地球科学进展 ›› 2018, Vol. 33 ›› Issue (2): 189 -205. doi: 10.11867/j.issn.1001-8166.2018.02.0189

研究论文 上一篇    下一篇

北祁连西段熬油沟组玄武岩地球化学特征及构造意义
刘懿馨 1( ), 侯克选 2, 沙鑫 1, 马蓁 1, 王金荣 1, *( )   
  1. 1.兰州大学地质科学与矿产资源学院 甘肃省西部矿产资源重点实验室(兰州大学),甘肃 兰州 730000
    2.河北省众联能源环保科技有限公司,河北 石家庄 050000
  • 收稿日期:2017-07-20 修回日期:2017-12-18 出版日期:2018-02-20
  • 通讯作者: 王金荣 E-mail:liuyx16@lzu.edu.cn;jrwang@lzu.edu.cn
  • 基金资助:
    甘肃省矿产资源补偿费项目“甘肃省肃南卡瓦铁矿综合研究”(编号:甘财建【2014】99号);中央高校基本科研业务费(编号:lzujbky-2016-197)资助

Geochemical Characteristics and Tectonic Significance of Aoyougou Group Basalts in Western North Qilian

Yixin Liu 1( ), Kexuan Hou 2, Xin Sha 1, Zhen Ma 1, Jinrong Wang 1, *   

  1. 1.School of Earth Sciences, Lanzhou University, Key Laboratory of Mineral Resources in Western China, Lanzhou 730000, China
    2.Zhong-Lian Environmental Protection and Scientific Technology Co. Ltd., Shijiazhuang Hebei 050000,China
  • Received:2017-07-20 Revised:2017-12-18 Online:2018-02-20 Published:2018-04-02
  • Contact: Jinrong Wang E-mail:liuyx16@lzu.edu.cn;jrwang@lzu.edu.cn
  • About author:

    First author:Liu Yixin(1988-),female,Qin’an City,Gansu Province,Ph.D student. Research areas include petrotectonics.E-mail:liuyx16@lzu.edu.cn

  • Supported by:
    Project supported by Gansu Mineral Resources Compensation Project “Comprehensive study of the Kawa iron ore mine in Sunan, Gansu” (Gansu Financial Construction [2014] No.99);Basic Research Service Fee of Central University (lzujbky-2016-197)

北祁连造山带是一典型的板块缝合带,其中镶嵌着众多大小不一的由前震旦系变质岩系组成微陆壳残块,为解析北祁连前造山构造过程提供了重要的研究载体。北祁连西段卡瓦—祁青一带分布有较为完整的中元古界长城系朱龙关群熬油沟组火山岩—碎屑岩—碳酸盐岩建造。岩石地球化学研究表明,熬油沟组玄武岩主量元素含量变化较为稳定,具高K2O(4.27%~6.07%),TFe2O3(10.49%~13.01%),TiO2(1.96%~2.90%)以及中等的MgO(5.37%~6.71%,Mg# 48~51),CaO(2.57%~ 5.51%),为钾玄碱性玄武岩。岩石Cr和Ni含量随着Mg#降低而减小、CaO与CaO/Al2O3呈正相关,明显富集轻稀土元素(LREE)和大离子亲石元素(LILE),轻微正Eu异常,高含量的高场强元素(Nb,Ta,Ti),以及元素对Gd/Yb(2.5~3.0),Zr/Y(8.6~10.2),Ta/Yb(0.96~1.23),Ti/Yb(5 074~6 021),Zr/Yb(81~97),Ce/Nb(1.87),Zr/Nb(6.41)值均揭示了熬油沟组玄武岩具有洋岛玄武岩(OIB)地球化学特征。结合区域地质背景研究表明,熬油沟组碱性玄武岩源于类似于OIB的深部富集地幔,在岩浆作用过程中发生过橄榄石和单斜辉石的分离结晶作用以及一定程度的大陆地壳物质的混染作用,形成于大陆裂谷背景,并认为其是对中元古代Columbia超大陆裂解的响应,进一步为中元古代华北克拉通裂解与Columbia超大陆裂解事件的关系提供了重要的岩石学证据。

The North Qilian orogenic belt is a typical plate suture zone, which is studded with numerous different sizes of fragments of micro-continental crust consisting of pre-Sinian metamorphic rocks and the North Qilian orogenic belt provides important study carrier for studying the pre-orogenic tectonic process of the North Qilian. The relatively complete volcanic-clastic-carbonate rocks formation of Zhulongguan Group, Changchengian System, Mesoproterozoic are distributed in the Kawa-Qiqing area, Western North Qilian orogenic belt. Geochemical characteristics of the Aoyougou Group basalts in the North Qilian indicated that the contents of major element were relatively stable, high K2O contents(4.27%~6.07%), TFe2O3(10.49%~13.01%),TiO2(1.96%~2.90%)and middle MgO(5.37%~6.71%,Mg# 48~51), CaO(2.57%~5.51%)content. Thus, the Aoyougou Group basalts belong to potassium alkaline basalt. The contents of Cr and Ni of the basalts decreased with the decreasing of Mg#, and there was a positive correlation between CaO and CaO/Al2O3, Furthermore, the Eu anomaly of samples was slightly negative, high contents of high field strength elements (HFSE, Nb, Ta, Ti), and the ratios of Gd/Yb(2.5~3.0), Zr/Y(8.6~10.2), Ta/Yb(0.96~1.23), Ti/Yb(5 074~6 021), Zr/Yb(81~97), Ce/Nb(1.87), Zr/Nb(6.41)indicated that the Aoyougou Group basalts had obvious OIB-type magmatic affinity. In combination with the regional geological background, the study results showed that Aoyougou Group alkaline basalt generated from deep enrichment mantle similar to the source of OIB, with fractional crystallization of olivine and monoclinic pyroxene and a certain degree of contamination of continental crust in the process of magmatism, formed in the background of continental rift, might response to the Proterozoic Columbia supercontinent rifting, which further provides important petrological evidences for the relationship between North China Craton rifting events and Columbia supercontinent rifting during Proterozoic.

中图分类号: 

图1 研究区地质简图(据参考文献[15,46]修改)
(a)北祁连西段卡瓦地区大地构造纲要图(据参考文献[15]修改);(b)卡瓦一带地层分布图(据参考文献[46]修改).1.中新生界;2.古生界;3.第四系;4. 青白口系;5.长城纪桦树沟组;6.长城纪熬油沟组;7.古元古代北大河岩群;8.基性—超基性岩;9.中酸性侵入岩体;10.地质界线;11. 图2 剖面位置(采样位置见 图2 )
Fig.1 Geology sketch of the research area(modified after references[15,46])
(a)Structure outline map of Western North Qilian (modified after reference [15]). (b) Stratigraphic map of Kawa region (modified after reference [46]).1:Middle Cenozoic. 2:Paleozoic. 3:Quaternary. 4:Qingbaikou System. 5:Huashugou Group, Changcheng Period. 6:Aoyougou Group, Changcheng Period. 7:Paleoproterozoic Beidahe terrain. 8:Mafic-ultramafic rocks. 9:Neutral-acid intrusion. 10:Geology boundary. 11:Samples and geological section location of Fig.2
图2 熬油沟组—桦树沟组地质剖面图及采样点(剖面位置见 图1 )
Fig.2 Aoyougou-Huashugou Group geological sectionmap and sample position (the position of section map are shown in Fig.1 )
图3 玄武岩及其镜下特征(正交5X)
Cpx.单斜辉石;Pl.斜长石
Fig.3 Basalts with its microscopic photasl (perpendicular 5X)
Cpx:Clinopyroxene. Pl:Plagioclase
图4 火山岩分类图
(a)火山岩TAS分类图(据参考文献[50]修改); (b)Nb/Y-Zr/TiO 2图解(据参考文献[51]修改)
Fig.4 Classification diagrams for volcanic rocks
(a)TAS classification of volcanic rocks(modified after reference [50] ). (b)Nb/Y-Zr/TiO 2 diagram (modified after reference [51])
图5 熬油沟组玄武岩SiO 2-K 2O图解 [ 50 ]
Fig.5 SiO 2-K 2O diagram for Aoyougou Group Basalts [ 50 ]
图6 熬油沟组玄武岩REE球粒陨石标准化配分图(标准化值来自参考文献[52])
Fig.6 Chondrite-normalized rare earth element patterns diagram of Aoyougou Group Basalts (normalized value from reference[52])
表1 北祁连西段熬油沟组玄武岩主微量元素(%)、微量元素(×10 -6)分析结果
Table 1 The contents of major (%) and trace elements (×10 -6)of Aoyougou Group Basalts in the Western North Qilian
样号 14-KW-H30 14-KW-H31 14-KW-H32 14-KW-H33 14-KW-H34 14-KW-H35 14-KW-H36
SiO2 44.86 44.56 45.64 45.56 48.07 46.78 46.64
Al2O3 15.64 16.15 15.72 15.16 15.47 15.71 15.59
TiO2 2.90 2.43 2.50 2.30 1.96 2.55 2.39
TFe2O3 13.01 10.99 11.30 10.58 10.49 11.53 11.04
MnO 0.65 0.85 0.72 0.46 0.46 0.63 0.55
MgO 6.71 6.35 5.68 5.99 5.37 5.80 5.75
CaO 2.57 2.99 3.22 5.51 3.56 2.74 3.67
Na2O 1.91 1.08 1.72 1.61 1.60 2.07 2.57
K2O 4.33 6.07 5.36 5.13 6.01 4.95 4.27
P2O5 0.49 0.56 0.54 0.51 0.47 0.56 0.52
LOI 6.41 7.27 7.01 6.40 6.05 6.12 6.59
Total 99.48 99.30 99.41 99.21 99.51 99.44 99.58
Mg# 48 51 48 50 48 48 48
Ba 1 280 3 810 2 380 1 790 2 040 1 890 1 290
Rb 42.80 67.20 83.00 68.40 86.80 64.60 40.00
Cs 2.99 3.49 3.32 2.89 3.18 3.21 2.75
Th 3.12 3.19 3.65 3.13 3.37 3.71 3.30
U 0.80 0.73 0.78 0.94 0.77 0.80 0.79
Nb 43.90 36.20 36.90 42.00 36.90 37.90 39.00
Ta 3.55 2.75 2.78 3.02 2.86 2.88 2.98
Pb 4.27 3.81 4.03 3.19 3.81 6.15 3.08
Sr 211.00 275.00 312.00 307.00 250.00 257.00 236.00
Zr 272.00 236.00 236.00 264.00 238.00 248.00 252.00
Hf 6.81 5.59 5.96 6.27 5.80 6.04 6.19
P 2 140 2 446 2 358 2 227 2 052 2 446 2 271
Cr 246.00 165.00 181.00 223.00 123.00 170.00 207.00
Ni 134.00 96.10 93.30 107.00 54.80 94.90 91.10
Co 50.20 39.60 38.80 37.40 28.00 45.00 34.60
V 274.00 229.00 220.00 204.00 169.00 236.00 213.00
Sc 24.90 20.60 21.80 15.50 16.70 24.20 20.60
Ga 24.00 21.20 21.20 22.30 20.70 21.50 21.30
La 27.90 29.00 36.90 35.80 33.90 36.80 31.10
Ce 61.60 63.80 81.20 79.40 75.90 78.20 67.20
Pr 7.85 8.53 10.40 9.82 9.25 10.20 8.28
Nd 31.20 35.60 42.80 40.20 37.10 41.20 32.40
Sm 7.43 8.24 9.15 8.69 8.47 9.40 7.46
Eu 2.54 3.30 3.33 3.10 2.96 3.28 2.66
Gd 7.23 7.56 8.76 8.17 7.62 8.75 7.07
Tb 1.18 1.19 1.38 1.29 1.23 1.45 1.11
Dy 6.58 6.44 7.30 6.53 6.36 7.39 5.96
Ho 1.23 1.20 1.34 1.23 1.22 1.35 1.11
Er 3.24 3.06 3.42 3.06 3.12 3.56 2.90
Tm 0.46 0.42 0.47 0.43 0.44 0.48 0.42
Yb 2.89 2.60 2.91 2.72 2.75 2.96 2.60
Lu 0.43 0.38 0.42 0.38 0.40 0.41 0.38
Y 30.10 27.50 31.00 26.40 25.50 31.80 24.80
∑REEEE 191.86 198.82 240.78 227.22 216.22 237.23 195.45
LREE 138.52 148.47 183.78 177.01 167.58 179.08 149.10
HREE 53.34 50.35 57.00 50.21 48.64 58.15 46.35
LREE/HREE 2.60 2.95 3.22 3.53 3.45 3.08 3.22
δEu 1.02 1.12 1.06 1.05 1.05 1.04 1.05
δCe 0.86 0.86 0.87 0.87 0.88 0.87 0.87
(La/Yb)N 6.92 8.00 9.10 9.44 8.84 8.92 8.58
Nb /U 54.88 49.59 47.31 44.68 47.92 47.38 49.37
图7 熬油沟组玄武岩微量元素原始地幔标准化蛛网图(标准化值来自参考文献[52])
Fig.7 Primitive-mantle-normalised multi-element diagram of Aoyougou Group Basalts (normalized value from reference [52])
图8 玄武岩Zr/Nb-Ce/Y变异图 [ 54 ]
Fig.8 Zr/Nb-Ce/Y variation diagram of basalts [ 54 ]
图9 玄武岩Nb/Yb-TiO 2/Yb变异图 [ 55 ]
Fig.9 Nb/Yb-TiO 2/Yb variation diagram of basalts [ 55 ]
图10 玄武岩源区判别图
(a)熬油沟组玄武岩Zr-Nb图;(b)Zr-Y图解 [ 56 ];直线为原始地幔
Fig.10 Resource discrimination diagrams of basalts
(a)Zr-Nb. (b)Zr-Y diagram of Aoyougou Group basalts [ 56 ]. Straight line represents the PM
图11 岩石部分熔融演化图
(a)熬油沟组玄武岩La/Yb-Sm/Yb [ 60 ];(b) La/Sm-Sm/Yb图解 [ 61 ]
Fig.11 Partial melting evolution diagram
(a)La/Yb-Sm/Yb diagram [ 60 ]. (b) La/Sm-Sm/Yb [ 61 ] diagram of Aoyougou Group basalts
图12 Nb/La-Nb/Th变异图(据参考文献[55]修改)
Fig.12 Nb/La-Nb/Th variation diagram(modified after reference[55])
图13 熬油沟组玄武岩构造背景判别图
(a)玄武岩Th/Yb-Ta/Yb [ 65 ];(b)Hf/3-Th-Ta [ 66 ];(c)Zr-Zr/Y [ 67 ];(d)Ti/100-Zr-Y*3 [ 68 ]
Fig.13 Tectonic setting discrimination diagrams for Aoyougou Groups Basalts
(a)Th/Yb-Ta/Yb diagram [ 65 ]. (b)Hf/3-Th-Ta diagram [ 66 ]. (c)Zr-Zr/Y diagram [ 67 ]. (d)Ti/100-Zr-Y*3 diagram [ 68 ]
图14 熬油沟组玄武岩构造背景判别图
(a)玄武岩MgO-Al 2O 3-TFeO [ 67 ];(b) Ce/Nb-Th/Nb构造判别图 [ 12 ];PM.原始地幔;DMM.亏损地幔端员;N-MORB.N型洋中脊玄武岩;E-MORB.E型洋中脊玄武岩;OIB.洋岛玄武岩;BC.平均大陆壳;UCC.大陆上地壳;GLOSS.全球俯冲沉积物组成;Iceland plume.冰岛地幔柱;ECFB.峨眉山大陆溢流玄武岩
Fig.14 Tectonic setting discrimination diagrams for Aoyougou Groups basalts
(a) MgO-Al 2O 3-TFeO diagram [ 67 ]. (b) Ce/Nb-Th/Nb diagram [ 12 ]. PM: Primitive Mantle.DMM: Depleted mantle. N-MORB: Normal mid-ocean ridge basalt. E-MORB:Enriched mid-ocean ridge basalt. OIB: Oceanic island basalt.BC:Average continental crust. UCC:Upper continental crust. GLOSS:Global subducted sediments. ECFB: Emei Mountain continental flood basalt
[1] Feng Yimin,He Shiping,Yan Jun.The discovery and geological significance of the sheeted dyke complex rocks within the Early-Middle Ordovician ophiolite in the middle of the Northern Qilian Mountains[J].Geological Review,1994,40(3):252-264.
[冯益民,何世平,阎军.祁连山中段早中奥陶世蛇绿岩中席状岩墙杂岩的发现及其地质意义[J].地质论评,1994,40(3):252-264.]
[2] Feng Yimin,Wu Hanquan.The tectonic evolution in the Northern Qilian Mountains and its adjacent areas[J].Northwest Geoscience,1992,13(2):61-74.
[冯益民,吴汉泉.北祁连山及其邻区古生代以来的大地构造演化初探[J]. 西北地质科学, 1992, 13(2): 61-74.]
URL    
[3] Feng Yimin,He Shiping.Geological and geochemical research of ophiolite in Northern Qilian Mountain[J]. Acta Petrologica Sinica,1995,11(Suppl.1):125-146.
[冯益民,何世平.北祁连山蛇绿岩地质和地球化学研究[J].岩石学报,1995,11(增刊1):125-146.]
[4] Feng Yimin.Qilian orogenic belt research overview:History,present situation and prospects[J]. Advances in Earth Science,1997,12(4):307-314.
[冯益民. 祁连造山带研究概况——历史,现状及展望[J]. 地球科学进展, 1997, 12(4): 307-314.]
URL    
[5] Zuo Guochao,Wu Hanquan.Early Paleozoic two-way subduction,collision orogeny model analysis of the Middle North Qilian[J]. Advances in Earth Science,1997,12(4):215-232.
[左国朝,吴汉泉.北祁连中段路段早古生代双向俯冲—碰撞造山模式剖析[J].地球科学进展,1997,12(4):215-232.]
[6] Zhang Qi,Sun Xiaomeng,Zhou Dejin, et al.The characteristics,forming environment and its tectonic significance of the North Qilian ophiolites[J].Advances in Earth Science,1997,12(4):366-393.
[张旗,孙晓猛,周德进,等.北祁连蛇绿岩特征、形成环境及其构造意义[J].地球科学进展,1997,12(4): 366-393.]
doi: 10.11867/j.issn.1001-8166.1997.04.0366     URL    
[7] Zhang Qi,Wang Yueming.The diversity of mafic-super maifc rocks in Qilian Mountain region[J]. Advances in Earth Science,1997,12(4):324-330.
[张旗,王岳明.祁连山地区镁铁—超镁铁岩的多样性[J]. 地球科学进展,1997,12(4):324-330.]
[8] Zhang Qi,Zhou Guoqing.Chinese Ophiolite[M].Beijing:Science Press,2001.
[张旗,周国庆.中国蛇绿岩[M].北京:科学出版社,2001.]
[9] Xia Linxi,Xia Zuchun.Certainty about the nature of the Archean continent overflow basalt formation in west section of North of Qilian Mountain[J]. Science in China (Series D),2000,30(1):1-8.
[夏林圻,夏祖春.北祁连山西段元古宙大陆溢流玄武岩性质的确定[J].中国科学:D辑,2000,30(1):1-8.]
doi: 10.3321/j.issn:1006-9267.2000.01.001     URL    
[10] Song Shuguang.Tectonic evolution of the North Qilian Mountain subduction complex belt[J]. Advances in Earth Science,1997,12(4):351-365.
[宋述光. 北祁连山俯冲杂岩带的构造演化[J].地球科学进展, 1997, 12(4): 351-365.]
[11] Song Shuguang,Zhang Lifei, Niu Yaoling, et al.Zircon SHRIMP date and the tectonic significance of eclogite in North Qilian Mountain[J]. Chinese Science Bulletin,2004,49(6):592-595.
[宋述光,张立飞,牛耀龄,等.北祁连山榴辉岩锆石SHRIMP定年及其构造意义[J].科学通报,2004,49(6):592-595.]
doi: 10.3321/j.issn:0023-074X.2004.06.017     URL    
[12] Song S G,Zhang L F,Niu Y L.Ultra-deep origin of garnet peridotite from the North Qaidam ultrahigh-pressure belt, Northern Tibetan Plateau, NW China[J].American Mineralogist,2004,89:1 330-1 336.
doi: 10.2138/am-2004-8-922     URL    
[13] Song S G, Su L, Niu L, et al.Lai, CH4 inclusions in orogenic harzburgite: Evidence for reduced slab fluids and implication for redox melting in mantle wedge[J].Geochimica et Cosmochimica Acta,2009,73(6):1 737-1 754.
doi: 10.1016/j.gca.2008.12.008     URL    
[14] Song S G,Niu Y L,Zhang L,et al.Tectonic evolution of early Paleozoic HP metamorphic rocks in the North Qilian Mountains, NW China: New perspectives[J].Journal of Asian Earth Sciences,2009,35(3):334-353.
doi: 10.1016/j.jseaes.2008.11.005     URL    
[15] Song S G,Niu Y L,Su L,et al.Tectonics of the North Qilian orogen,NW China[J].Gondwana Research,2013,23(4):1 378-1 401.
doi: 10.1016/j.gr.2012.02.004     URL    
[16] Zuo Guochao, Liu Yike,Zhang Chong.Tectono-stratigraphic charateristics of continent crustal remnants in central-western section of the North Qilian Orogen[J].Chinese Journal of Geology, 2002, 37(3):302-312.
[左国朝,刘义科,张崇. 北祁连造山带中—西段陆壳残块群的构造—地层特征[J]. 地质科学, 2002,37(3):302-312.]
doi: 10.3321/j.issn:0563-5020.2002.03.006     URL    
[17] Xu Zhiqin, Xu Huifen,Zhang Jianxin,et al.Zoulang Nanshan Caledonian subduction complex in the Northern Qilian Mountains and its dynamics[J]. Acta Geologica Sinica,1994,68(1):1-15.
[许志琴,徐惠芬,张建新,等.北祁连走廊南山加里东俯冲杂岩增生地体及其动力学[J].地质学报,1994,68(1):1-15.]
URL    
[18] Hou Rongna,Wang Shuhua,Zhang Xiang,et al.Geochemical characteristics and tectonic significance of the granotoids in the western section of the Mid-Qilian[J]. Advances in Earth Science,2015,30(9): 1 034-1 049.
[侯荣娜,王淑华,张翔,等.中祁连西段花岗岩类的地球化学特征及构造意义[J].地球科学进展,2015,30(9):1 034-1 049.]
doi: 10.11867/j.issn.1001-8166.2015.09.1034     URL    
[19] Zhang Jianxin,Xu Zhiqin.North qilian middle caledonian dive hyperplasia complex/volcanic arc belt and its deformation characteristics[J]. Acta Geoscientica Sinica,1995,16(2):153-163.
[张建新,许志琴. 北祁连中段加里东俯冲—增生杂岩/火山弧带及其变形特征[J].地球学报,1995,16(2):153-163.]
[20] Yang Jingsui,Song Shuguang,Xu Zhiqin.Early Paleozoic in northern Qaidam basin shearing section at high pressure metamorphic belt were found in a typical ultrahigh pressure minerals:coesite[J]. Acta Geologica Sinica,2001,75(2):175-179.
[杨经绥,宋述光,许志琴.柴北缘早古生代高压—超高压变质带中发现典型的超高压矿物——柯石英[J].地质学报, 2001,75(2):175-179.]
[21] Wang Jinrong,Guo Yuansheng,Zhai Xinwei,et al.Gansu Baiyin mines field:Early-Middle Cambrian volcanic tectonic environment[J].Geological Journal of China Universities,2003,9(1) :89-98.
[王金荣,郭原生,翟新伟,等.甘肃白银厂矿田早—中寒武世火山岩形成的构造环境[J].高校地质学报,2003,9(1): 89-98.]
doi: 10.3969/j.issn.1006-7493.2003.01.011     URL    
[22] Wang Jinrong,Dong Ningfang,Chang Huajin,et al.Ductile shear zone volume loss and composition variation of Xiaotie Mountain Baiyinchan Gansu[J]. Journal of Lanzhou University (Natural Sciences),2005, 41(6):1-5.
[王金荣,董宁芳,常华进,等.甘肃白银厂小铁山韧性剪切带体积亏损与成分变异[J].兰州大学学报:自然科学版,2005,41(6):1-5.]
[23] Wang Jinrong,Wu Chunjun,Cai Zhenghong,et al.Early Paleozoic high-Mg adakite from Yindongliang in eastern section of the North Qilian:Implications for geodynamics and Cu-Au mineralization[J]. Acta Petrologica Sinica,2006,22(11):2 655-2 664.
[王金荣,吴春俊,蔡郑红,等.北祁连山东段银洞粱早古生代高镁银洞粱埃达克岩:大陆动力学及成矿意义[J]. 岩石学报,2006,22(11):2 655-2 664.]
[24] Hu Wanlong,Hou Rongna,Zhang Cheng,et al.Geochemical characteristics and tectonic implications of basaltic porphyry in the western segment of the central Qilian Mountains[J].Journal of Lanzhou University (Natural Sciences),2016,52(3):287-294.
[胡万龙,侯荣娜,张铖,等.中祁连西段玄武玢岩地球化学特征及其构造意义[J].兰州大学学报:自然科学版,2016,52(3):287-294.]
[25] Hu Wanlong,Jia Zhilei,Wang Jinrong,et al.Geochronology and geochemistry characteristics of the granites from the Huashigou area,South Qilian and their tectonic significance[J].Geological Journal of China Universities,2016,22(2):242-253.
[胡万龙,贾志磊,王金荣,等. 南祁连化石沟花岗岩年代学、地球化学特征及其构造意义[J]. 高校地质学报,2016,22(2):242-253.]
[26] Chen N S,Gong S L,Sun M,et al.Precambrian evolution of the Quanji Block,northeastern margin of Tibet:Insights from zircon U-Pb and Lu-Hf isotope compositions[J].Journal of Asian Earth Sciences,2009, 35:367-376.
doi: 10.1016/j.jseaes.2008.10.004     URL    
[27] Zhang Z C,Zhou M F,Robinson P T,et al.SHRIMP dating of the Aoyougou ophiolite in the west sector of the north Qilian Mountains and its geological significance[J].Acta Petrologica Sinica,2001,17:222-226.
doi: 10.1016/S0037-0738(00)00182-2     URL    
[28] Fu Guomin,Su Jianping,Hu Nenggao,et al.The geochemical characteristics and tectonic setting of Beidahe Group amphibolites of the Paleoproterozoic of the western Qilian Mountain[J].Geology in China, 2006, 22(12):2 910-2 922.
[付国民,苏建平,胡能高,等.祁连山西段古元古代北大河岩群中斜长角闪岩的地球化学特征及构造背景[J].中国地质,2005,32(4):541-547.]
[29] Zhang Hongfei,Chen Yuelong,Xu Wangchun, et al.The origin and tectonic significances of Yinzhi period granitoid in Qinghai Gonghe Basin[J]. Acta Petrologica Sinica,2006,22(12):2 910-2 922.
[张宏飞,陈岳龙, 徐旺春,等.青海共和盆地周缘印支期花岗岩类的成因及其构造意义[J].岩石学报,2006,22(12): 2 910-2 922.]
doi: 10.3321/j.issn:1000-0569.2006.12.009     URL    
[30] Guo Jinjing,Lu Songnian.China Neoproterozoic continental collage with Rodinia supercontinent[J].Geological Journal of China Universities,1999,5(2):29-37.
[郭进京,陆松年.中国新元古代大陆拼合与Rodinia超大陆[J].高校地质学报,1999,5(2):29-37.]
[31] Guo Jinjing,Zhang Guowei,Lu Songnian,et al.Discussion on the stratigraphic framework of the Proterozoic basement in the Eastern Middle Qililian block[J].China Regional Geology,1999,2(4): 379-396.
[郭进京,张国伟,陆松年,等.中祁连地块东段元古宙基底地层格架讨论[J].中国区域地质, 1999,2(4):379-396.]
doi: 10.3969/j.issn.1671-2552.1999.04.007     URL    
[32] Guo Jinjing,Zhao Fengqing,Li Huaikun.Geological significance of the Jinning period collision type granite in the Eastern Middle Qilian[J].Acta Geoscientica Sinica,1999,20(1):10-15.
[郭进京,赵凤清,李怀坤.中祁连东段晋宁期碰撞型花岗岩及其地质意义[J].地球学报,1999,20(1):10-15.]
doi: 10.3321/j.issn:1006-3021.1999.01.002     URL    
[33] Guo Jinjing,Zhao Fengqing,Li Huaikun,et al.The new evidence and geological significance of Huangyuan Group in the Eastern Middle Qilian[J].China Regional Geology,2000,6(1):27-32.
[郭进京,赵凤清,李怀坤,等.中祁连东段湟源群的年代学新证据及其地质意义[J].中国区域地质,2000,6(1): 27-32.]
doi: 10.3969/j.issn.1671-2552.2000.01.005     URL    
[34] Gao Xiaofeng,Li Wenyuan,Ye Meifang, et al.Geochemical characteristics and tectonic significance of Hualong Group amphibolites in the Eastern Middle Qilian[J]. Acta Petrologica et Mineralogica,2010,29(5):507-515.
[高晓峰,李文渊,叶美芳, 等.中祁连东段化隆群中斜长角闪岩地球化学特征及构造意义[J].岩石矿物学杂志,2010,29(5):507-515.]
doi: 10.3969/j.issn.1000-6524.2010.05.006     URL    
[35] Xia Linxi,Xia Zuchun,Xu Xueyi.The Origin of Marine Volcanic Rocks in the Northern Qilian Mountains[M].Beijing: Beijing Geology Press,1996.
[夏林圻,夏祖春,徐学义.北祁连山海相火山岩岩石成因[M].北京:地质出版社,1996.]
[36] Feng Beizhan,Wang Xiaowei,Zeng Junjie, et al.The nature of Paleoproterozoic continental rift volcanic rocks in the western North Qilian[J].Gansu Geology,2005,14(1):15-20.
[冯备战,王晓伟,曾俊杰,等.北祁连西段古元古代大陆裂谷火山岩性质的确定[J].甘肃地质学报,2005,14(1):15-20.]
[37] Wang Zhongliang.The Disintegration and Its Geological Significance of Tuolai Rock Mass in Rimucheer, Western North Qilian[D].Beijing:China University of Geosciences (Beijing),2013.
[王忠良. 中祁连西段上日木策尔地区托赖岩群的解体及其地质意义[D].北京:中国地质大学 (北京),2013.]
[38] Xu Xiaochun,Yue Shucang.The diagenesis mechanism of the Changcheng Group volcanic rock in the Northern Qililian[J].Journal of Hefei University of Technology(Natural Science),1997,20(1):28-33.
[徐晓春, 岳书仓. 北祁连长城系火山岩的成岩作用机制[J].合肥工业大学学报:自然科学版,1997,20(1): 28-33.]
[39] Mao Jingwen,Yang Jianmin,Zhang Zhaochong,et al.The dating and geological significance of single zircon of the Precambrian strata in the Western North Qilian[J].Chinese Science Bulletin,1997,42(13): 1 414-1 417.
[毛景文,杨建民,张招崇,等.北祁连山西段前寒武纪地层单颗粒锆石测年及其地质意义[J].科学通报,1997,42(13):1 414-1 417.]
[40] Zhang Zhaochong,Mao Jingwen.The geochemical characteristics and tectonic setting of the Proterozoic metamorphic volcanic rocks in the Western North Qilian[J].Journal of Mineralogy and Petrology,1998,18(4): 22-30.
[张招崇,毛景文.北祁连山西段早元古代变质火山岩的地球化学特征及其构造背景[J].矿物岩石, 1998,18(4):22-30.]
doi: 10.1038/sj.cr.7290029     URL    
[41] Zhang Zhaochong,Zhou Meifu,Robinson P T,et al.SHRIMP dating of the Aoyougou ophiolite in the west sector of the North Qilian Mountains and its geological significance[J]. Acta Petrologica Sinica,2001, 17(2):222-226
[张招崇,周美付, Robinson P T,等.北祁连山西段熬油沟蛇绿岩 SHRIMP 分析结果及其地质意义[J].岩石学报,2001,17(2):222-226.]
doi: 10.3321/j.issn:1000-0569.2001.02.006     URL    
[42] Xia Xiaohong,Sun Nan,Song Shuguang,et al.Age and tectonic setting of the Aoyougou-Erzhihaladaban ophiolite in the Western North Qilian Mountains,NW China[J].Acta Scientiarum Naturalium Univeisitatis Pekinensis,2012,48(5):757-769.
[夏小洪,孙楠,宋述光,等.北祁连西段熬油沟二只哈拉达坂蛇绿岩的形成环境和时代[J].北京大学学报:自然科学版,2012,48(5):757-769.]
[43] Xiang Zhenqun,Lu Songnian,Li Huaikun, et al.SHRIMP U-Pb zircon age of gabbro in Aoyougou in the western segment of the North Qilian Mountains,China and its geological implications[J].Geological Bulletin of China,2007,26(12):1 686-1 691.
[相振群,陆松年,李怀坤,等.北祁连西段熬油沟辉长岩的锆石Shrimp U-Pb年龄及地质意义[J].地质通报,2007,26(12):1 686-1 691.]
[44] Sha Xin.Study on the Diagenesis and Tectonic Implications of Mafic-ultramafic Rocks in the Western Sector of The Northern Qilianshan[D]. Lanzhou:Lanzhou University,2017.
[沙鑫. 北祁连西段镁铁质—超镁铁质岩的成因与构造意义的研究[D].兰州:兰州大学,2017.]
[45] Feng Yimin.Allochthones along the west section of the North Qilian Orogenic Belt[J]. Geological Review, 1998, 44(4):365-371.
[冯益民. 北祁连造山带西段的外来移置体[J]. 地质论评, 1998, 44(4):365-371.]
[46] Qi Ruirong,Chen Shiqiang,Hu Xiaochun.The exploration practice of Jingtieshan iron ore deposit in the Western North Qilian, Gansu:An example of mining breakthrough in the rich area of Kawa iron ore[J].Gansu Geology,2015,24(1):11-18.
[齐瑞荣,陈世强,胡小春.甘肃北祁连西段镜铁山铁矿外围勘查实践——以卡瓦铁矿富集区找矿突破为例[J].甘肃地质, 2015,24(1):11-18.]
URL    
[47] Xu Xiaochun,Yue Shucang,Liu Yin,et al.The era and petrochemical characteristics of Zhulongguan Group volcanic rocks in Zoulang Mountian,Gansu[J].Anhui Geology,1996,6(4):1-6.
[徐晓春,岳书仓,刘因,等.甘肃走廊南山朱龙关群的时代及其火山岩的岩石化学特征[J].安徽地质,1996,6(4):1-6.]
URL    
[48] Yu Boda.New understanding of Changcheng Period stratigraphic division,Gansu[J].Gansu Geology, 1997,6(1):1-15.
[俞伯达. 关于甘肃长城纪地层划分的新认识:甘肃地质[J],1997,6(1):1-15.]
[49] Govindaraju K.Compilation of working values and sample description for 383 geostandards[J].Geostandards Newsletter,1994,18(Suppl.1):1-158.
doi: 10.1046/j.1365-2494.1998.53202081.x-i1     URL    
[50] Le Maitre R W B,Dudek P,Keller A,et al. A Classification of Igneous Rocks and Glossary of Terms:Recommendations of the International Union of Geological Sciences,Subcommission on the Systematics of Igneous Rocks[M].London:International Union of Geological Sciences,1989.
[51] Winchester J A,Floyd P A.Geochemical magma type discrimination:Application to altered and metarnorphosed basic igneous rocks[J]. Earth and Planetary Science Letters,1976,28:459-469.
doi: 10.1016/0012-821X(76)90207-7     URL    
[52] Sun S S,Mcdonough W F.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[J].Geological Society London Special Publications,1989,42(1):313-345.
doi: 10.1144/GSL.SP.1989.042.01.19     URL    
[53] Wilson M.Igneous Petrogenesis:A Global Tectonic Approach[M].London:Unwin Hyman,1989.
[54] Goncuoglu M C,Sayit K,Tekin U K.Oceanization of the northern Neotethys:Geochemical evidence from ophiolitic melange basalts within the Izmir-Ankara suture belt, NW Turkey[J].Lithos,2010,116:175-187.
doi: 10.1016/j.lithos.2010.01.007     URL    
[55] Pearce J A.Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust[J]. Lithos,2008,100:14-48.
doi: 10.1016/j.lithos.2007.06.016     URL    
[56] Roex A P L,Dick H J B,Erlank A J,et al. Geochemistry,mineralogy and petrogenesis of lavas erupted along the Southwest Indian ridge between the bouvet triple junction and 11 degrees east[J].Journal of Petrology,1983,24(3):267-318.
doi: 10.1093/petrology/24.3.267     URL    
[57] DePaolo D J,Bryce J G,Dodson A,et al. Isotopic evolution of Mauna Loa and the chemical structure of the Hawaiian plume[J].Geochemistry, Geophysics, Geosystems, 2001,2(7):223-235.
doi: 10.1029/2000GC000139     URL    
[58] Hawkesworth C,Scherstén A.Mantle plumes and geochemistry[J].Chemical Geology,2007,241(3):319-331.
doi: 10.1016/j.chemgeo.2007.01.018     URL    
[59] Xu Y G,Ma J L,Frey F A,et al.Role of lithosphere-asthenosphere interaction in the genesis of Quaternary alkali and tholeiitic basalts from Datong,western North China Craton[J].Chemical Geology,2005,224(4):247-271.
doi: 10.1016/j.chemgeo.2005.08.004     URL    
[60] Zhu Yusheng,Hou Guangshun,Yang Jinhui.The origin and genesis of the Cenozoic basalts in Hebi: Evidence from geochemistry and Sr-Nd-Hf isotope[J].Acta Petrologica Sinica,2012, 28(12):4 064-4 076.
[朱昱升, 侯广顺, 杨进辉.鹤壁新生代玄武岩源区及成因:地球化学和 Sr-Nd-Hf 同位素证据[J].岩石学报,2012,28(12):4 064-4 076.]
URL    
[61] Dilek Y,Furnes H.Ophiolite genesis and global tectonics:Geochemical and tectonic fingerprinting of ancient oceanic lithosphere[J].Geological Society of America Bulletin,2011,123(3/4):387-411.
doi: 10.1130/B30446.1     URL    
[62] Rudnick R L,Fountain D M.Nature and composition of the continental crust:A lower crustal perspective[J].Reviews of Geophysics,1995,33(3):267-310.
doi: 10.1029/95RG01302     URL    
[63] Wang Jian,Li Jianping,Wang Jianghai,et al.The geology implication of inclusion of the Cenozoicshoshonite series in Jianchuan-Dali region[J]. Acta Mineralogica Sinica,2002,22(2):113-125.
[王建,李建平,王江海,等.滇西剑川—大理地区新生代钾玄岩系中深源包体的地质意义[J].矿物学报,2002, 22(2):113-125.]
[64] Condie K C.Geochemical changes in baslts and andesites across the Archean-Proterozoic boundary:Identification and significance[J].Lithos,1989,23(1):1-18.
doi: 10.1016/0024-4937(89)90020-0     URL    
[65] Rudnick R L,Fountain D M.Nature and composition of the continental crust: A lower crustal perspective[J].Reviews of Geophysics,1995,33(3):267-310.
doi: 10.1029/95RG01302     URL    
[66] Wood D A.The application of a Th,Hf,Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary Volcanic Province[J].Earth and Planetary Science Letters,1980,50(1):11-30.
doi: 10.1016/0012-821X(80)90116-8     URL    
[67] Pearce J A,Norry M J.Petrogenetic implications of Ti,Zr,Y,and Nb variations in volcanic rocks[J].Contributions to Mineralogy & Petrology,1979,69(1):33-47.
doi: 10.1007/BF00375192     URL    
[68] Pearce J A,Cann J R.Tectonic setting of basic volcanic rocks determined using trace element analyses[J].Earth and Planetary Science Letters,1973,19(2):290-300.
doi: 10.1016/0012-821X(73)90129-5     URL    
[69] Sun Shuqin,Zhang Chengjiang,Zhao Songjiang.The trace elements determination of intra-plate tectonic setting[J].Geotectonica et Metallogenia,2007,31(1):104-109.
[孙书勤,张成江,赵松江.大陆板内构造环境的微量元素判别[J].大地构造与成矿学,2007, 31(1):104-109.]
[70] Xiong Lijuan.The Tectonics Evolution and Collage of the Western North Proto-Tethys[D]. Qingdao:Ocean University of China,2014.
[熊莉娟. 原特提斯北界西段构造演化与拼合方式[D].青岛:中国海洋大学,2014.]
[71] Rogers J J W,Santosh M. Configuration of Columbia,a Mesoproterozoic Supercontinent[J].Gondwana Research,2002,5(1):5-22.
doi: 10.1016/S1342-937X(05)70883-2     URL    
[72] Lu Songnian,Yang Chunliang,Li Huaikun,et al.Northern China and Colombia supercontinent[J].Geoscience Frontiers,2002,9(4):225-233.
[陆松年,杨春亮,李怀坤,等.华北古大陆与哥伦比亚超大陆[J].地学前缘,2002,9(4):225-233.]
doi: 10.3321/j.issn:1005-2321.2002.04.002     URL    
[73] Lu Songnian,Li Huaikun,Xiang Zhenqun.A review on the research progress of isotope geochronology during the Paleoproterozoic,China[J].Geology in China,2010, 37(4):1 002-1 013.
[陆松年,李怀坤, 相振群.中国中元古代同位素地质年代学研究进展述评[J].中国地质,2010,37(4):1 002-1 013.]
doi: 10.3969/j.issn.1000-3657.2010.04.015     URL    
[74] Chen Nengsong,Wang Qinyan,Chen Qiang,et al.The preliminary discussion on the relationship between composition and metamorphism of the Qaidam and Olongbluk continental block basement and the evolution of ancient continent in West China[J].Geoscience Frontiers,2007,14(1):43-55.
[陈能松,王勤燕, 陈强,等.柴达木和欧龙布鲁克陆块基底的组成和变质作用及中国中西部古大陆演化关系初探[J].地学前缘,2007,14(1):43-55.]
doi: 10.3321/j.issn:1005-2321.2007.01.004     URL    
[75] Tang Dongjie,Shi Xiaoying,Liu Dianbo,et al.Termianl Paleoproterozoic ooidal ironstone from North China: A sedimentary response to the initial breakup of Columbia supercontinen[J].Earth Science—Journal of China University of Geosciences, 2015,40(2):290-304.
[汤冬杰,史晓颖,刘典波,等.华北古元古代末鲕铁岩:Columbia 超大陆裂解初期的沉积响应[J].地球科学——中国地质大学学报,2015,40(2):290-304.]
doi: 10.3799/dqkx.2015.022     URL    
[76] Wu Hailin,Zhu Wenbin,Shu Liangshu,et al.The record of the Columbia supercontinent polymerization in the North Tarim Craton[J].Geological Journal of China Universities,2012,18(4):686-700.
[吴海林,朱文斌,舒良树,等.Columbia 超大陆聚合事件在塔里木克拉通北缘的记录[J].高校地质学报,2012,18(4):686-700.]
URL    
[77] Xu Huiru,Yang Zhenyu,Zhu Rixiang.Paleo-position of the North China Craton within Supercontinent Columbia[C].Chinese Geophysics Proceedings of the Fifth Conference,2013.
[徐慧茹,杨振宇,朱日祥.华北克拉通在Columbia超大陆的古位置[C].中国地球物理第五分会场论文集,2013.]
[78] Pei Junling,Yang Zhenyu,Zhao Yue.New results of the Palaeoproterozoic ancient geomagnetic testing in North China and reseacch of Columbia supercontinent[J].Geological Bulletin of China,2005,24(6):496-498.
[裴军令,杨振宇,赵越.华北中元古界古地磁测试新结果与 Columbia 超级大陆研究[J].地质通报,2005,24(6):496-498.]
doi: 10.3969/j.issn.1671-2552.2005.06.002     URL    
[79] Zhang S B,Zheng Y F,Wu Y B,et al.Zircon isotope evidence for ≥3.5 Ga continental crust in the Yangtze craton of China[J].Precambrian Research,2006,146(1):16-34.
doi: 10.1016/j.precamres.2006.01.002     URL    
[80] Peng Min.Paleoproterozoic Magmatism of Yangtze Craton:Timing and Geological Implications[D].Wuhan: China University of Geosciences(Wuhan),2010.
[彭敏. 扬子板块古元古代岩浆事件年龄及其地质意义[D].武汉:中国地质大学, 2010.]
[81] QiuY 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 Arehean crustal evolution and Phanerozoic tectonics[J].Geology, 2000,26(1):11-14.
[82] Ling Wenli,Gao Shan,Zhang Benren,et al.The Paleoproterozoic tectonic heat events and evolution of the Yangtze Craton[J].Chinese Science Bulletin,2000,45(21):2 343-2 348.
[凌文黎,高山,张本仁,等.扬子陆核古元古代晚期构造热事件与扬子克拉通演化[J].科学通报,2000,45(21):2 343-2 348.]
doi: 10.3321/j.issn:0023-074X.2000.21.019     URL    
[83] Lei Hengcong,Xiang Hua,Zhang Zeming,et al.Paleoproterozoic UHT granulite in the Sulu orogen and its tectonic implications[J].Acta Petrologica Sinica,2014,30(8):2 435-2 445.
[雷恒聪,向华,张泽明,等.苏鲁造山带古元古代超高温麻粒岩及其构造意义[J].岩石学报,2014,30(8):2 435-2 445.]
URL    
[84] Compston W,Williams I S,Kirschvink J L,et al.Zircon U-Pb ages for the Early Cambrian time-scale[J].Journal of the Geological Society,1992,149(2):171-184.
doi: 10.1144/gsjgs.149.2.0171     URL    
[85] Zheng J,Griffin W L,O'Reilly S Y,et al. 3.6 Ga lower crust in central China:New evidence on the assembly of the North China craton[J].Geology,2004,32(3):229-232.
doi: 10.1130/G20133.1     URL    
[86] Wu Yuanbao,Chen Daogong,Xia Qunke,et al.SIMS U-Pb dating of zircons in granulite of Huangtuling from Northern Dabieshan[J].Acta Petrolog ica Sinica,2002,18(3):378-382.
[吴元保,陈道公,夏群科,等.北大别黄土岭麻粒岩错石U-Pb离子探针定年[J].岩石学报,2002,18(3):378-382.]
doi: 10.3969/j.issn.1000-0569.2002.03.013     URL    
[87] Yin Congyu,Liu Dunyi,Gao Linzhi,et al.The age of the Nanhua Period foundation and the Gucheng ice era: Evidence from SHRIMP Ⅱdating[J].Chinese Science Bulletin,2003,48(16):1 721-1 725.
[尹崇玉,刘敦一,高林志,等.南华系底界与古城冰期的年龄:SHRIMP Ⅱ定年证据[J].科学通报,2003,48(16): 1 721-1 725.]
doi: 10.3321/j.issn:0023-074X.2003.16.002     URL    
[88] Peng Touping,Wang Yuejun,Fan Weiming,et al.Zircon U-Pb dating and its tectonic significance of Early Mesozoic acid igneous rocks in southern part of Lancang River[J].Science in China (Series D),2006, 36(2):123-132.
[彭头平,王岳军,范蔚茗,等.澜沧江南段早中生代酸性火成岩SHRIMP锆石U-Pb定年及其构造意义[J].中国科学:D辑,2006,36(2):123-132.]
doi: 10.3969/j.issn.1674-7240.2006.02.002     URL    
[89] Zhang Shaobing.Geoehemistry of the Yangtze Continental Nucleus and Its Anatectic Granitoids[D].Wuhan: China University of Geosciences(Wuhan),2008.
[张少兵. 扬子陆核古老地壳及其深熔产物花岗岩的地球化学研究[D].武汉:中国地质大学,2008.]
[90] Li Jianghai,Hou Guiting,Huang Xiongnan,et al.Precambrian geology of North China Block[J]. Acta Petrologica Sinica,2001,17(2):177-186.
[李江海,侯贵廷,黄雄南,等.华北克拉通对前寒武纪超大陆旋回的基本制约[J].岩石学报,2001,17(2):177-186.]
doi: 10.3321/j.issn:1000-0569.2001.02.001     URL    
[91] Hou G,Liu Y,Li J.Evidence for ~1.8Ga extension of the Eastern Block of the North China Craton from SHRIMP U-Pb dating of mafic dyke swarms in Shandong Province[J].Journal of Asian Earth Sciences,2006,27(4):392-401.
doi: 10.1016/j.jseaes.2005.05.001     URL    
[92] Peng P.Reconstruction and interpretation of giant mafic dyke swarms: A case study of 1.78 Ga magmatism in the North China craton[J].Geological Society London Special Publications,2010,338(1):163-178.
doi: 10.1144/SP338.8     URL    
[93] Gao Shanlin,Lin Jinyan,Lu Yanjun.Formation epoch and its geological implications of Paleoprotozoic A-type granite in Shizuizi of Jingyuan County,Ningxia Province[J].Acta Petrologica Sinica, 2013,29(8):2 676-2 684.
[高山林,林晋炎,陆彦俊.宁夏泾源石咀子古元古代A型花岗岩的形成时代及其地质意义[J].岩石学报,2013,29(8):2 676-2 684.]
URL    
[94] Lu Songnian,Yuan Guibang.Geochronology of early Precambrian magmatic activities in Aketashitage,east Altyn tage[J].Acta Geologica Sinica,2003,77(1):61-68.
[陆松年,袁桂邦.阿尔金山克塔什塔格早前寒武纪岩浆活动的年代学证据[J].地质学报,2003,77(1):61-68.]
[95] Wang Yuxi,Wang Jinrong,Zhou Xiaoling,et al.The cracking of Columbia Supercontinental:Evidence from the Dahongshan A-type granite in the southeastern Tarim Craton[J].Acta Geologica Sinica,2017,91(11):2 369-2 386.
[王玉玺,王金荣,周小玲,等.Columbia超大陆裂解:来自塔里木克拉通东南缘大红山A型花岗岩的证据[J].地质学报,2017,91(11):2 369-2 386.]
[96] Xiao Qinghui,Lu Huanxiang,Wang Fei,et al.Geochronological studies of rapakivi granites in North of Qaidam Basin and its geological implications[J].Science in China (Series D),2003,33(12):1 193-1 200.
[肖庆辉,卢欣祥,王菲,等.柴达木北缘鹰峰环斑花岗岩的时代及地质意义[J].中国科学:D辑,2003,33(12):1 193-1 200.]
doi: 10.3321/j.issn:1006-9267.2003.12.008     URL    
[97] Zhao Guochun,Sun Min,Wilde S A.The research progress of the Early-Middle Proterozoic Columbia super-continental[J].Chinese Science Bulletin,2002,47(18):1 361-1 364.
[赵国春,孙敏,Wilde S A.早—中元古代Columbia超级大陆研究进展[J]. 科学通报,2002,47(18):1 361-1 364.]
[98] Hou Guiting, Li Jianghai, Qian Xianglin.Geochemical characteristics and tectonic setting of Mesoproterozoic dyke swarms in northern Shanxi[J]. Acta Petrologica Sinica,2001,17(3):352-357.
[侯贵廷,李江海,钱祥麟.晋北地区中元古代岩墙群的地球化学特征和大地构造背景[J].岩石学报,2001,17(3):352-357.]
doi: 10.3321/j.issn:1000-0569.2001.03.002     URL    
[99] Peng Suxia,Yin Chuanming,Liu Jianchao,et al.The analysis and review of nature of Cambrian basement, origin of volcanic rocks and the prospecting problems in Northern Qilian Orogenic Belt[J].Geology and Prospecting,2012,48(2):250-258.
[彭素霞,尹传明,刘建朝,等.对北祁连造山带前寒武纪基底物性, 火山岩的源区性质及找矿问题的分析和综述[J].地质与勘探,2012,48(2):250-258.]
URL    
[100] Li Jianghai,Qian Xianglin,Huang Xiongnan,et al.Tectonic framework of North China Block and its cratonization in the early Precambrian[J].Acta Petrologica Sinica,2000,16(1):1-10.
[李江海,钱祥麟,黄雄南,等.华北陆块基底构造格局及早期大陆克拉通化过程[J].岩石学报,2000,16(1):1-10.]
doi: 10.3321/j.issn:1000-0569.2000.01.001     URL    
[101] Liu Chaohui,Liu Fulai.The Mesoproterozoic rifting in the North China Craton:A case study for magmatism and sedimentation of the Zhaertai-Bayan Obo-Huade rift zone[J].Acta Petrologica Sinica,2015, 31(10):3 107-3 128.
[刘超辉, 刘福来.华北克拉通中元古代裂解事件:以渣尔泰—白云鄂博—化德裂谷带岩浆与沉积作用研究为例[J].岩石学报,2015,31(10):3 107-3 128.]
URL    
[1] 赵振洋, 李双建, 王根厚. 中下扬子北缘中二叠统孤峰组层状硅质岩沉积环境、成因及硅质来源探讨[J]. 地球科学进展, 2020, 35(2): 137-153.
[2] 牛耀龄, 龚红梅, 王晓红, 肖媛媛, 郭鹏远, 邵凤丽, 孙普, 陈硕, 段梦, 孔娟娟, 王国栋, 薛琦琪, 高雅洁, 洪迪. 用非传统稳定同位素探索全球大洋玄武岩、深海橄榄岩成因和地球动力学的几个重要问题[J]. 地球科学进展, 2017, 32(2): 111-127.
[3] 何冰辉. 关于峨眉山大火成岩省一些问题的研究现状[J]. 地球科学进展, 2016, 31(1): 23-42.
[4] 杨婧, 王金荣, 张旗, 陈万峰, 潘振杰, 焦守涛, 王淑华. 弧后盆地玄武岩(BABB)数据挖掘:与MORB及IAB的对比[J]. 地球科学进展, 2016, 31(1): 66-77.
[5] 卜文瑞,李 力,朱爱美,张 辉,张 俊,崔菁菁. 海底蚀变玄武岩中次生组分去除实验研究[J]. 地球科学进展, 2012, 27(10): 1167-1172.
[6] 孙书勤,张成江,黄润秋. 板块汇聚边缘玄武岩大地构造环境的Th、Nb、Zr判别[J]. 地球科学进展, 2006, 21(6): 593-598.
[7] 王永锋;金振民;. 地震波各向异性:窥测地球深部构造的“探针”[J]. 地球科学进展, 2005, 20(9): 946-953.
[8] 彭头平;王岳军;彭冰霞. 一种罕见的岩石——富铁玄武岩/富铁苦橄岩研究进展[J]. 地球科学进展, 2005, 20(5): 525-532.
[9] 张海祥;张伯友;牛贺才. 富铌玄武岩:板片熔体交代的地幔楔橄榄岩部分熔融产物[J]. 地球科学进展, 2005, 20(11): 1234-1242.
[10] 朱炳泉,常向阳,胡耀国,张正伟. 滇—黔边境鲁甸沿河铜矿床的发现与峨眉山大火成岩省找矿新思路[J]. 地球科学进展, 2002, 17(6): 912-917.
[11] 张树明,王方正. 玄武岩在研究岩石圈深部过程及构造背景中的应用[J]. 地球科学进展, 2002, 17(5): 685-692.
[12] 李荫亭. 地幔柱假说及其发展[J]. 地球科学进展, 1997, 12(5): 484-487.
[13] 孙晓猛,张旗,钱青. 甘肃肃南白泉门地区蛇绿混杂岩地质特征[J]. 地球科学进展, 1997, 12(4): 340-350.
阅读次数
全文


摘要