Geochronology, geochemical characteristics and tectonic implications of the amphibolite from Paxialayidang area on the southern margin of Altun terrain
-
摘要:
阿尔金造山带南缘帕夏拉依档沟零星发育一些斜长角闪岩，主要呈透镜状或豆荚状产于阿尔金岩群大理岩中。文章对这些斜长角闪岩开展了岩相学、年代学以及地球化学方面的研究，获得斜长角闪岩LA-ICP-MS锆石U-Pb年龄为（857.4±7.1）Ma和（432.5±5）Ma，前者代表其形成年龄，后者代表其变质年龄。地球化学特征显示斜长角闪岩轻稀土微弱富集，轻重稀土分异不显著，并有部分消减带玄武岩地球化学特征，源区为古俯冲带再循环的富集地幔源区，并受到流体或熔体的改造。结合判别图解和区域构造演化，分析得出斜长角闪岩原岩形成于初始裂谷环境，是大陆拉张向裂谷转换机制下形成的过渡岩石类型，较新年龄（432.5±5）Ma为早志留世陆壳伸展和软流圈底辟作用引起的变质年龄。本次研究为新元古代中晚期阿尔金南缘基性岩浆活动提供了新的年代学和地球化学方面的证据，这期基性岩浆活动可能为Rodinia超大陆初始裂解事件在阿尔金南缘的响应。
-
关键词:
- 斜长角闪岩 /
- 帕夏拉依档 /
- 初始裂谷 /
- Rodinia超大陆 /
- 阿尔金南缘
Abstract:Amphibolite is distributed sporadically in Paxialayidang area on the southern margin of Altun terrain. The amphibolite is ellipsoidal or lenticular in shape and is wrapped by marble of Altun terrain. In this paper, the authors studied petrology, geochronology and geochemistry of the amphibolites. LA-ICPMS zircon U-Pb dating yielded ages of (432.5±5) Ma and (857.4±7.1) Ma for metamorphic event and protolith respectively, and shows that the protolith was formed during Neoproterozoic Qingbaikou period. Amphibolite is slightly enriched in REE, and shows unnoticeable fractionation between light rare earth elements (LREE) and heavy rare earth elements (LREE) and the signatures of subduction zone basalt. The primary magma originated from an enriched mantle source, which was formed by the recirculation of subducted slab, and was modified by fluid or melt subsequently. Combined with the evolution of regional tectonic, the authors hold that the protolith of amphibolite was formed in an incipient continental rift and was a transitional type formed during the transition from continental extension to continental rift. The younger age of (432.5±5) Ma represents the time of metamorphic event, which was caused by the detachment of continental lower crust during Early Silurian. In this paper, the authors provide new geochronological and geochemical evidence about basic magmatic activity during middle-late stage of Neoproterozoicin on the southern margin of Altun terrain. The basic magmatic activity was the response to the Rodinia supercontinent breakup on the southern margin of Altun terrain.
-
1. 研究目的（Objective）
松科二井，获取了从基底—火石岭组—沙河子组—营城组—登娄库组下部连续完整的原位岩心。本文对松科二井沙河子组上部的孢粉化石进行研究，为研究白垩纪地球温室气候和环境变化，建立服务“百年大庆”目标和基础地质研究的“金柱子”提供基础资料。
2. 研究方法（Methods）
孢粉样品采自松科二井3395.46~3901.35 m，岩性为黑色、灰黑色泥岩、粉砂质泥岩，层位为沙河子组上部。孢粉分析鉴定在吉林大学古生物学与地层学研究中心完成，具体过程为：每个样品取过筛的干样50 g，进行盐酸→氢氟酸→氢氧化钾→盐酸→硝酸→氢氧化钾→盐酸等分析处理，用筛选法将样品中的孢粉化石集中在试管中，制2个固定片在生物显微镜下鉴定。
3. 研究结果（Results）
依据松科二井3395.46~3901.35 m井段的孢粉化石演化特征，划分出两个孢粉组合。
（1）Leiotriletes sp.- Cyathidites australis - Chasmatosporites sp.组合（简称LCC组合），分布在3832.94~3901.35m井段。蕨类孢子占绝对优势，裸子类花粉较低，未见被子类花粉。蕨类孢子含量最高的是Cyathidites australis，其次是Leiotriletes sp.和Cyclogranisporites sp.，有时代意义的还有Cicatricosisporites exilis、C. minutaestriatus、C. splendidus、C.australiensis、Klukisporites sp.、Maculatisporites sp.、Triporoletes singularis、Trilobosporites tribotrys、Aequitriradites sp.和Polycingulatisporites reduncus等；裸子类花粉含量最高的是Chasmatosporites sp.，其次是Psophosphaera sp.，有时代意义的类型有Parvisaccites sp.、Erlianpollis minisculus、Paleoconifersp.、Pseudowalchia sp.和Classopollis sp.等。
（2）Klukisporites triangulus- Aequitriradites sp.- Pristinuspollenites sp.组合（简称KAP组合），分布在3395.46~3613.62 m井段。裸子类花粉百分含量（53.03%~72.13%）较高，其次为蕨类孢子（27.87% ~46.97%），未见到被子类花粉。裸子类花粉中含量最高的是Alisporites parvus，其次是Piceaepollenites sp.，含量较高的类型还有Chasmatosporites sp.、Pinuspollenites divulgatus和P. sp.等，有时代意义的还有Parvisaccites otagoensis、Erlianpollis minisculus、E. mediocris、Jiaohepollis sp.和Classopollis classoides等。蕨类孢子含量最高的是Klukisporites sp.，其次是Leiotriletes sp.和Cyathidites australis，含量较高的类型还有Cyclogranisporites sp.等，有时代意义的有Cicatricosisporites exilis、C.apiteretus、C. australiensis、Klukisporites triangulus、K.variegatus、Pilosisporites scitulus、Impardecispora sp.、Levisporites wulinensis、Triporoletes singularis、Trilobosporites humilis、Aequitriradites sp.和Schizaeoisporites sp.等。
含有早白垩世特有或在早白垩世繁盛的分子：Cicatricosisporites、Klukisporites、Pilosisporites、Maculatisporites、Impardecispora、Levisporites、Triporoletes、Trilobosporites、Aequitriradites、Schizaeoisporites、Polycingulatisporites、Parvisaccites、Paleoconiferus、Erlianpollis、Foveotriletes.和Classopollis等（图 1）。
![]()
图 1 松科二井沙河子组部分孢粉化石（1-Cicatricosisporites exilis，样品号：SK2-375；2. -Cicatricosisporites minutaestriatus，标品号：SK2-385；3-Cicatricosisporites splendidus，标品号：SK2-385；4-Cicatricosisporites australiensis，样品号(sample number)：SK2-375；5-Levisporites wulinensis，样品号(sample number)：SK2-205；6. Aequitriradites sp.，样品号(sample number)：SK2-389; 7-Trilobosporites tribotrys，样品号(sample number)：SK2-389；8- Classopollis classoides，标品号：SK2-97；9-Erlianpollis minisculus，样品号(number)：SK2-395; 10. Parvisaccites sp.，样品号：SK2-395；11. Pilosisporites scitulus，标品号：SK2-201；12-Triporoletes asper，标品号(specimen number)：SK2-219；13. Foveotriletes subtriangulularis，样品号：SK2-219；14-Klukisporites triangulus，样品号(sample number)：SK2-205；15-Impardecispora sp.，样品号：SK2-201; 16-Schizaeoisporites polaris，样品号：SK2-173；17-Polycingulatisporites reduncus，标品号：SK2-395；18-Maculatisporites sp.，样品号：SK2-391。19-Chasmatosporites sp.，样品号：SK2-389; 20-Paleoconiferae sp.，样品号(sample number)：SK2-391;线段比例尺为10 μm, the scale of the line segment is 10 μm）Figure 1. Spores and pollen from the Lower Cretaceous Shahezi Formation in Well SK2上述2个孢粉组合分布在，属沙河子组上部，LCC组合蕨类孢子百分含量占绝对优势，裸子类花粉较少，从组合特点来看，可以与高瑞琪等人建立的沙河子组上部Granulatisporites-Lophotriletes-Cicatricosisporites组合大致对比，但上部的KAP组合层位显然高于高瑞琪等人建立的孢粉组合。与高瑞琪等人建立的孢粉组合相比，当前孢粉组合出现的有时代意义的孢粉类型更多且时代更新。
4. 结论（Conclusions）
两个孢粉组合海金砂科孢子繁盛，类型多样化，没有发现早期被子植物花粉；虽在蕨类孢子与裸子类花粉的百分含量及属种构成上明显不同，但出现的有时代意义的化石类型基本相同，其时代均为早白垩世早期。
5. 致谢（Acknowledgement）
本文为国家自然科学基金项目（41790451)和中国地质调查局项目（DD20190097）共同资助。孢粉化石由张淑琴研究员鉴定。
致谢: 本稿在成文过程中，匿名评审专家和编辑部的老师给出了建设性的审稿意见，中国地质大学（武汉）续海金老师、吴元保老师和西安地调中心的专家也提出了指导性建议，笔者在此一并表示衷心的感谢。 -
![]()
图 1 研究区地质简图及采样位置
TRB—塔里木盆地; QL—祁连山; QDB—柴达木盆地; WKL—西昆仑; EKL—东昆仑; TIBET—西藏; HMLY—喜马拉雅山; INP—印度板块; Ⅰ—阿北变质地块; Ⅱ—红柳沟-拉配泉混杂岩带; Ⅲ—米兰河-金雁山地块; Ⅳ—阿尔金南缘俯冲碰撞杂岩带; 1—第四系; 2—新近系油砂山组; 3—侏罗系大煤沟组；4—奥陶纪茫崖蛇绿混杂岩; 5—青白口系索尔库里群; 6—古元古代阿尔金岩群; 7—玉苏普阿勒塔格岩体；8—帕夏拉依档岩体；9—亚干布阳片麻岩；10—盖里克片麻岩；11—超基性岩块体; 12—玄武岩块体; 13—辉长岩脉；14—斜长角闪岩；15—区域大断裂；16—韧性剪切带；17—断层；18—不整合界限; 19—采样位置
Figure 1. Simplified geological map of the study area and sampling sites
TRB-Tarim basin; QL-Qilian Mountains; QDB-Qaidam basin; WKL-West Kunlun; EKL-East Kunlun; TIBET-Tibet; INP-Indian plate; HMLY-The Himalayas; INP-Indian plate; Ⅰ-Metamorphism plot of northern Altyn; Ⅱ-Hongliugou-Lapeiquan melange; Ⅲ-Milanhe-Jinyanshan plot; Ⅳ-Subduction collision complex zone of southern Altyn; 1-Quaternary; 2-Youshashan Formation; 3-Dameigou Group; 4-Mangya ophiolite melange; 5-Suoerkuliqun Group; 6-Aerjin Group; 7-Yusupualetage rock body; 8-Paxialayidang rock body; 9-Yaganbuyang gneiss; 10-Gailike gneiss; 11-Ultrabasic block; 12-Basalt block; 13-Gabbro dyke; 14-Amphibolite; 15-Regional fault; 16-Ductile shear zone; 17-Fault; 18-Unconformity; 19-Sampling location
![]()
图 2 斜长角闪岩野外及镜下特征
a、b—样品呈透镜状或豆荚状产出；c—单偏镜下斜长角闪岩；d—正交镜下斜长角闪岩Q—石英；Am—角闪石；Ep—绿帘石；Ch—绿泥石；Bi—黑云母
Figure 2. Photos of the outcrops and microscopic identification
a, b-Amphibolite in lenticular or podiform form in the open pit; c-Amphibolite (plainlight); d-Amphibolite (crossed nicols) Q-Quartz; Am-Amphibole; Ep-Epidote; Ch-Chlorite; Bi-Biotite
![]()
图 3 斜长角闪岩U-Pb年龄谐和图(a)和部分锆石阴极发光图(b)
Figure 3. U-Pb concordant diagram (a) of the zircons and CL images (a) from the plagioclase amphibolite
![]()
图 4 斜长角闪岩的TAS图解(a, 据文献[21])和Nb/Y-Zr/TiO2图解(b, 据文献[22])
Ir—Irvine分界线，上方为碱性，下方为亚碱性；1—橄榄辉长岩；2a—碱性辉长岩；2b—亚碱性辉长岩；3—辉长闪长岩；4—闪长岩；5—花岗闪长岩；6—花岗岩；7—硅英岩；8—二长辉长岩；9—二长闪长岩；10—二长岩；11—石英二长岩；12—正长岩；13—副长石辉长岩；14—副长石二长闪长岩；15—副长石二长正长岩；16—副长正长岩；17—副长深成岩；18—霓方钠岩/磷霞岩/粗白榴岩
Figure 4. TAS diagram (a) and Nb/Y versus Zr/TiO2 diagram of the Plagioclase amphibolites (b)
Ir-Irvine dividing line, The upper part is alkaline and the lower is sub-alkaline; 1-Olivine gabbro; 2a-Alkaline gabbro; 2b-Sub-alkaline gabbro; 3-Gabbro-diorite; 4-Diorite; 5-Granodiorite; 6-Granite; 7-Quartzolite; 8-Monzogabbro; 9-Monzodiorite; 10-Monzonite; 11-Adamellite; 12-Syenite; 13-Foid-gabbro; 14-Foid-monzodioritee; 15-Foid-monzosyenite; 16-Foid-syenite; 17-Foid-plutonite; 18-Beloeilite/urtite/italite
![]()
![]()
图 6 斜长角闪岩不活动元素构造环境判别图解
a—玄武岩的Cr-Y判别图解据文献[37]；VAB—火山弧玄武岩，WPB—板内玄武岩，MORB—大洋中脊玄武岩；b—玄武岩Zr-Zr/Y判别图解据文献[37]，IAB—岛弧玄武岩; MORB—大洋中脊玄武岩; WPB—板内玄武岩；c—玄武岩Nb/Zr-Th/Zr判别图解据文献[38]，A—大洋板块发散边缘N-MORB区; B1—大洋岛弧玄武岩区; B2—陆缘岛弧及陆缘火山弧玄武岩区; C—大洋板内区; D1—陆内裂谷及陆缘裂谷拉斑玄武岩区; D2—大陆拉张带(或初始裂谷)玄武岩区; D3—陆-陆碰撞带玄武岩; E—地慢热柱玄武岩区
Figure 6. Immobile trace element tectonic discrimination diagrams of plagioclase amphibolite
a-Cr-Y tectonic discrimination diagrams for the basalt; VAB-Volcanic arc basalts; WPB-Intraplate basalt; MORB-Mid ocean ridge basalt; b-Zr-Zr/Y, IAB=Island arc basalts; WPB-Intraplate basalt; MORB-Mid ocean ridge basalt; c-Nb/Zr-Th/Zr. A-Margin of divergent ocean; B1-Island arc of continental margin; B2-Volcanic arc of continental margin; C-Oceanic intraplate; D1-Continental rift; D2-Tentional zone; D3-Collision zone of two continental plates; E-Mantle plume
表 1 帕夏拉依档斜长角闪岩锆石LA-ICP-MS U-Pb测年分析结果
Table 1 LA-ICP-MS U-Pb analytical results of zircon from amphibolite of the Paxialayidang area
下载: 导出CSV
表 2 帕夏拉依档斜长角闪岩主量元素（%）、微量元素（10-6）地球化学测试结果
Table 2 Major (%) and trace elements (10-6) concentrations of the amphibolite in Paxialayidang area
下载: 导出CSV
-
[1] 许志琴,杨经绥,张建新,等.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制[J].地质学报,1999,73(3):193-205. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199903000.htm Xu Zhiqin,Yang Jingsui,Zhang Jianxin,et al.A comparison between the tectonic units on the two sides of the Altun sinistral strike-slip fault and the mechanism of lithospheric shearing[J].Acta Geologica Sinica,1999,73(3):193-205(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199903000.htm
[2] 覃小锋,李江,陆济璞,等.阿尔金碰撞造山带西段的构造特征[J].地质通报,2006,25(1/2):104-112. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2006Z1016.htm Qin Xiaofeng,Li Jiang,Lu Jipu,et al.The structural characteristics in the western part of Altyn collision orogenic belt[J].Geological Bulletin of China,2006,25(1/2):104-112(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2006Z1016.htm
[3] 张显庭,郑健康,苟金,等.阿尔金东段槽型晚奥陶世地层的发现及其构造意义[J].地质论评,1984,30(2):184-186. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198402011.htm Zhang Xianting,Zheng Jiankang,Gou Jin,et al.The discovery of late Ordovician strata of geosynclinal type in the eastern segment of the altun mountains and their tectonic implications[J].Geological Review,1984,30(2):184-186(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198402011.htm
[4] 葛肖虹,刘俊来.北祁连造山带的形成与背景[J].地学前缘,1999,6(4):222-229. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY199904005.htm Ge Xiaohong,Liu Junlai.Formation and tectonic background of the Northern Qilian orogenic belt[J].Earth Science Frontiers,1999,6(4):222-229(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY199904005.htm
[5] 程裕淇.中国区域地质概论[M].北京:地质出版社,1994. Cheng Yuqi.Regional Geological Survey China[M].Beijing:Geological Publishing House,1994(in Chinese).
[6] 伍跃中.阿尔金山的构造归属及其构造运动特征[J].地球科学与环境学报,2008,30(2):111-117. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX200802001.htm Wu Yuezhong.Tectonic attribution and movement characteristic of Altyn Mountain[J].Journal of Earth Sciences and Environment,2008,30(2):111-117(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX200802001.htm
[7] 校培喜,张海泉,王永和,等.阿中地块南缘晚元古代火山岩地质特征及构造环境分析[J].成都理工大学学报(自然科学版),2004,31(5):461-466. http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200405004.htm Xiao Peixi,Zhang Haiquan,Wang Yonghe,et al.Analysis of geological feature and tectonic environment for Neoproterozoic volcanic rocks in southern margin of Middle Altun Plot[J].Journal of Chengdu University of Technology (Science&Technology Edition),2004,31(5):461-466(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200405004.htm
[8] 刘良,车自成,王焰,等.阿尔金高压变质岩带的特征及其构造意义[J].岩石学报,1999,15(1):57-64. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB901.005.htm Liu Liang,Che Zicheng,Wang Yan,et al.Characteristics and tectonic significance of high-pressure metamorphic belt Altun[J].Acta Petrologica Sinica,1999,15(1):57-64(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB901.005.htm
[9] 刘永顺,于海峰,辛后田,等.阿尔金山地区构造单元划分和前寒武纪重要地质事件[J].地质通报,2009,28(10):1430-1438. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200910011.htm Liu Yongshun,Yu Haifeng,Xin Houtian,et al.Altun tectonic unit division and the Precambrian important geological events[J].Geological Bulletin of China,2009,28(10):1430-1438(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200910011.htm
[10] 张建新,孟繁聪,Mattinson C G.南阿尔金-柴北缘高压-超高压变质带研究进展、问题及挑战[J].高校地质学报,2007,13(3):526-545. Zhang Jianxin,Meng Fancong,Mattinson C G.Progress,controversies and challenge of studies on south Altyn Tagh-North Qaidam HP/UHP metamorphic belt[J].Geological Journal of China Universities,2007,13(3):526-545(in Chinese with English abstract).
[11] 刘良,陈丹玲,王超,等.阿尔金、柴北缘与北秦岭高压-超高压岩石年代学研究进展及其构造地质意义[J].西北大学学报(自然科学版),2009,39(3):472-479. Liu Liang,Chen Danling,Wang Chao,et al.New progress on geochronology of high-pressure/ultrahigh-pressure metamorphic rocks from the South Altyn Tagh,the North Qaidam and the North Qinling orogenic belt,NW China and their geological significance[J].Journal of Northwest University (Natural Science Edition),2009,39(3):472-479(in Chinese with English abstract).
[12] 刘永顺,于海峰,修群业,等.南阿尔金地区榴辉岩特征及意义[J].岩石矿物学杂志,2010,39(2):166-174. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201002005.htm Liu Yongshun,Yu Haifeng,Xiu Qunye,et al.Characteristics and tectonic implications of eclogites in southern Altun area[J].Acta Petrologica et Mineralogica,2010,39(2):166-174(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201002005.htm
[13] 曹玉亭,刘良,王超,等.阿尔金南缘塔特勒克布拉克花岗岩的地球化学特征、锆石U-Pb定年及Hf同位素组成[J].岩石学报,2010,26(11):3259-3271. Cao Yuting,Liu Liang,Wang Chao,et al.Granite geochemical characteristics,zircon U-Pb dating and Hf isotope composition at Tatelekebulake in the South of Altun[J].Acta Petrologica Sinica,2010,26(11):3259-3271(in Chinese with English abstract).
[14] 董增产,校培喜,奚仁刚,等.阿尔金南缘构造混杂岩带中角闪辉长岩地球化学特征及同位素测年[J].地质论评,2011,57(2):307-216. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201102006.htm Dong Zengchan,Xiao Peixi,Xi Rengang,et al.Geochemical characteristics and isotopic dating of bojites in the tectonic melange belt on south margin of Altun[J].Geological Review,2011,57(2):307-216(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201102006.htm
[15] 刘良,张安达,陈丹玲,等.阿尔金江尕勒萨依榴辉岩和围岩锆石LA-ICP-MS微区原位定年及其地质意义[J].地学前缘,2007,14(1):98-107. doi: 10.1016/S1872-5791(07)60004-9 Liu Liang,Zhang Anda,Chen Danling,et al.Implications based on LA-ICP-MS zircon U-Pb ages of eclogite and its country rock from Jianggalesayi area,Altyn Tagh[J].Earth Science Frontiers,2007,14(1):98-107(in Chinese with English abstract). doi: 10.1016/S1872-5791(07)60004-9
[16] Ludwig K R.User's Manual for Isoplot 3.0:A geochronological Toolkit for Microsoft Excel[J].Berkeley Geochronological Center,Special Publication,2003,4:1-71.
[17] 袁洪林,吴福元,高山,等.东北地区新生代侵入体的锆石激光探针U-Pb测定与稀土元素成分分析[J].科学通报,2003,48(14):1511-1520. Yuan Honglin,Wu Fuyuan,Gao Shan,et al.Cenozoic intrusive laser probe zircon U-Pb and rare earth element composition analysis determination in Northeast[J].Chinese Science Bulletin,2003,48(14):1511-1520(in Chinese).
[18] 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. Wu Yuanbao,Zheng Yongfei.Zircon minerageny and its restriction on interpretion of U-Pb age[J].Chinese Science Bulletin,2004,49(16):1589-1604(in Chinese).
[19] Hoskin P W O,Black L P.Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon[J].Journal of Metamorphic Geology,2000,18:423-439. http://cn.bing.com/academic/profile?id=1521262137&encoded=0&v=paper_preview&mkt=zh-cn
[20] Rubatto D,Gebauer D.Use of cathodoluminescence for U-Pb zircon dating by IOM Microprobe:Some examples from the western Alps[J].Cathodoluminescence in Geoscience,Springer-Verlag Berlin Heidelberg,Germany.2000:373-400. http://www.researchgate.net/publication/230814801_Use_of_Cathodoluminescence_for_U-Pb_Zircon_Dating_by_Ion_Microprobe_Some_Examples_from_the_Western_Alps
[21] Le Bas B M,Le Maitre R W,Strckeisen A,et al.A chemical classification of volcanic rocks based on the total alkali-silica diagram[J].Journal of Petrology,1986,27:745-750. doi: 10.1093/petrology/27.3.745
[22] Winchester J A,Floyd P A.Geochemical discrimination of different magma series and their differentiation products using immobile elements[J].Chemical Geology,1977,20:325-343. doi: 10.1016/0009-2541(77)90057-2
[23] Woodhead J D.The origin of geochemical variations in Mariana lavas:A general model for petrogenesis in Intra-Oceanic Island Arcs?[J].Journal of Petrology,1988,29(4):805-830. doi: 10.1093/petrology/29.4.805
[24] 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
[25] 杨红,刘平华,孟恩,等.扬子地块西南缘大红山群变质基性岩的地球化学研究及构造意义[J].岩石学报,2014,30(10):3021-3033. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201410017.htm Yang Hong,Liu Pinghua,Meng En,et al.Geochemistry and tectonic significance for metabasite in the Dahongshan Group at the western margin of the Yangtze Block[J].Acta Petrologica Sinica,2014,30(10):3021-3033(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201410017.htm
[26] McCulloch M T,Gamble J A.Geochemical and geodynamical constraints on subduction zone magmatism[J].Earth and Planetary Science Letters,1991,102(3-4):358-374. doi: 10.1016/0012-821X(91)90029-H
[27] Pearce J A,Peate D W.Tectonic implications of the composition of volcanic arc magmas[J].Annual Reviews of Earth and Planetary Sciences,1995,23:251-286. doi: 10.1146/annurev.ea.23.050195.001343
[28] Dupuy C,Dostal J.Trace element geochemistry of some continental tholeiites[J].Earth and Planetary Science Letters,1984,67(1):61-69. doi: 10.1016/0012-821X(84)90038-4
[29] 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. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200504002.htm Fu Guomin,Su Jianping,Hu Nenggao,et al.Geochemistry and tectonic setting of amphibolites in the Paleoproterozoic Beidahe Group-complex in the western segment of the Qilian Mountains[J].Geology in China,2005,32(4):541-547(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200504002.htm
[30] Hawkesworth C,Turner S,Gallagher K,et al.Calc-alkaline magmatism,lithosphericthinning and extension in the Basinand Range[J].Geophys Research,1995,100(B6):10271-10286. doi: 10.1029/94JB02508
[31] Weaver B L.The origin of oceanic basalt end-member compositions:Trace element and isotopic constrains[J].Earth and Planetary Science Letters,1991,104(2-4):381-397. doi: 10.1016/0012-821X(91)90217-6
[32] Wilson M.Igneous petrogenesis,London:Unwin Hyman,1989:1-466.
[33] 张招崇,肖序常,王军,等.西昆仑山普鲁新生代火山岩中包体的发现及其地质意义[J].地球科学——中国地质大学学报,2002,27(4):386-390. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200204006.htm Zhang Zhaochong,Xiao Xuchang,Wang Jun,et al.Discovery of Enclaves from Cenozoic Pulu Volcanic Rocks of West Kunlun Mountains and Their Geological Implications[J].Earth Science——(Journal of China University of Geosciences,2002,27(4):386-390(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200204006.htm
[34] Woodhead J D,McCullon M T.Ancient seafloor signals in Pitcairn Island lavas and evidence for large amplitude,small lengthscale mantle heterogeneities[J].Earth Planetary Sci Lett,1989,94(3):257-273. http://cn.bing.com/academic/profile?id=2016684177&encoded=0&v=paper_preview&mkt=zh-cn
[35] Pearce J A.Role of the sub-continental lithosphere in magma genesis at active continental margin[C]//Hawkesworth C J and Norry M J.Continental bBasalts and Mantle Xenoliths,1983:230-272.
[36] Huang Y,Hawkesworth C,Smith I,et al.Geochemistry of late Cenozoic basaltic volcanism in Northland and Coromandel,New Zealand:Implications for mantle enrichment processes[J].Chemical Geology,2000,164(15):219-238. http://cn.bing.com/academic/profile?id=2160257318&encoded=0&v=paper_preview&mkt=zh-cn
[37] 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,2007,26(1):77-89. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200701010.htm Xia Linqi,Xia Zuchun,Xu Xueyi et al.The discrimination between continental basalt and island arc basalt based on geochemical method[J].Acta Petrologica et Mineralogica,2007,26(1):77-89(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200701010.htm
[38] 孙书勤,汪云亮,张成江.玄武岩类岩石大地构造环境的Th、Nb、Zr判别[J].地质论评,2003,49(1):40-47. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200301005.htm Sun Shuqin,Wang Yunliang,Zhang Chengjiang.Disecrimination of the tectonic settings of basalts by Th、Nb and Zr[J].Geological ophiolite belt[J].Chinese Science Bulletin,1998,43(18):1981-1984(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200301005.htm
[39] Agrawal S,Guevara M,Verma S P.Tectonic discrimination of basic and ultrabasic volcanic rocks through log-transformed ratios of immobile trace elements[J].International Geology Review,2008,50(12):1057-1079. doi: 10.2747/0020-6814.50.12.1057
[40] 李江海,钱祥麟,翟明国.华北北部麻粒岩相带构造区划及其早前寒武纪构造演化[J].地质科学,1997,32(3):224-226. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX703.001.htm Li Jianghai,Qian Xianglin,Zhai Mingguo.The tectonic division of north China Granulite facies belt and its early Precambrian tectonic evolution[J].Scientia Geologica Sinica,1997,32(3):224-226(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX703.001.htm
[41] Li Z X,Bogdanova S V,Collins A S,et al.Assembly,configuration and break-up history of Rodinia:A synthesis[J].Precambrian Research,2008,160(1/2):179-210. http://cn.bing.com/academic/profile?id=2048240400&encoded=0&v=paper_preview&mkt=zh-cn
[42] Lu S N,Li H K,Zhang C L,et al.Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton and surrounding continental fragments[J].Precambrian Research,2008,160(1-2):94-107. doi: 10.1016/j.precamres.2007.04.025
[43] 梅华林,李惠民,陆松年,等.甘肃柳园地区花岗质岩石时代及成因[J].岩石矿物学杂志,1999,18(1):14-17. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW901.002.htm Mei Hualin,Li Huimin,Lu Songnian,et al.The age and origin of the Liuyuan granitoid,northwestern Gansu[J].Acta Petrologica et Mineralogica,1999,18(1):14-17(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW901.002.htm
[44] 王超,刘良,张安达,等.阿尔金造山带南缘岩浆混合作用:玉苏普阿勒克塔格岩体岩石学和地球化学证据[J].岩石学报,2008,24(12):2809-2819. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200812016.htm Wang Chao,Liu Liang,Zhang Anda,et al.Geochemistry of Early Paleozoic Yusupuleke Tagh rapakivi-textured granite complex,South Altyn:An example for magma mixing[J].Acta petrologica Sinica,2008,24(12):2809-2819(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200812016.htm
[45] 王立社,张巍,段星星,等.阿尔金环形山花岗片麻岩同位素年龄及成因研究[J].岩石学报,2015,31(1):119-132. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201501009.htm Wang Lishe,Zhang Wei,Duan Xingxing,et al.Isotopic age and genesis of the monzogranitic gneiss at the Huanxingshan in middle Altyn Tagh[J].Acta Petrologica Sinica,2015,31(1):119-132(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201501009.htm
[46] 叶晓峰,宗克清,张泽明,等.北山造山带南缘柳园地区新元古代花岗岩的地球化学特征及其地质意义[J].地质通报,2015,32(2-3):307-317. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2013Z1009.htm Ye Xiaofeng,Zong Keqing,Zhang Zeming,et al.Geochemistry of Neoproterozoic granite in Liuyuan area of southern Beishan orogenic belt and its geological significance[J].Geological Bulletin of China,2015,32(2-3):307-317(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2013Z1009.htm
[47] 陆松年,于海峰,李怀坤,等.中央造山带(中-西部)前寒武纪地质[M].北京:地质出版社,2009. Lu Songnain,Yu Haifeng,Li Huaikun,et al.Central Orogenic Belt (Middle-West) Precambrian Geology[M].Beijing:Geological Publishing House,2009.
[48] 李琦,曾忠诚,陈宁,等.阿尔金南缘新元古代盖里克片麻岩年代学、地球化学特征及其构造意义[J].现代地质,2015,29(6):1271-1283. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201506002.htm Li Qi,Zeng Zhongcheng,Chen Ning,et al.Zircon U-Pb ages,geochemical characteristics and tectonic implications of Neoproterozoic Gailike gneiss in the South Altyn Tagh[J],2015,29(6):1271-1283(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201506002.htm
[49] Meert J G,Torsvik T H.The making and unmaking of supercontinent:Rodinia revisited[J].Tectonophysics,2003,375(1-4):261-228. doi: 10.1016/S0040-1951(03)00342-1
[50] Li Z X,Li X H,Kinny P D,et al.The breakup of Rodinia:did it sart with a mantle plume beneath South China?[J].Earth and Planetary Science Letters,1999,173(3):171-181. doi: 10.1016/S0012-821X(99)00240-X
[51] 王超,刘良,车自成,等.塔里木南缘铁克里克构造带东段前寒武纪地层时代的新限定和新元古代地壳再造:锆石定年和Hf同位素的约束[J].地质学报,2009,83(11):1647-1656. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200911011.htm Wang Chao,Liu Liang,Che Zicheng,et al.Zircon U-Pb and Hf isotopic from the East Segment of Tiekelike tectonic belt:Constrains on the timing of Precambrian basement at the southwestern margin of Tarim[J].Acta Geologica Sinica,2009,83(11):1647-1656(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200911011.htm
[52] 曾建元,杨宏仪,万渝生,等.北祁连山变质杂岩中新元古代(-775Ma)岩浆活动纪录的发现:来自SHRIMP锆石U-Pb定年的证据[J].科学通报,2006,51(5):575-581. Zeng Jianyuan,Yang Hongyi,Wan Yusheng,ta al.Neoproterozoic (-775Ma) magmatism record North Qilian metamorphic rocks:Evidence from SHRIMP zircon U-Pb[J].Chinese Science Bulletin,2006,51(5):575-581(in Chinese).
[53] 刘函,王国灿,曹树钊,等.北阿尔金南华纪双峰式火山岩的发现及构造意义[J].地球科学——中国地质大学学报,2012,37(5):917-928. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201205007.htm Liu Han,Wang Guocan,Cao Shuzhao,et al.Discovery of Nanhuaian Bimodal volcanics in Nothern Altyn Tagh and its tectonic significan[J].Earth Science——Journal of China University of Geoscience,2012,37(5):917-928(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201205007.htm
[54] 郭召杰,张志诚,王建君.阿尔金山北缘蛇绿岩带的Sm-Nd等时线年龄及其大地构造意义[J].科学通报,1998,43(18):1981-1984. Guo Shaojie,Zhang Zhicheng,Wang Jianjun.Isochron age (Sm-Nd) and tectonic significance in northern margin of Altun ophiolite belt[J].Chinese Science Bulletin,1998,43(18):1981-1984(in Chinese with English abstract).
[55] 董顺利,李忠,高剑,等.阿尔金-祁连-昆仑造山带早古生代构造格架及结晶岩年代学研究进展[J].地质论评,2013,59(4):731-746. Dong Shunli,Li Zhong,Gao Jian,et al.Progress of studies on early Paleozoic tectonic framework and crystalline rock geochronology in Altun-Qilian-Kunlun orogen[J].Geological Review,2013,59(4):731-746(in Chinese with English abstract).
[56] 李德威,夏义平,徐礼贵.大陆板内盆山耦合及盆山成因——以青藏高原及周边盆地为例[J].地学前缘,2009,16(3):110-119. doi: 10.1016/S1872-5791(08)60097-4 Li Dewei,Xia Yiping,Xu Ligui.Coupling and formation mechanism of continental intraplate basin and orogen-Examples from the Qinghai-Tibet Plateau and adjacent basins[J].Earth Science Frontiers,2009,16(3):110-119(in Chinese with English abstract). doi: 10.1016/S1872-5791(08)60097-4
[57] Zhang J X,Mattinson C G,Meng F C,et al.Polyphase tectonothermal history recorded in granulitized gneisses from the North Qaidam HP/UHP metamorphic terrane,Western China:Evidence from zircon U-Pb geochronology[J].Geological Society of America Bulletin,2008,120(5/6):732-749. http://cn.bing.com/academic/profile?id=2008478454&encoded=0&v=paper_preview&mkt=zh-cn
[58] 杨经绥,史仁灯,吴才来,等.柴达木盆地北缘新元古代蛇绿岩的厘定——罗迪尼亚大陆裂解的证据?[J].地质通报,2004,23(9-10):892-898. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2004Z2009.htm Yang Jingsui,Shi Rendeng,Wu Cailai,et al.Recognition of Neoproterozoic ophiolite on the Northern margin of the Qaidam basin:evidence of breakup of Rodinia[J].Geological Bulletin of China,2004,23(9/10):892-898(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2004Z2009.htm
[59] 陈宣华,Gehrels G,王小凤,等.阿尔金山北缘花岗岩的形成时代及其构造环境探讨[J].矿物岩石地球化学通报,2003,22(4):294-298. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH200304002.htm Chen Xuanhua,Gehrels G,Wang Xiaofeng,et al.Tectonic environments of magmatism in Early Paleozoic in the north Altyn Tagh[J].Journal of geomechanics,2003,22(4):294-298(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH200304002.htm
[60] 吴才来,杨经绥,姚尚志,等.北阿尔金巴什考供盆地南缘花岗杂岩体特征及锆石SHRIMP定年[J].岩石学报,2005,21(3):846-858. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503025.htm Wu Cailai,Yang Jingsui,Yao Shangzhi,et al.Characteristics of the granitoid complex and its zircon SHRIMP dating at the south margin of the Bashikaogong Basin[J].Acta Petrologica Sinica,2005,21(3):846-858(in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503025.htm
[61] 陈丹玲,孙勇,刘良,等.柴北缘鱼卡河榴辉岩的超高压变质年龄:锆石LA-ICP-MS微区定年[J].中国科学,2007,37(增刊):279-287. Chen Danling,Sun Yong,Liu Liang,et al.The eclogite UHP age in North Qaidam:Zircon LA-ICP-MS micro dating[J].Science China Press,37(supp.):279-287(in Chinese with English abstract).
[62] Song S G,Zhang L F,Niu Y L,et al.Evolution from oceanic subduction to continental collision:a case study of the Northern Tibetan Plateau inferred from geochemical and geoch ronological data[J].Journal of Petrology,2006,47:435-455.
-
期刊类型引用(2)
1. 吴怀春，李山，王成善，褚润健，王璞珺，高远，万晓樵，贺怀宇，邓成龙，杨光，黄永建，高有峰，席党鹏，王天天，房强，杨天水，张世红. 松辽盆地白垩纪综合年代地层格架. 地学前缘. 2024(01): 431-445 . 
百度学术
2. 张德军，郑月娟，张淑芹，张健，黄欣，陈树旺，孙雷. 松科2井早白垩世沙河子组孢粉组合及其古气候意义. 地质通报. 2024(Z1): 429-442 . 百度学术
其他类型引用(2)
计量
- 文章访问数: 3174
- HTML全文浏览量: 510
- PDF下载量: 6041
- 被引次数: 4
