Nature and Tectonic Affinity[J].Science in China:Series D,Earth Sciences,2005,35(10):10-22.

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备注/Memo

备注/Memo:
收稿日期:2018-10-05; 修回日期:2018-11-24 投稿网址:http://jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41190072)
作者简介:杨 航(1996-),男,河南临颍人,理学硕士研究生,E-mail:yanghang6768@163.com。
*通讯作者:赖绍聪(1963-),男,四川安岳人,教授,博士研究生导师,理学博士,E-mail:shaocong@nwu.edu.cn。
更新日期/Last Update: 2019-02-28