Geochemistry, geochronology and Hf isotopic compositions of metagabbro dykes on the northwestern margin of Oulongbuluke micro-block on the northern margin of Qaidam Basin
-
摘要:
侵位于柴北缘构造带欧龙布鲁克地块西北缘达肯大坂岩群中的辉长岩脉岩石Al2O3、CaO含量较高,P2O5、TiO2含量较低,属于钙碱性系列。稀土元素总量低(43.17×10-6~57.53×10-6),LREE/HREE值为1.82~2.77,稀土元素配分曲线整体表现为右倾型。岩石Ti亏损,具高ThN/NbN值(3.75~8.03)和低Nb/La值(0.44~0.84)特征。辉长岩锆石的176Hf/177Hf值介于0.282813~0.282979之间,εHf(t)值为9.25~15.11,Hf模式年龄(TDM)分布在378~610Ma之间,平均494Ma。综合研究认为,辉长岩岩浆源区为软流圈地幔且后期可能受到壳源富集组分的混染。LA-ICP-MS锆石U-Pb定年结果表明,辉长岩脉形成于357±4Ma,即早石炭世。结合区域地质背景,认为早石炭世柴北缘仍处于后造山伸展的构造演化阶段,而辉长岩脉是后造山伸展阶段柴北缘造山带去根、软流圈地幔上涌作用形成的。
Abstract:Metagabbro dykes were emplaced in the Dakendaban Rock Group on the northwestern margin of the Oulongbuluke Block, northern margin of Qaidam. They are characterized by higher Al2O3, CaO but lower P2O5, TiO2, belonging to subalkalic calcalkaline series. Meanwhile, the rocks have lower Σ REE and LREE/HREE ratios between 1.82~2.77, with the chondritenormalized REE showing right-inclined patterns. The rocks are characterized by low Ti and Nb/La(0.44~0.84), but high ThN/NbN (3.75~8.03). The εHf(t)values vary in the range of 9.25~15.11, 176Hf/177Hf ratios vary from 0.282813 to 0.282979, and Hf model ages vary from 378Ma to 610Ma. Comprehensive researches show that the magma of metagabbro dykes was derived from asthenosphere mantle, and was probably contaminated by the crust. LA-ICP-MS zircon U-Pb dating of metagabbro dykes in the Dakendaban Rock Group yielded the formation age of 357±4Ma. Combined with regional geological background, the authors hold that the northwestern margin of the Qaidam Basin was still in the extensional tectonic stage in Early Carboniferous, and the rocks were formed under the condition of unrooting of the north of Qaidam orogenic belt and the upwelling of asthenospheric mantle.
-
Key words:
- metagabbro dykes /
- geochemistry /
- geochronology /
- Hf isotopic /
- northern margin of the Qaidam
-
图 5 辉长岩稀土元素球粒陨石标准化图解(a)和微量元素原始地幔标准化蛛网图(b)[37]
Figure 5.
图 8 辉长岩锆石年龄-εHf(t)图解(底图据参考文献[45])
Figure 8.
图 9 辉长岩ThN/NbN-Nb/La图解(底图据参考文献[48])
Figure 9.
表 1 辉长岩主量、微量及稀土元素含量分析结果
Table 1. Major, trace elements and REE compositions of metagabbro
表 2 辉长岩LA-ICP-MS锆石U-Th-Pb同位素测年结果
Table 2. LA-ICP-MS zircon U-Th-Pb isotopic analyses of metagabbro
表 3 变辉长岩锆石Hf同位素组成
Table 3. Zircon Hf isotope compositions of metagabbro
-
[1] Wang H Z, Mo X X. An outline of the tectonic evolution of China[J]. Episodes, 1995, 18(12):6-16. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=4e237d110fb232f41af1847b6d4f050f
[2] 王惠初, 陆松年, 莫宣学, 等.柴达木盆地北缘早古生代碰撞造山系统[J].地质通报, 2005, 24(7):603-612. doi: 10.3969/j.issn.1671-2552.2005.07.003 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=200507123&flag=1
[3] 郭安林, 张国伟, 强娟, 等.青藏高原东北缘印支期宗务隆造山带[J].岩石学报, 2009, 25(1):1-12. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200901001
[4] 陆松年, 王惠初, 李怀坤, 等.柴达木盆地北缘"达肯大坂群"的再厘定[J].地质通报, 2002, 21(1):19-23. doi: 10.3969/j.issn.1671-2552.2002.01.004 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20020106&flag=1
[5] 朱小辉, 陈丹玲, 刘良, 等.柴北缘绿梁山地区早古生代弧后盆地型蛇绿岩的年代学、地球化学及大地构造意义[J].岩石学报, 2014, 30(3):822-834. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201403021
[6] 宋述光, 牛耀龄, 张立飞, 等.大陆造山运动:从大洋俯冲到大陆俯冲、碰撞、折返的时限——以北祁连山、柴北缘为例[J].岩石学报, 2009, 25(9):2067-2077. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200909003
[7] Zhang G B, Song S G, Zhang L F, et al. The subducted oceanic crust within continental-type UHP metamorphic belt in the North Qaidam, NW China:Evidence from petrology, geochemistry and geochronology[J]. Lithos, 2008, 104:99-118. doi: 10.1016/j.lithos.2007.12.001
[8] Zhang G B, Zhang L F, Christy A G. From oceanic subduction to continental collision:An overview of HP-UHP metamorphic rocks in the North Qaidam UHP belt, NW China[J]. J. Asian Earth Sci., 2013, 63:98-111. doi: 10.1016/j.jseaes.2012.07.014
[9] 宋述光, 张贵宾, 张聪, 等.大洋俯冲和大陆碰撞的动力学过程:北祁连-柴北缘高压-超高压变质带的岩石学制约[J].科学通报, 2013, 58(23):2240-2245. http://www.cnki.com.cn/Article/CJFDTotal-KXTB201323001.htm
[10] 郝国杰, 陆松年, 王惠初, 等.柴达木盆地北缘前泥盆纪构造格架及欧龙布鲁克古陆块地质演化[J].地学前缘, 2004, 11(3):115-122. doi: 10.3321/j.issn:1005-2321.2004.03.013
[11] 史仁灯, 杨经绥, 吴才来.柴北缘早古生代岛弧火山岩中埃达克质英安岩的发现及其地质意义[J].岩石矿物学杂志2003, (3):229-236. doi: 10.3969/j.issn.1000-6524.2003.03.004
[12] 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), 2008, 38(8):930-949. doi: 10.3321/j.issn:1006-9267.2008.08.002
[13] 高晓峰, 校培喜, 贾群子.滩间山群的重新厘定——来自柴达木盆地周缘玄武岩年代学和地球化学证据[J].地质学报, 2011, 85(9):1452-1463. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201109005
[14] 吴才来, 杨经绥, 许志琴, 等.柴达木盆地北缘古生代超高压带中花岗质岩浆作用[J].地质学报, 2004, (5):658-674. doi: 10.3321/j.issn:0001-5717.2004.05.010
[15] Wu C L, Wooden J L, Robinson P T, et al. Geochemistry and zircon SHRIMP U-Pb dating of granitoids from the west segment of the North Qaidam[J].Science in China D:Earth Sciences, 2009, 38(8):930-949. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-ed200911009
[16] 吴才来, 郜源红, 李兆丽, 等.都兰花岗岩锆石SHRIMP定年及柴北缘超高压带花岗岩年代学格架[J].中国科学:地球科学, 2014, 44(10):2142-2165. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd201410004
[17] Song S G, Su L, Li X H, et al. Tracing the 850Ma continental flood basalts from a piece of subducted continental crust in the North Qaidam UHPM belt, NW China[J]. Precambrian Research, 2010, 183, 805-816. doi: 10.1016/j.precamres.2010.09.008
[18] Zhang C, Zhang L, Herman V R, et al. Petrology and SHRIMP U-Pb dating of Xitieshan eclogite, North Qaidam UHP metamorphic belt, NW China[J]. Journal of Asian Earth Sciences, 2011, 42, 752-767. doi: 10.1016/j.jseaes.2011.04.002
[19] Zhang J X, Mattinson C G, Yu S Y, et al. U-Pb zircon geochronology of coesite-bearing eclogites from the southern Dulan area of the North Qaidam UHP terrane, northwestern China:spatially and temporally extensive UHP metamorphism during continental subduction[J]. Journal of metamorphic Geology, 2010, 28, 955-978. doi: 10.1111/j.1525-1314.2010.00901.x
[20] Song S G, Niu Y L, Su L, et al. Continental orogenesis from ocean subduction, continent collision/subduction, to orogen collapse, and orogen recycling:The example of the North Qaidam UHPM belt, NW China[J]. Earth-Science Reviews, 2014, 129:59-84. doi: 10.1016/j.earscirev.2013.11.010
[21] 彭渊, 马寅生, 刘成林, 等.东昆仑大干沟火山岩SHRIMP锆石U-Pb测年及其地质意义[J].地质通报, 2016, 35(213):356-363. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20160318&flag=1
[22] Walker G P L, Eyre P R. Dike compleses in American Samoa[J]. J. Volc. Geother. Res., 1995, 69:241-254. doi: 10.1016/0377-0273(95)00041-0
[23] Windley B F. The evolving continents(3rd ed)[M]. New York:John Wiley, 1995:1-526.
[24] Ernst R E, Buchan K L, Hamilton M A, et al. Integrated paleomagnetism and U-Pb geochronology of mafic dikes of the eastern Anabar Shield Region, Siberia:Implications for Mesoproterozoic Paleolatitude of siberia and Comparison with Laurentia[J]. The Journal of Geology, 2000, 108:381. doi: 10.1086/314413
[25] 邵济安, 张永北, 张履桥, 等.大同地区早古生代煌斑岩-碳酸岩岩墙群[J].岩石学报, 2003, 19(1):93-104. http://www.cnki.com.cn/Article/CJFDTotal-YSXB200301009.htm
[26] 杨经绥, 宋述光, 许志琴, 等.柴达木盆地北缘早古生代高压-超高压变质带中发现典型超高压矿物——柯石英[J].地质学报, 2001, 2:175-179. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200102005
[27] 查显锋, 辜平阳, 计文化, 等.欧龙布鲁克地块西段达肯大坂岩群物质组成及变形特征研究[J].地质科学, 2013, 4:1103-1114. doi: 10.3969/j.issn.0563-5020.2013.04.010
[28] Anderson T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192:59-79. doi: 10.1016/S0009-2541(02)00195-X
[29] Ludwig K R. 3.0-A geochronologycal toolkit for Microsoft Excel[J]. Berkeley Geochronology Certer, Special Publication, 2003(, 4):1-70.
[30] Chu N C, Taylor R N, Chavagnac V, et al. Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry:An evaluation of isobaric interference corrections[J]. Journal of Analytical Atomic Spectrometry, 2002, 17(12):1567-1574.
[31] Albarède F, Scherer E E, Blichert-Toft J, et al. γ-ray irradiation in the early Solar System and the conundrum of the 176Lu decay constant[J]. Geochimica et Cosmochimica Acta, 2006, 70(5):1261-1270. doi: 10.1016/j.gca.2005.09.027
[32] Bouvier A, Vervoort J D, Patchett P J. The Lu-Hf and Sm-Nd isotopic composition of CHUR:Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets[J]. Earth and Planetary Science Letters, 2008, 273(12):48-57. doi: 10.1016/j.epsl.2008.06.010
[33] Nowell G, Kempton P, Noble S, et al. High precision Hf isotope measurements of MORB and OIB by thermal ionization mass spectrometry:insights into the depleted mantle[J]. Chemical Geology, 1998, 149(3):211-233. doi: 10.1016/S0009-2541(98)00036-9
[34] 李文宣, 吴新国, 冯家麟.大同火山群玄武岩研究[J].河北地质学院学报, 1994, 6:547-555. http://www.cnki.com.cn/Article/CJFDTotal-HBDX199406005.htm
[35] 韩吟文, 马振东.地球化学[M].北京:地质出版社, 2003.
[36] 王立社, 李智明, 仇银江, 等.阿尔金奇克山东斜长角闪岩地球化学、年代学及其成因意义[J].地质学报, 2016, 4:739-751. doi: 10.3969/j.issn.0001-5717.2016.04.010
[37] Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and process[C]//Sauders A D, Norry M J. Magmatism in the Ocean Basins. Geological Society Special Publication, 1989, 42: 3l3-345.
[38] Hajash A J. Rare earth element abundances and distribution patterns in hydrothermally altered basalts:Experimental results[J]. Contributions to Mineralogy and petrology, 1984, 85(4):409-412. doi: 10.1007/BF01150297
[39] Becker H, Jochum K P, Carlson R W. Constraints from highpressure veins in eclogites on the composition of hydrous fluids in subduction zones[J]. Chemical Geology, 1999, 160(4):291-308. doi: 10.1016/S0009-2541(99)00104-7
[40] Escuder-Viruete J, Pérez-Estaún A, Weis D, et al. Geochemical characteristics of the Río Verde complex, central Hispaniola:Implications for the paleotectonic reconstruction of the Lower Cretaceous Caribbean island-arc[J]. Lithos, 2010, 114(12):168-185. doi: 10.1016/j.lithos.2009.08.007
[41] Ormerod D S, Hawkesworth C J, Rogers N W, et al. Tectonic and magmatic transition in the western Great Basin, USA[J]. Nature, 1988, 333(61716172):394-353.
[42] Saunders A D, Storey M, Kent R W, et al. Consequences of plume-lithosphere interactions[J]. Geological Society, London, Special Publications, 1992, 68(1):41-60. doi: 10.1144/GSL.SP.1992.068.01.04
[43] Bienvenu P, Bougault H, Joron J, et al. MORB alteration:Rare earth element/non-rare-earth hugromagmaphile element fractionation[J]. Chemical Geology, 1990, 82:1-14. doi: 10.1016/0009-2541(90)90070-N
[44] Rudnick R L, Gao S. Composition of the continental crust[C]//Turekian K K, Holland H D. Treatise on Geochemistry. Oxford: Pergamon, 2003: 1-64.
[45] 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, 32(2):185-220. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200702001
[46] 第五春荣, 孙勇, 王倩.华北克拉通地壳生长和演化, 来自现代河流碎屑锆石Hf同位素组成的启示[J].岩石学报, 2012, 28(11):3520-3530. http://d.old.wanfangdata.com.cn/Conference/7863094
[47] 王冬兵, 王立全, 尹福光, 等.滇西北金沙江古特提斯洋早期演化时限及其性质:竹林层状辉长岩锆石U-Pb年龄及Hf同位素约束[J].岩石学报, 2012, 28(5):1542-1550. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201205016
[48] 夏林圻, 夏祖春, 徐学义, 等.利用地球化学方法判别大陆玄武岩和岛弧玄武岩[J].岩石矿物学杂志, 2007, (1):77-89. doi: 10.3969/j.issn.1000-6524.2007.01.011
[49] Song S G, Su L, Li X H, et al. Grenville-age orogenesis in the Qaidam-Qilian block:The link between South China and Tarim[J]. Precambrian Research, 2012, 220:9-22. doi: 10.1016/j.precamres.2012.07.007
[50] 周宾, 郑有业, 许荣科, 等.青海柴达木山岩体LA-ICP-MS锆石U-Pb定年及Hf同位素特征[J].地质通报, 2013, 32(7):1027-1034. doi: 10.3969/j.issn.1671-2552.2013.07.008 http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20130708&flag=1
[51] 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. doi: 10.3969/j.issn.1000-0569.2007.08.008
[52] Wang M J, Song S G, Niu Y L, et al. Post-collisional magmatism:Consequences of UHPM terrane exhumation and orogen collapse, N. Qaidam UHPM belt, NW China[J]. Lithos, 2014, 210211:81-198. doi: 10.1016/j.lithos.2014.10.006
[53] 李睿华, 孙丰月, 李良, 等.青海牛鼻子梁镍矿勘查区闪长岩UPb年代学、地球化学及Hf同位素研究[J].地质学报, 2017, 91(10):2273-2284. doi: 10.3969/j.issn.0001-5717.2017.10.009
[54] 许志琴, 杨经绥, 李海兵, 等.造山的高原——青藏高原地体的拼合、碰撞造山及隆升机制[M].北京:地质出版社, 2007:1-458.
[55] 张贵山, 温汉捷, 裘愉卓.闽西晚中生代基性岩脉的地球化学研究[J].地球化学, 2004, (3):243-253. doi: 10.3321/j.issn:0379-1726.2004.03.003
① 辜平阳,董增产,陈锐明,等.青海阿尔金1:5万打柴沟(J46E005011、J46E005012、J46E005013、J46E006011、J46E006012、J46E006013)等6幅区调.2016.