Age and origin of Muzidian fine-grained monzogranite dyke in Dabie orogenic belt: Zircon U-Pb dating and Hf isotopic constraints

LIU Jinsong; HU Junliang; LIU Asui; JIN Shichao; DING Li

2016 Vol. 35, No. 12

Article Contents

Article navigation > Geological Bulletin of China > 2016 > 35(12): 2088-2099

Next Article Previous Article

LIU Jinsong, HU Junliang, LIU Asui, JIN Shichao, DING Li. Age and origin of Muzidian fine-grained monzogranite dyke in Dabie orogenic belt: Zircon U-Pb dating and Hf isotopic constraints[J]. Geological Bulletin of China, 2016, 35(12): 2088-2099.

Citation:

LIU Jinsong, HU Junliang, LIU Asui, JIN Shichao, DING Li. Age and origin of Muzidian fine-grained monzogranite dyke in Dabie orogenic belt: Zircon U-Pb dating and Hf isotopic constraints[J]. Geological Bulletin of China, 2016, 35(12): 2088-2099.

Age and origin of Muzidian fine-grained monzogranite dyke in Dabie orogenic belt: Zircon U-Pb dating and Hf isotopic constraints

1. Wuhan Center of Geological Survey, China Geological Survey, Wuhan 430205, Hubei, China;
2. Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, Hubei, China

Received Date: 01 December 2015

Revised Date: 02 February 2016

Publish Date: 15 December 2016

Abstract

Abstract

This paper presents LA-ICP-MS zircon U-Pb dating and zircon in-situ Hf isotopic analytical results for the Muzidian fine-grained monzogranite dyke in northern Dabie orogenic belt. The dating results show that the granite was formed at 128.9±0.7Ma in Early Cretaceous. Two Paleoproterozoic and Neoproterozoic inherited zircons were found in the granites. The Hf isotopic analytical results show that the zircons ε_Hf(t) values are from -25.1 to -19.2 with the mean of -22.7, and the two-stage Hf model ages (T_DM2) generally range from 2115Ma to 2505Ma. The ε_Hf(t) values of the two inherited zircons are -10.5 and 6.5, with the corresponding T_DM2 of 1151Ma and 1709Ma, respectively. The zircon U-Pb dating and in-situ Hf isotopic results indicate that the parental magmas of Muzidian finegrained monzogranite dyke were derived from partial melting of Paleoproterozoic crustal rocks, with some Mesoproterozoic mantle and Archean crustal materials probably making contributions to the source. The Muzidian finegrained monzogranite dyke is considered to have been formed at the time of tectonic transition from compression to extension during Early Cretaceous in the Dabie orogen.
- fine-grained monzogranites /
- LA-ICP-MS zircon U-Pb dating /
- Hf isotope /
- Muzidian /
- Dabie orogenic belt

FullText(HTML)

References

[1]	Xue F,Rowley D B,Tucker R D,et al.U-Pb zircon ages of granitoid rocks in the north Dabie complex,eastern Dabie Shan,China[J].Journal of Geology,1997,105:744-753. Google Scholar
[2]	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,1998,161:215-230. Google Scholar
[3]	薛怀民,董树文,刘晓春.北大别东部白垩纪埃达克质火山岩及其锆石U-Pb年代学[J].地球化学,2002,31(5):455-463. Google Scholar
[4]	薛怀民,马芳,赵逊,等.大别山造山带东南部天柱山花岗岩类侵入体的特征及其LA-ICP-MS锆石U-Pb年龄[J].岩石矿物学杂志2011,30(5):935-950. Google Scholar
[5]	Xie Z,Zheng Y F,Zhao Z F,et al.Mineral isotope evidence for the contemporaneous process of Mesozoic granite emplacement and gneiss metamorphism in the Dabie orogen[J].Chemical Geology,2006,231:214-235. Google Scholar
[6]	Zhao Z F,Zheng Y F,Wei C S,et al.Post-collisional granitoids from the Dabie orogen in China:Zircon U-Pb age,element and Oisotope evidence for recycling of subducted continental crust[J].Lithos,2007,93:248-272. Google Scholar
[7]	Xu H J,Ma C Q,Ye K.Early cretaceous granitoids and their implications for the collapse of the Dabie orogen,eastern China:SHRIMP zircon U-Pb dating and geochemistry[J].Chemical Geology,2007,240:238-259. Google Scholar
[8]	赵新福,李建威,马昌前,等.北淮阳古碑花岗闪长岩侵位时代及地球化学特征:对大别山中生代构造体制转换的启示[J].岩石学报,2007,23(6):1392-1402. Google Scholar
[9]	周红升,马昌前,陈玲.大别造山带研子岗碱性岩体成因及其构造意义:锆石U-Pb年龄和地球化学制约[J].岩石学报,2009,25(5):1079-1091. Google Scholar
[10]	周红升,刘明华,严育通,等.大别造山带新县岩体的锆石U-Pb年龄及其地质意义[J].信阳师范学院学报:自然科学版,2015,26(1):94-98. Google Scholar
[11]	吴开彬,邓新,杨坤光.北大别白垩纪花岗岩多期侵位与造山带演化的关系[J].地球科学-中国地质大学学报,2013,38(S1):43-52. Google Scholar
[12]	周伟伟,蔡剑辉,阎国翰,等.安徽金寨响洪甸碱性侵入岩年代学、岩石地球化学及其意义[J].矿床地质,2014,33(1):104-122. Google Scholar
[13]	刘晓强,闫峻,王爱国,等.北大别岳西岩体和飞旗寨岩体的LAICPMS锆石U-Pb定年及其地质意义[J].地球化学,2015,44(2):155-166. Google Scholar
[14]	Ma C Q,Li Z C,Ehlers C,et al.A post-collisional magmatic plumbing system:Mesozoic granitoid plutons from the Dabieshan high-pressure and ultrahigh-pressure metamorphic zone,east-central China[J].Lithos,1998,45:431-456. Google Scholar
[15]	Chen B,Jahn B M,Wei C J.Petrogenesis of Mesozoic granitoids in the Dabie UHP complex,Central China:trace element and NdSr isotope evidence[J].Lithos,2002,60:67-88. Google Scholar
[16]	Zhang H F,Gao S,Zhong Z Q,et al.Geochemical and Sr-NdPb isotopic compositions of Cretaceous granitoids:Constraints on tectonic framework and crustal structure of the Dabieshan ultrahighpressure metamorphic belt,China[J].Chemical Geology,2002,186:281-299. Google Scholar
[17]	Yang J H,Wu F Y,Chung S L,et al.Petrogenesis of Early Cretaceous intrusions in the Sulu ultrahigh-pressure orogenic belt,east China and their relationship to lithospheric thinning[J].Chemical Geology,2005,222:200-231. Google Scholar
[18]	Wang Q,Wyman D A,Xu J F,et al.Early Cretaceous adakitic granites in the Northern Dabie Complex,central China:Implications for partial melting and delamination of thickened lower crust[J].Geochi-mica et Cosmochimica Acta,2007,71(10):2609-2636. Google Scholar
[19]	He Y S,Li S G,Hoefs J,et al.Postcollisional granitoids from the Dabie orogen:New evidence for partial melting of a thickened continental crust[J].Geochimica et Cosmochimica Acta,2011,75(13):3815-3838 Google Scholar
[20]	He Y S,Li S G,Hoefs J,et al.Sr-Nd-Pb isotopic compositions of Early Cretaceous granitoids from the Dabie orogen:Constraints on the recycled lower continental crust[J].Lithos,2013,156/159:204-217. Google Scholar
[21]	Zhao Z F,Zheng Y F,Wei C S,et al.Origin of postcollisional magmatic rocks in the Dabie orogen:Implications for crust-mantle interaction and crustal architecture[J].Lithos,2011,126:99-114. Google Scholar
[22]	Xu H J,Ma C Q,Zhang J F,et al.Early Cretaceous low-Mg adakitic granites from the Dabie orogen,eastern China:Petrogenesis and implications for destruction of the over-thickened lower continental crust[J].Gondwana Research,2012,23:190-207. Google Scholar
[23]	李曙光,洪吉安,李惠民,等.大别山辉石岩-辉长岩体锆石UPb年龄及其地质意义[J].高校地质学报,1999,5(3):351-355. Google Scholar
[24]	王江海,邓尚贤.湖北北大别镁铁-超镁铁质侵入体的时代:锆石U-Pb、Sm-Nd和⁴⁰Ar/³⁹Ar定年结果[J].中国科学(D辑),2002,32(1):1-9. Google Scholar
[25]	侯振辉,李曙光.大别造山带超高压变质岩和镁铁质岩浆岩锆石U-Pb年代学的TIMS和SIMS法定年结果比较[J].岩石学报,2003,19(3):490-496. Google Scholar
[26]	赵子福,郑永飞,魏春生,等.大别山沙村和椒子岩基性-超基性岩锆石U-Pb定年、元素和碳氧同位素地球化学研究[J].高校地质学报,2003,9(2):139-162. Google Scholar
[27]	Zhao Z F,Zheng Y F,Wei C S,et al.Zircon U-Pb age,element and C-O isotope geochemistry of post-collisional mafic-ultramafic rocks from the Dabie orogen in east-central China[J].Lithos,2005,83:1-28. Google Scholar
[28]	Huang F,Li S G,Dong F,et al.Recycling of deeply subducted continental crust in the Dabie Mountains,central China[J].Lithos,2007,96:151-169. Google Scholar
[29]	陈玲,马昌前,张金阳,等.首编大别造山带侵入岩地质图(1:50万)及其说明[J].地质通报,2012,31(1):13-20. Google Scholar
[30]	任志,周涛发,袁峰,等.安徽沙坪沟钼矿区中酸性侵入岩期次研究—年代学及岩石化学约束[J].岩石学报,2014,30(4):1097-1116. Google Scholar
[31]	刘清泉,邵拥军,张智慧,等.大别山姚冲花岗岩锆石U-Pb年龄、Hf同位素及地质意义[J].中国有色金属学报,2015,25(2):479-491. Google Scholar
[32]	赵子福,郑永飞,魏春生,等.大别山中生代中酸性岩浆岩锆石U-Pb定年、元素和氧同位素地球化学研究[J].岩石学报,2004,20(5):1151-1174. Google Scholar
[33]	杨泽强,唐相伟.北大别山肖畈岩体地球化学特征和锆石LAICPMS U-Pb同位素定年[J].地质学报,2015,89(4):692-700. Google Scholar
[34]	Griffin W L,Wang X,Jackson S E,et al.Zircon chemistry and magma genesis,SE China:In-situ analysis of Hf isotopes,Tonglu and Pingtan igneous complexes[J].Lithos,2002,61:237-269 Google Scholar
[35]	Zhang D Y,Zhang Z C,Encarnación J,et al.Petrogenesis of the Kekesai composite porphyry intrusion,western Tianshan,NW China:Implications for metallogenesis,tectonic evolution and continental growth during Late Paleozoic time[J].Lithos,2012,146/147:65-79. Google Scholar
[36]	续海金,叶凯,马昌前.北大别早白至纪花岗岩类的Sm-Nd和锆石Hf同位素及其构造意义[J].岩石学报,2008,24(1):83-103. Google Scholar
[37]	高昕宇,赵太平,施小斌,等.大别山北麓早白垩世商城和达权店岩体的地球化学特征与成因[J].地球化学,2013,42(4):307-339. Google Scholar
[38]	高阳,叶会寿,李永峰,等.大别山千鹅冲钼矿区花岗岩的SHRIMP锆石U-Pb年龄、Hf同位素组成及微量元素特征[J].岩石学报,2014,30(1):49-63. Google Scholar
[39]	王清晨,丛柏林.大别山超高压变质带的大地构造框架[J].岩石学报,1998,14(4):481-492. Google Scholar
[40]	高山,张本仁,金振民.秦岭-大别造山带下地壳拆沉作用[J].中国科学(D辑),1999,29(6):532-541. Google Scholar
[41]	戴圣潜,邓晋福,吴宗絮,等.大别造山带燕山期造山作用的岩浆岩石学证据[J].中国地质,2003,30(2):159-165. Google Scholar
[42]	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 of Mantle Xenoliths[J].Journal of Petrology,2010,51:537-571. Google Scholar
[43]	Hu Z C,Liu Y S,Gao S,et al.Improved in situ Hf isotope ratio analysis of zircon using newly designed X skimmer cone and Jet sample cone in combination with the addition of nitrogen by laser ablation multiple collector ICP-MS[J].Journal of Analytical Atomic Spectrometry,2012,27:1391-1399. Google Scholar
[44]	Blichert T J,Chauvel C,Albarède F.Separation of Hf and Lu for high-precision isotope analysis of rock samples by magnetic sectormultiple collector ICP-MS[J].Contributions to Mineralogy and Petrology,1997,127:248-260. Google Scholar
[45]	Scherer E,Munker C,Mezger K.Calibration of the lutetium-hafnium clock[J].Science,2001,293:683-687. Google Scholar
[46]	Blichert-Toft J,Albarède F.The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system[J].Earth and Planetary Science Letters,1997,148:243-258. Google Scholar
[47]	Vervoort J D,Blichert-Toft J.Evolution of the depleted mantle:Hf isotope evidence from juvenile rocks through time[J].Geochimica et Cosmochimica Acta,1999,63:533-556. Google Scholar
[48]	Griffin W L,Pearson N J,Belousova E,et al.The Hf isotope composition of cratonic mantle:LA-MC-ICP-MS analysis of zircon megacrysts in kimberlites[J].Geochimica et Cosmochimica Acta,2000,64:133-147. Google Scholar
[49]	吴福元,李献华,郑永飞,等.Lu-Hf同位素体系及其岩石学应用[J].岩石学报,2007,23(2):185-220. Google Scholar
[50]	吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589-1604. Google Scholar
[51]	Cherniak D J,Watson E B.Pb diffusion in zircon[J].Chemical Ge-ology,2000,172:5-24. Google Scholar
[52]	邱检生,肖娥,胡建,等.福建北东沿海高分异I型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约[J].岩石学报,2008,24(11):2467-2484. Google Scholar
[53]	Li S G,Yang W.Decoupling of surface and subsurface sutures in the Dabie orogen and a continent-collisional lithospheric-wedging model:Sr-Nd-Pb isotopic evidences of Mesozoic igneous rocks in eastern China[J].Chinese Science Bulletin,2003,48:831-838. Google Scholar
[54]	Wang Y J,Fan W M,Peng T P,et al.Nature of the Mesozoic lithospheric mantle and tectonic decoupling beneath the Dabie orogen,Central China:Evidence from ⁴⁰Ar/³⁹Ar geochronology,elemental and Sr-Nd-Pb isotopic compositions of early Cretaceous mafic igneous rocks[J].Chemical Geology,2005,220:165-189. Google Scholar
[55]	Zheng Y F,Fu B,Gong B,et al.Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China:Implications for geodynamics and fluid regime[J].Earth Science Reviews,2003,62:105-161. Google Scholar
[56]	Huang J,Zheng Y F,Zhao Z F.Melting of subducted continent:element and isotopic evidence for a genetic relationship between Neoproterozoic and Mesozoic granitoids in the Sulu orogen[J].Chemical Geology,2006,229:227-256. Google Scholar
[57]	赵子福,郑永飞.俯冲大陆岩石圈重熔:大别-苏鲁造山带中生代岩浆岩成因[J].中国科学(D辑),2009,39(7):888-909. Google Scholar
[58]	陈伟,徐兆文,李红超,等.河南新县花岗岩岩基的岩石成因、来源及对西大别构造演化的启示[J].岩石学报,2013,87(10):1510-1524. Google Scholar
[59]	Zhang S B,Zheng Y F,Zhao Z F,et al.Neoproterozoic anatexis of Archean lithosphere:Geochemical evidence from felsic to mafic instrusions at Xiaofeng in the Yangtze Gorge,South China[J].Precambrian Research,2008,163:210-238. Google Scholar
[60]	Zhang S B,Zheng Y F,Zhao Z F,et al.Origin of TTG-like rocks from anatexis of ancient lower crust:Geochemical evidence from Neoproterozoic granitoids in South China[J].Lithos,2009,113:347-368. Google Scholar
[61]	Zhao Z F,Zheng Y F,Wei C K,et al.Zircon U-Pb ages,Hf and O isotopes constrain the crustal architecture of the ultrahigh-pressure Dabie orogen in China[J].Chemical Geology,2008,253:222-242. Google Scholar
[62]	Chen W,Xu Z W,Qiu W H,et al.Petrogenesis of the Yaochong granite and Mo deposit,Western Dabie orogen,eastern-central China:Constraints from zircon U-Pb and molybdenite Re-Os ages,Sr-Nd-Pb-Hf isotopes[J].Journal of Asian Earth Sciences,2015,103:198-211. Google Scholar
[63]	Wang G G,Ni P,Yu W,et al.Petrogenesis of Early Cretaceous post-collisional granitoids at Shapinggou,Dabie Orogen Implications for crustal architecture and porphyry Mo mineralization[J].Lithos,2014,184/187:393-415. Google Scholar
[64]	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 Petrology,2002,143(5):602-622. Google Scholar
[65]	敖文昊,张宇昆,张瑞英,等.新元古代扬子北缘地壳增生事件:来自汉南祖师店奥长花岗岩地球化学、锆石LA-ICP-MS U-Pb年代学和Hf同位素证据[J].地质论评,2014,60(6):1393-1408. Google Scholar
[66]	Qiu Y M,Gao S,McNaughton N J,et al.First evidence of ≥3.2 Ga continental crust in the Yangtze craton of south China and its implications for Archean crustal evolution and Phanerozoic tectonics[J].Geology,2000,28:11-14. Google Scholar
[67]	Zhang S B,Zheng Y F,Wu Y B,et al.Zircon isotope evidence for ≥3.5Ga continental crust in the Yangtze craton of China[J].Pre-cambrian Res.,2006,146:16-34. Google Scholar
[68]	Zhang S B,Zheng Y F,Wu Y B,et al.Zircon U-Pb age and HfO isotope evidence for Paleoproterozoic metamorphic event in South China[J].Precambian Res.,2006,151:265-288. Google Scholar
[69]	Zhang S B,Zheng Y F,Wu Y B,et al.Zircon U-Pb age and Hf isotope evidence for 3.8 Ga crustal remnant and episodic reworking of Archean crust in South China[J].Earth Planet.Sci.Lett.,2006,252:56-71. Google Scholar
[70]	Zheng J P,Griffin W L,O'Reilly S Y,et al.Widespread Archean basement beneath the Yangtze craton[J].Geology,2006,34:417-420. Google Scholar
[71]	Li S G,Jagoutz E,Chen Y Z,et al.Sm-Nd and Rb-Sr isotopic chronology and cooling history of ultrahigh pressure metamorphic rocks and their country rocks at Shuanghe in the Dabie Mountains,Central China[J].Geochim Cosmochim Acta,2000,64:1077-1093. Google Scholar
[72]	李曙光,李秋立,侯振辉,等.大别山超高压变质岩的冷却史及折返机制[J].岩石学报,2005,21(4):1117-1124. Google Scholar
[73]	刘福来,薛怀民,许志琴,等.大别超高压变质带的进变质、超高压和退变质时代的准确限定:以双河大理岩中榴辉岩锆石SHRIMP U-Pb定年为例[J].岩石学报,2006,22(7):1761-1778. Google Scholar
[74]	Liu F L,Gerdes A,Robinson P T,et al.Zoned zircon from eclogite lenses in marbles from the Dabie-Sulu UHP belt:A clear record of ultra-deep subduction and fast exhumation[J].Geochim Cosmochim Acta,2007,81:204-225. Google Scholar
[75]	Liu Y C,Li S G,Xu S T.Zircon SHRIMP U-Pb dating for gneisses in northern Dabie high TIP metamorphic zone,central China:Implications for decoupling within subducted continental crust[J].Lithos,2007,96:170-185. Google Scholar
[76]	Li S G,Xiao Y L,Liu D L,et al.Collision of the North China and Yangtse Blocks and formation of coesite-bearing eclogites:Timing and processes[J].Chemical Geology,1993,109:89-111. Google Scholar
[77]	Leech M L.Arrested orogenic development:Eclogitization,delamination,and tectonic collapse[J].Earth and Planetary Science Letters,2001,185:149-159. Google Scholar
[78]	许长海,周祖翼,马昌前,等.大别造山带140-85Ma热窿伸展作用—年代学约束[J].中国科学(D辑),2001,31(11):925-937. Google Scholar
[79]	马昌前,杨坤光,明厚利,等.大别山中生代地壳从挤压转向伸展的时间:花岗岩的证据[J].中国科学(D辑),2003,33(9):817-827. Google Scholar