新疆祁漫塔格花土沟地区中酸性侵入岩的年代学、地球化学特征及其地质意义

doi:10.19657/j.geoscience.1000-8527.2022.041

现代地质 ›› 2023, Vol. 37 ›› Issue (03): 599-612.DOI: 10.19657/j.geoscience.1000-8527.2022.041

• 岩石学与岩石地球化学 • 上一篇下一篇

新疆祁漫塔格花土沟地区中酸性侵入岩的年代学、地球化学特征及其地质意义

马德成¹(), 席振²^,³(), 高光明³, 李欢³

1.新疆维吾尔自治区有色地质勘查局七○一队, 新疆昌吉 831100
2.湖南城市学院市政与测绘工程学院, 湖南益阳 413000
3.中南大学地球科学与信息物理学院, 湖南长沙 410083

收稿日期:2022-02-10 修回日期:2023-04-05 出版日期:2023-06-10 发布日期:2023-07-20
通讯作者: 席振,男,博士,讲师,1986年出生,地球探测与信息技术专业,从事构造地质与遥感地质研究。Email: xizhen@hncu.edu.cn。
作者简介:马德成,男,高级工程师,1983年出生,矿产普查与勘探专业,从事区域地质与矿产勘查研究。Email:hjnh-2004@qq.com。
基金资助:
国家自然科学基金项目(40827002);国家自然科学基金项目(41204054);新疆维吾尔自治区中央返还两权价款项目(K15-1-LQ06)

Geochronology, Geochemistry and Geological Significance of the Huatugou Intermediate-acid Intrusions at Qimantag, Xinjiang

MA Decheng¹(), XI Zhen²^,³(), GAO Guangming³, LI Huan³

1. No.701 Geological Team, Xinjiang Nonferrous Geoexploration Bureau, Changji, Xinjiang 831100, China
2. School of Municipal and Geomatics Engineering, Hunan City University, Yiyang,Hunan 413000, China
3. School of Geosciences and Info-Physics, Central South University, Changsha, Hunan 410083, China

Received:2022-02-10 Revised:2023-04-05 Online:2023-06-10 Published:2023-07-20

摘要/Abstract

摘要：

东昆仑祁漫塔格志留纪到泥盆纪岩浆活动强烈,其形成与大洋岩石圈俯冲造山、碰撞-后碰撞造山活动有关。本文对东昆仑祁漫塔格花土沟地区花岗闪长岩开展锆石U-Pb年代学、全岩地球化学研究,探讨岩石成岩过程及构造背景。花岗闪长岩LA-ICP-MS锆石U-Pb定年结果为(396.5±4.6) Ma,为早—中泥盆世岩浆活动产物。全岩SiO₂含量为63.01%~74.70%,显示高K₂O(1.53%~4.01%)、Na₂O(2.16%~3.80%)和Al₂O₃(12.95%~14.48%)特征,Mg^#为17.01~61.23,属钙碱性-高钾钙碱性系列岩石。稀土元素球粒陨石标准化配分曲线呈中等倾斜的右倾平滑型曲线,具有负铕异常(δEu=0.48~0.72),微量元素蛛网图显示富集Rb、Th、La、Ce等大离子亲石元素和轻稀土元素,亏损Nb、Ta、Ba等高场强元素,属I型花岗岩。结合岩体成岩年龄、地球化学特征与区域构造演化,认为花岗闪长岩为造山带地壳物质特别是增生地壳物质的部分熔融,有幔源物质的混入,演化过程中经历了长石等矿物的结晶分离作用,形成于大陆碰撞造山末期向后碰撞转化阶段下的挤压向伸展过渡的构造环境。

关键词: I型花岗岩, 高钾钙碱性系列, 泥盆纪, 东昆仑造山带, 祁漫塔格

Abstract:

The Qimantag in East Kunlun orogen has strong magmatic activity from the Silurian to Devonian, and its formation is related to oceanic lithosphere subduction orogeny and collision-post-collision orogeny. In this paper, zircon U-Pb chronology and whole-rock major and trace element geochemistry are carried out on the Hua-tugou granodiorite in Qimantag, and the petrogenesis and tectonic background are discussed. LA-ICP-MS zircon U-Pb dating of the granodiorite is (396.5±4.6) Ma, which is the product of Early-Middle Devonian magmatic activity. The whole-rock SiO₂ content is 63.01%-74.70%, showing characteristics of high K₂O (1.53%-4.01%), Na₂O (2.16%-3.80%) and Al₂O₃ (12.95%-14.48%), Mg^# is 17.01-61.23, belonging to calc-alkaline and high-K calc-alkaline series. The chondrite-normalized REE patterns are moderately right-dipping and smooth, with negative Eu anomaly (δEu=0.48-0.72). Trace element spider diagram shows that the rocks are enriched in large ion lithophile elements (LILEs), such as Rb, Th, La, Ce and light rare earth elements (LREEs), and is depleted in Nb and Ta, Ba and other high field strength elements (HFSEs), belonging to I-type granite. Combined with the magmatic age, geochemical characteristics and regional tectonic evolution, we considered that the granodiorite is the partial melting product of orogenic crustal materials (especially accretionary crustal materials), mixing with some mantle-derived material, and experienced fractionation of feldspar and other minerals during the magma evolution. The tectonic regime may have been a compression-extension transition from syn-collisional to post-collisional setting.

Key words: I-type granite, high-K calc-alkaline, Devonian, East Kunlun orogen, Qimantag

中图分类号:

马德成, 席振, 高光明, 李欢. 新疆祁漫塔格花土沟地区中酸性侵入岩的年代学、地球化学特征及其地质意义[J]. 现代地质, 2023, 37(03): 599-612.

MA Decheng, XI Zhen, GAO Guangming, LI Huan. Geochronology, Geochemistry and Geological Significance of the Huatugou Intermediate-acid Intrusions at Qimantag, Xinjiang[J]. Geoscience, 2023, 37(03): 599-612.

图/表 12

参考文献 58

[1]	莫宣学, 罗照华, 邓晋福, 等. 东昆仑造山带花岗岩及地壳生长[J]. 高校地质学报, 2007, 13(3): 403-414.
[2]	钱兵, 高永宝, 李侃, 等. 新疆东昆仑于沟子地区与铁-稀有多金属成矿有关的碱性花岗岩地球化学、年代学及Hf同位素研究[J]. 岩石学报, 2015, 31(9): 2508-2520.
[3]	王松, 丰成友, 李世金, 等. 青海祁漫塔格卡尔却卡铜多金属矿区花岗闪长岩锆石SHRIMP U-Pb测年及其地质意义[J]. 中国地质, 2009, 36(1): 74-84.
[4]	姚磊. 青海祁漫塔格地区三叠纪成岩成矿作用及地球动力学背景[D]. 北京: 中国地质大学(北京), 2015.
[5]	YAO L, LÜ Z C, ZHAO C S, et al. Zircon U-Pb geochronological, trace element, and Hf isotopic constraints on the genesis of the Fe and Cu skarn deposits in the Qiman Tagh area, Qinghai Province, Eastern Kunlun Orogen, China[J]. Ore Geology Reviews, 2017, 91: 387-403. DOI URL
[6]	DONG Y P, HE D F, SUN S S, et al. Subduction and accretionary tectonics of the East Kunlun orogen, western segment of the Central China Orogenic System[J]. Earth-Science Reviews, 2018, 186: 231-261. DOI URL
[7]	YU M, DICK J M, FENG C Y, et al. The tectonic evolution of the East Kunlun Orogen, northern Tibetan Plateau:A critical review with an integrated geodynamic model[J]. Journal of Asian Earth Sciences, 2020, 191: 104168. DOI URL
[8]	于淼, 丰成友, 何书跃, 等. 祁漫塔格造山带: 青藏高原北部地壳演化窥探[J]. 地质学报, 2017, 91(4): 703-723.
[9]	WANG Q, ZHAO J, ZHANG C L, et al. Paleozoic post-collisional magmatism and high-temperature granulite-facies metamorphism coupling with lithospheric delamination of the East Kunlun Orogenic Belt, NW China[J]. Geoscience Frontiers, 2022, 13(1): 101271. DOI URL
[10]	DAI J G, WANG C S, HOURIGAN J, et al. Multi-stage tectono-magmatic events of the Eastern Kunlun Range, northern Tibet: Insights from U-Pb geochronology and (U-Th)/He thermochronology[J]. Tectonophysics, 2013, 599: 97-106. DOI URL
[11]	LI R B, PEI X Z, LI Z C, et al. Late Silurian to Early Devonian volcanics in the East Kunlun orogen, northern Tibetan Plateau: Record of postcollisional magmatism related to the evolution of the Proto-Tethys Ocean[J]. Journal of Geodynamics, 2020, 140: 101780. DOI URL
[12]	XIONG F H, MA C Q, JIANG H A, et al. Geochronology and geochemistry of Middle Devonian mafic dykes in the East Kunlun orogenic belt, northern Tibet Plateau: Implications for the transition from Prototethys to Paleotethys orogeny[J]. Geochemistry, 2014, 74(2): 225-235. DOI URL
[13]	DONG J L, SONG S G, SU L, et al. Early Devonian mafic ig-neous rocks in the East Kunlun Orogen, NW China: Implications for the transition from the Proto- to Paleo-Tethys oceans[J]. Lithos, 2020, 376/377: 105771. DOI URL
[14]	QIN Y, FENG Q, CHEN G, et al. Devonian post-orogenic extension-related volcano-sedimentary rocks in the northern margin of the Tibetan Plateau, NW China: Implications for the Paleozoic tectonic transition in the North Qaidam Orogen[J]. Journal of Asian Earth Sciences, 2018, 156: 145-166. DOI URL
[15]	王秉璋, 罗照华, 李怀毅, 等. 东昆仑祁漫塔格走廊域晚古生代—早中生代侵入岩岩石组合及时空格架[J]. 中国地质, 2009, 36(4): 769-782.
[16]	郝娜娜, 袁万明, 张爱奎, 等. 东昆仑祁漫塔格晚志留世—早泥盆世花岗岩: 年代学、地球化学及形成环境[J]. 地质论评, 2014, 60(1): 201-215.
[17]	LIU Y S, HU Z C, GAO S, et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257(1/2): 34-43. DOI URL
[18]	RICKWOOD P C. Boundary lines within petrologic diagrams which use oxides of major and minor elements[J]. Lithos, 1989, 22(4):247-263. DOI URL
[19]	PECCERILLO A, TAYLOR S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58: 63-81. DOI URL
[20]	陈静, 谢智勇, 李彬, 等. 东昆仑拉陵灶火地区泥盆纪侵入岩成因及其地质意义[J]. 矿物岩石, 2013, 33(2): 26-34.
[21]	王冠, 孙丰月, 李碧乐, 等. 东昆仑夏日哈木矿区早泥盆世正长花岗岩锆石U-Pb年代学、地球化学及其动力学意义[J]. 大地构造与成矿学, 2013, 37(4): 685-697.
[22]	郭通珍, 刘荣, 陈发彬, 等. 青海祁漫塔格山乌兰乌珠尔斑状正长花岗岩LA-MC-ICP MS锆石U-Pb定年及地质意义[J]. 地质通报, 2011, 30(8): 1203-1211.
[23]	高永宝, 李文渊, 钱兵, 等. 东昆仑野马泉铁矿相关花岗质岩体年代学、地球化学及Hf同位素特征[J]. 岩石学报, 2014, 30(6): 1647-1665.
[24]	MIDDLEMOST E A K. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994, 37(3/4): 215-224. DOI URL
[25]	WHALEN J B. Geochemistry of an Island-Arc Plutonic Suite: the Uasilau-Yau Yau intrusive complex, New Britain, P.N.G[J]. Journal of Petrology, 1985, 26(3): 603-632. DOI URL
[26]	MILLER C F, MCDOWELL S M, MAPES R W. Hot and cold granites? Implications of zircon saturation temperatures and pre-servation inheritance[J]. Geology, 2003, 31(6): 529-532. DOI URL
[27]	王川, 彭建堂, 徐接标, 等. 湘中白马山复式岩体成因及其成矿效应[J]. 岩石学报, 2021, 37(3): 805-829.
[28]	EBY G N. Chemical subdivision of the A-type granitoids: Petrogenetic and tectonic implications[J]. Geology, 1992, 20(7): 641-644. DOI URL
[29]	GAO P, ZHENG Y F, ZHAO Z F. Distinction between S-type and peraluminous I-type granites: Zircon versus whole-rock geochemistry[J]. Lithos, 2016, 258/259: 77-91. DOI URL
[30]	国显正, 栗亚芝, 贾群子, 等. 东昆仑五龙沟金多金属矿集区晚二叠世—三叠纪岩浆岩年代学、地球化学及其构造意义[J]. 岩石学报, 2018, 34(8): 2359-2379.
[31]	SUN S S, MCDONOUGH W F. Chemical and isotopic systema-tics of oceanic basalts: Implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989, 42(1):313-345. DOI URL
[32]	RUDNICK R L, GAO S. Composition of the continental crust[M]// Treatise on Geochemistry. Amesterdam: Elsevier, 2014: 1-51.
[33]	ZHOU H Z, ZHANG D H, WEI J H, et al. Petrogenesis of Late Triassic mafic enclaves and host granodiorite in the Eastern Kunlun Orogenic Belt, China: Implications for the reworking of juve-nile crust by delamination-induced asthenosphere upwelling[J]. Gondwana Research, 2020, 84: 52-70. DOI URL
[34]	CHAPPELL B W. Origin of infracrustal (I-type) granite magmas[J]. Transactions of the Royal Society of Edinburgh (Earth Sciences), 1988, 79:71-86.
[35]	吴福元, 李献华, 杨进辉, 等. 花岗岩成因研究的若干问题[J]. 岩石学报, 2007, 23(6):1217-1238.
[36]	WHALEN J B, CURRIE K L, CHAPPELL B W. A-type gra-nites: Geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy and Petrology, 1987, 95(4): 407-419. DOI URL
[37]	邓晋福, 刘翠, 冯艳芳, 等. 关于火成岩常用图解的正确使用: 讨论与建议[J]. 地质论评, 2015, 61(4): 717-734.
[38]	WEAVER B L. The origin of ocean island basalt end-member compositions: Trace element and isotopic constraints[J]. Earth and Planetary Science Letters, 1991, 104(2/3/4): 381-397. DOI URL
[39]	GAO P, ZHENG Y F, ZHAO Z F. Experimental melts from crustal rocks: A lithochemical constraint on granite petrogenesis[J]. Lithos, 2016, 266/267: 133-157. DOI URL
[40]	ALTHERR R, SIEBEL W. I-type plutonism in a continental back-arc setting: Miocene granitoids and monzonites from the central Aegean Sea, Greece[J]. Contributions to Mineralogy and Petrology, 2002, 143(4): 397-415. DOI URL
[41]	PATIÑO DOUCE A E. What do experiments tell us about the re-lative contributions of crust and mantle to the origin of granitic magmas?[J]. Geological Society, London, Special Publications, 1999, 168: 55-75. DOI URL
[42]	高永宝. 东昆仑祁漫塔格地区中酸性侵入岩浆活动与成矿作用[D]. 西安: 长安大学, 2013.
[43]	王盘喜, 郭峰, 王振宁. 东昆仑祁漫塔格鸭子沟地区花岗岩类岩石年代学、地球化学及地质意义[J]. 现代地质, 2020, 34(5): 987-1000.
[44]	LI J Y, QIAN Y, LI H R, et al. The Late Ordovician granitoids in the East Kunlun Orogenic Belt, Northwestern China: Petroge-nesis and constraints for tectonic evolution of the Proto-Tethys Ocean[J]. International Journal of Earth Sciences, 2020, 109(4): 1439-1461. DOI
[45]	HUANG H, NIU Y L, NOWELL G, et al. Geochemical constraints on the petrogenesis of granitoids in the East Kunlun Orogenic belt, northern Tibetan Plateau: Implications for continental crust growth through syn-collisional felsic magmatism[J]. Chemical Geology, 2014, 370: 1-18. DOI URL
[46]	CHEN J J, FU L B, WEI J H, et al. Proto-Tethys magmatic evolution along northern Gondwana: Insights from Late Silurian-Middle Devonian A-type magmatism, East Kunlun Orogen, Northern Tibetan Plateau, China[J]. Lithos, 2020, 356/357: 105304. DOI URL
[47]	LI W, NEUBAUER F, LIU Y J, et al. Paleozoic evolution of the Qimantagh magmatic arcs, Eastern Kunlun Mountains: Constraints from zircon dating of granitoids and modern river sands[J]. Journal of Asian Earth Sciences, 2013, 77: 183-202. DOI URL
[48]	ZHOU B, DONG Y P, ZHANG F F, et al. Geochemistry and zircon U-Pb geochronology of granitoids in the East Kunlun Orogenic Belt, northern Tibetan Plateau: Origin and tectonic implications[J]. Journal of Asian Earth Sciences, 2016, 130: 265-281. DOI URL
[49]	CHEN J, WANG B Z, LU H F, et al. Geochronology and geochemistry of Early Devonian intrusions in the Qimantagh area, Northwest China: Evidence for post-collisional slab break-off[J]. International Geology Review, 2018, 60(4): 479-495. DOI URL
[50]	SONG S G, BI H Z, QI S S, et al. HP-UHP metamorphic belt in the East Kunlun orogen: Final closure of the Proto-Tethys Ocean and formation of the Pan-North-China Continent[J]. Journal of Petrology, 2018, 59(11): 2043-2060. DOI URL
[51]	国显正, 贾群子, 李金超, 等. 东昆仑高压变质带榴辉岩年代学、地球化学及其地质意义[J]. 地球科学, 2018, 43(12): 4300-4318.
[52]	孟繁聪, 崔美慧, 贾丽辉, 等. 东昆仑造山带早古生代的大陆碰撞: 来自榴辉岩原岩性质的证据[J]. 岩石学报, 2015, 31(12): 3581-3594.
[53]	刘彬, 马昌前, 蒋红安, 等. 东昆仑早古生代洋壳俯冲与碰撞造山作用的转换:来自胡晓钦镁铁质岩石的证据[J]. 岩石学报, 2013, 29(6): 2093-2106.
[54]	谌宏伟, 罗照华, 莫宣学, 等. 东昆仑喀雅克登塔格杂岩体的SHRIMP年龄及其地质意义[J]. 岩石矿物学杂志, 2006, 25(1): 25-32.
[55]	PEARCE J A, HARRIS N B W, TINDLE A G. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984, 25(4): 956-983. DOI URL
[56]	HARRIS N B W, PEARCE J A, TINDLE A G. Geochemical characteristics of collision-zone magmatism[J]. Geological So-ciety, London, Special Publications, 1986, 19(1): 67-81.
[57]	BARBARIN B. A review of the relationships between granitoid types, their origins and their geodynamic environments[J]. Lithos, 1999, 46(3): 605-626. DOI URL
[58]	吴泰然. 花岗岩及其形成的大地构造环境[J]. 北京大学学报(自然科学版), 1995, 31(3): 358-365.

测点	Th (10^-6)	U (10^-6)	Th/U	同位素比值			年龄(Ma)
测点	Th (10^-6)	U (10^-6)	Th/U	²⁰⁷Pb /²⁰⁶Pb(1σ)	²⁰⁷Pb /²³⁵U(1σ)	²⁰⁶Pb /²³⁸U(1σ)	²⁰⁷Pb/²⁰⁶Pb(1σ)	²⁰⁷Pb/²³⁵U(1σ)	²⁰⁶Pb/²³⁸U(1σ)
1	376	516	0.73	0.0553(0.0018)	0.4732(0.0155)	0.0617(0.0016)	433(72)	393(11)	386(10)
2	314	523	0.6	0.0552(0.0018)	0.4703(0.0157)	0.0614(0.0017)	420(77)	391(11)	384(10)
4	134	270	0.5	0.0563(0.0020)	0.4897(0.0173)	0.0629(0.0017)	465(80)	405(12)	393(10)
5	195	393	0.5	0.0581(0.0019)	0.5049(0.0157)	0.0630(0.0016)	532(75)	415(11)	394(10)
6	268	397	0.67	0.0538(0.0018)	0.4689(0.0158)	0.0628(0.0017)	365(68)	390(11)	393(10)
8	152	297	0.51	0.0555(0.0019)	0.4790(0.0170)	0.0624(0.0017)	435(78)	397(12)	390(10)
9	174	336	0.52	0.0539(0.0019)	0.4732(0.0165)	0.0637(0.0017)	365(80)	393(11)	398(10)
10	168	283	0.59	0.0531(0.0019)	0.4617(0.0169)	0.0630(0.0017)	332(79)	385(12)	394(10)
11	216	402	0.54	0.0564(0.0019)	0.4710(0.0159)	0.0605(0.0016)	478(74)	392(11)	378(10)
14	231	366	0.63	0.0558(0.0018)	0.4692(0.0154)	0.0610(0.0017)	443(77)	391(11)	382(10)
15	230	424	0.54	0.0543(0.0018)	0.4759(0.0162)	0.0635(0.0018)	383(74)	395(11)	397(11)
17	223	361	0.62	0.0544(0.0020)	0.4949(0.0214)	0.0665(0.0026)	387(88)	408(15)	415(16)
18	114	262	0.44	0.0531(0.0020)	0.4696(0.0171)	0.0650(0.0020)	332(79)	391(12)	406(12)
19	200	386	0.52	0.0540(0.0017)	0.4785(0.0156)	0.0642(0.0017)	372(72)	397(11)	401(11)
20	249	435	0.57	0.0534(0.0017)	0.4717(0.0151)	0.0642(0.0017)	346(42)	392(10)	401(10)
21	51	188	0.27	0.0569(0.0021)	0.5257(0.0197)	0.0669(0.0018)	487(49)	429(13)	418(11)
22	225	397	0.57	0.0549(0.0018)	0.4922(0.0163)	0.0650(0.0017)	406(74)	406(11)	406(11)
23	129	266	0.49	0.0565(0.0019)	0.4944(0.0170)	0.0633(0.0017)	472(76)	408(12)	396(10)
25	144	286	0.51	0.0584(0.0020)	0.5322(0.0178)	0.0662(0.0018)	543(69)	433(12)	413(11)
26	259	463	0.56	0.0531(0.0018)	0.4786(0.0159)	0.0651(0.0017)	345(76)	397(11)	406(10)
27	326	445	0.73	0.0541(0.0018)	0.4757(0.016)	0.0636(0.0017)	376(76)	395(11)	397(10)

测点	Th (10^-6)	U (10^-6)	Th/U	同位素比值			年龄(Ma)
测点	Th (10^-6)	U (10^-6)	Th/U	²⁰⁷Pb /²⁰⁶Pb(1σ)	²⁰⁷Pb /²³⁵U(1σ)	²⁰⁶Pb /²³⁸U(1σ)	²⁰⁷Pb/²⁰⁶Pb(1σ)	²⁰⁷Pb/²³⁵U(1σ)	²⁰⁶Pb/²³⁸U(1σ)
1	376	516	0.73	0.0553(0.0018)	0.4732(0.0155)	0.0617(0.0016)	433(72)	393(11)	386(10)
2	314	523	0.6	0.0552(0.0018)	0.4703(0.0157)	0.0614(0.0017)	420(77)	391(11)	384(10)
4	134	270	0.5	0.0563(0.0020)	0.4897(0.0173)	0.0629(0.0017)	465(80)	405(12)	393(10)
5	195	393	0.5	0.0581(0.0019)	0.5049(0.0157)	0.0630(0.0016)	532(75)	415(11)	394(10)
6	268	397	0.67	0.0538(0.0018)	0.4689(0.0158)	0.0628(0.0017)	365(68)	390(11)	393(10)
8	152	297	0.51	0.0555(0.0019)	0.4790(0.0170)	0.0624(0.0017)	435(78)	397(12)	390(10)
9	174	336	0.52	0.0539(0.0019)	0.4732(0.0165)	0.0637(0.0017)	365(80)	393(11)	398(10)
10	168	283	0.59	0.0531(0.0019)	0.4617(0.0169)	0.0630(0.0017)	332(79)	385(12)	394(10)
11	216	402	0.54	0.0564(0.0019)	0.4710(0.0159)	0.0605(0.0016)	478(74)	392(11)	378(10)
14	231	366	0.63	0.0558(0.0018)	0.4692(0.0154)	0.0610(0.0017)	443(77)	391(11)	382(10)
15	230	424	0.54	0.0543(0.0018)	0.4759(0.0162)	0.0635(0.0018)	383(74)	395(11)	397(11)
17	223	361	0.62	0.0544(0.0020)	0.4949(0.0214)	0.0665(0.0026)	387(88)	408(15)	415(16)
18	114	262	0.44	0.0531(0.0020)	0.4696(0.0171)	0.0650(0.0020)	332(79)	391(12)	406(12)
19	200	386	0.52	0.0540(0.0017)	0.4785(0.0156)	0.0642(0.0017)	372(72)	397(11)	401(11)
20	249	435	0.57	0.0534(0.0017)	0.4717(0.0151)	0.0642(0.0017)	346(42)	392(10)	401(10)
21	51	188	0.27	0.0569(0.0021)	0.5257(0.0197)	0.0669(0.0018)	487(49)	429(13)	418(11)
22	225	397	0.57	0.0549(0.0018)	0.4922(0.0163)	0.0650(0.0017)	406(74)	406(11)	406(11)
23	129	266	0.49	0.0565(0.0019)	0.4944(0.0170)	0.0633(0.0017)	472(76)	408(12)	396(10)
25	144	286	0.51	0.0584(0.0020)	0.5322(0.0178)	0.0662(0.0018)	543(69)	433(12)	413(11)
26	259	463	0.56	0.0531(0.0018)	0.4786(0.0159)	0.0651(0.0017)	345(76)	397(11)	406(10)
27	326	445	0.73	0.0541(0.0018)	0.4757(0.016)	0.0636(0.0017)	376(76)	395(11)	397(10)

样品	SiO₂	Fe₂O₃	FeO	Al₂O₃	CaO	MgO	K₂O	Na₂O	MnO	TiO₂	P₂O₅	烧失量	总量
H2-10	74.7	0.31	1.80	13.45	1.01	0.24	3.67	3.80	0.05	0.08	0.05	0.98	100.13
H4-4	63.01	1.11	4.24	14.48	4.05	2.04	4.01	2.16	0.09	0.53	0.19	3.85	99.75
H4-6	65.47	0.68	3.35	12.95	3.59	3.51	2.53	2.98	0.07	0.63	0.23	3.88	99.87
H2-1	65.10	0.04	5.01	15.27	4.39	2.33	0.98	3.07	0.09	0.50	0.10	2.90	99.78
H2-2	67.32	0.90	5.19	13.86	2.78	2.49	1.53	3.62	0.11	0.63	0.13	2.09	100.65
样品	Na₂O+K₂O	A/CNK	A/NK	Mg^#	La	Ce	Pr	Nd	Sm	Eu	Gd	Tb	Dy
H2-10	7.47	1.11	1.31	17.01	10.7	18.7	2.35	8.1	1.79	0.38	1.59	0.33	2.22
H4-4	6.17	0.95	1.83	40.97	35.3	58.4	7.13	25.4	4.07	0.91	3.53	0.58	3.28
H4-6	5.51	0.91	1.69	61.23	35.8	65.7	9.18	36.8	7.34	1.56	6.38	1.16	6.67
H2-1	6.05	0.92	1.60	46.10	15.0	31.0	4.81	21.5	5.23	0.84	5.46	1.14	7.55
H2-2	5.15	1.09	1.82	42.52	41.7	73.8	9.56	37.2	6.78	1.37	6.17	1.09	6.32
样品	Ho	Er	Tm	Yb	Lu	Y	Rb	Ba	Th	K	Sr	P	Hf
H2-10	0.49	1.41	0.25	1.68	0.26	17.3	109.8	533.6	5.0	30135.8	74.34	200	3.28
H4-4	0.63	1.79	0.28	1.76	0.27	33.3	59.0	1026.5	19.6	32764.6	350.20	810	2.43
H4-6	1.34	5.62	0.62	3.88	0.59	43.3	125.6	1224.2	14.4	32457.2	373.70	1180	3.88
H2-1	1.60	4.73	0.72	4.25	0.61	48.9	21.5	274.6	4.5	9176.4	308.20	500	0.86
H2-2	1.27	4.66	0.59	3.73	0.56	26.8	121.1	478.5	6.4	12963.8	285.30	540	8.69
样品	Zr	Ti	Nb	Ta	Sc	Cr	ΣREE	(La/Yb)_N		(Ce/Yb)_N		δEu	δCe
H2-10	75.9	400.7	6.4	0.62	1.51	10.5	50.25	4.31		2.89		0.67	0.87
H4-4	182.8	3439.0	14.8	0.89	5.72	44.2	143.33	13.57		8.61		0.72	0.85
H4-6	162.3	4478.0	25.8	1.61	17.62	290.0	182.64	6.24		4.39		0.68	0.87
H2-1	142.4	3913.0	8.5	0.47	10.52	30.7	104.44	2.39		1.89		0.48	0.89
H2-2	143.5	4283.0	20.5	1.54	12.79	22.9	194.80	7.54		5.12		0.64	0.87

样品	SiO₂	Fe₂O₃	FeO	Al₂O₃	CaO	MgO	K₂O	Na₂O	MnO	TiO₂	P₂O₅	烧失量	总量
H2-10	74.7	0.31	1.80	13.45	1.01	0.24	3.67	3.80	0.05	0.08	0.05	0.98	100.13
H4-4	63.01	1.11	4.24	14.48	4.05	2.04	4.01	2.16	0.09	0.53	0.19	3.85	99.75
H4-6	65.47	0.68	3.35	12.95	3.59	3.51	2.53	2.98	0.07	0.63	0.23	3.88	99.87
H2-1	65.10	0.04	5.01	15.27	4.39	2.33	0.98	3.07	0.09	0.50	0.10	2.90	99.78
H2-2	67.32	0.90	5.19	13.86	2.78	2.49	1.53	3.62	0.11	0.63	0.13	2.09	100.65
样品	Na₂O+K₂O	A/CNK	A/NK	Mg^#	La	Ce	Pr	Nd	Sm	Eu	Gd	Tb	Dy
H2-10	7.47	1.11	1.31	17.01	10.7	18.7	2.35	8.1	1.79	0.38	1.59	0.33	2.22
H4-4	6.17	0.95	1.83	40.97	35.3	58.4	7.13	25.4	4.07	0.91	3.53	0.58	3.28
H4-6	5.51	0.91	1.69	61.23	35.8	65.7	9.18	36.8	7.34	1.56	6.38	1.16	6.67
H2-1	6.05	0.92	1.60	46.10	15.0	31.0	4.81	21.5	5.23	0.84	5.46	1.14	7.55
H2-2	5.15	1.09	1.82	42.52	41.7	73.8	9.56	37.2	6.78	1.37	6.17	1.09	6.32
样品	Ho	Er	Tm	Yb	Lu	Y	Rb	Ba	Th	K	Sr	P	Hf
H2-10	0.49	1.41	0.25	1.68	0.26	17.3	109.8	533.6	5.0	30135.8	74.34	200	3.28
H4-4	0.63	1.79	0.28	1.76	0.27	33.3	59.0	1026.5	19.6	32764.6	350.20	810	2.43
H4-6	1.34	5.62	0.62	3.88	0.59	43.3	125.6	1224.2	14.4	32457.2	373.70	1180	3.88
H2-1	1.60	4.73	0.72	4.25	0.61	48.9	21.5	274.6	4.5	9176.4	308.20	500	0.86
H2-2	1.27	4.66	0.59	3.73	0.56	26.8	121.1	478.5	6.4	12963.8	285.30	540	8.69
样品	Zr	Ti	Nb	Ta	Sc	Cr	ΣREE	(La/Yb)_N		(Ce/Yb)_N		δEu	δCe
H2-10	75.9	400.7	6.4	0.62	1.51	10.5	50.25	4.31		2.89		0.67	0.87
H4-4	182.8	3439.0	14.8	0.89	5.72	44.2	143.33	13.57		8.61		0.72	0.85
H4-6	162.3	4478.0	25.8	1.61	17.62	290.0	182.64	6.24		4.39		0.68	0.87
H2-1	142.4	3913.0	8.5	0.47	10.52	30.7	104.44	2.39		1.89		0.48	0.89
H2-2	143.5	4283.0	20.5	1.54	12.79	22.9	194.80	7.54		5.12		0.64	0.87

新疆祁漫塔格花土沟地区中酸性侵入岩的年代学、地球化学特征及其地质意义

Geochronology, Geochemistry and Geological Significance of the Huatugou Intermediate-acid Intrusions at Qimantag, Xinjiang

RichHTML

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

图/表 12

参考文献 58

相关文章 15

编辑推荐

Metrics

本文评价

[1]	陈耀新, 刘文恒, 王凯兴, 刘晓东, 孙立强, 尹冬华. 甘肃青山堡中牌细粒花岗岩成因与构造环境:锆石U-Pb年龄和全岩元素组成制约[J]. 现代地质, 2024, 38(01): 169-182.
[2]	王建华, 朱幼安, 李强. 藏南亚东帕里地区早泥盆世沉积及古生物特征[J]. 现代地质, 2024, 38(01): 224-229.
[3]	程天赦, 杨文静, 滕超, 张学斌, 杨欣杰, 来林, 吴荣泽, 周长红. 内蒙古西乌旗早泥盆世I型石英闪长岩的发现及其地质意义[J]. 现代地质, 2023, 37(06): 1624-1633.
[4]	张国宾, 孔金贵, 吴子杰, 冯玥, 何云龙, 陈兴凯. 蒙古—鄂霍次克洋早侏罗世构造演化:来自大兴安岭北段新立屯地区花岗岩的证据[J]. 现代地质, 2023, 37(02): 404-418.
[5]	唐名鹰, 华磊, 丁正江, 董振昆, 王炜晓, 翟孝志, 王汝杰, 郑成龙. 东昆仑祁漫塔格地区乌腊德石墨矿床地球化学特征及成矿机制研究[J]. 现代地质, 2022, 36(06): 1475-1485.
[6]	王玉平, 吴文彬, 刘永俊, 李海洋, 王晓亮, 李超. 辽东岫岩地区晚侏罗世侵入岩的年代学、地球化学特征及地质意义[J]. 现代地质, 2021, 35(04): 955-967.
[7]	杨硕, 刘阁, 靳刘圆, 郑海峰. 东准噶尔卡拉麦里松喀尔苏岩体花岗岩年代学、地球化学特征及其构造意义[J]. 现代地质, 2021, 35(02): 492-503.
[8]	王盘喜, 郭峰, 王振宁. 东昆仑祁漫塔格鸭子沟地区花岗岩类岩石年代学、地球化学及地质意义[J]. 现代地质, 2020, 34(05): 987-1000.
[9]	李阅薇, 王成善, 李国彪, 徐星, 马文恩, 李兴鹏, 吕昶良, 吕贝贝, 张文苑, 韩丹丹. 广西龙江泥盆纪苔藓虫的发现及其地质意义[J]. 现代地质, 2020, 34(04): 745-756.
[10]	袁晓博, 方念乔, 董海龙. 海南岛高峰、保城地区花岗岩年代学、地球化学特征及构造意义[J]. 现代地质, 2019, 33(01): 85-97.
[11]	张耀玲, 倪晋宇, 沈燕绪, 王超群, 高万里, 胡道功. 柴北缘牦牛山组火山岩锆石U-Pb年龄及其地质意义[J]. 现代地质, 2018, 32(02): 329-334.
[12]	武若晨, 顾雪祥, 章永梅, 何格, 康继祖, 余福承, 冯李强, 徐劲驰. 东昆仑造山带早古生代—早中生代构造演化的沉积地球化学记录[J]. 现代地质, 2017, 31(04): 716-733.
[13]	鲁艳明, 专少鹏, 所承逊, 殷敏. 内蒙古阿鲁科尔沁地区晚侏罗世侵入岩年代学、地球化学特征及成矿潜力[J]. 现代地质, 2016, 30(5): 981-993.
[14]	王永文，颜丹平，刘红旭，潘澄雨，陈峰，孟云飞，丁波，刘涛. 西天山伊犁地块北缘桦木沟高分异I型花岗岩年代学、地球化学及其构造意义[J]. 现代地质, 2015, 29(3): 529-541.
[15]	宋忠宝，张雨莲，贾群子，陈向阳，江磊，李东生，何书跃，李金超，杨涛，全守村，栗亚芝，张晓飞. 东昆仑祁漫塔格地区野马泉深部的华力西期花岗闪长岩U-Pb年龄及其意义[J]. 现代地质, 2014, 28(6): 1161-1169.