|本期目录/Table of Contents|

[1]赵 强,汤静如*,杨恒毅,等.佳木斯地块中部晚三叠世埃达克岩年代学、地球化学特征及其地质意义[J].地球科学与环境学报,2023,45(02):240-255.[doi:10.19814/j.jese.2022.02007]
 ZHAO Qiang,TANG Jing-ru*,YANG Heng-yi,et al.Geochronology and Geochemistry of Late Triassic Adakite in the Central Jiamusi Block, China and Their Geological Significance[J].Journal of Earth Sciences and Environment,2023,45(02):240-255.[doi:10.19814/j.jese.2022.02007]
点击复制

佳木斯地块中部晚三叠世埃达克岩年代学、地球化学特征及其地质意义(PDF)
分享到:

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第45卷
期数:
2023年第02期
页码:
240-255
栏目:
基础地质与矿床地质
出版日期:
2023-03-15

文章信息/Info

Title:
Geochronology and Geochemistry of Late Triassic Adakite in the Central Jiamusi Block, China and Their Geological Significance
文章编号:
1672-6561(2023)02-0240-16
作者:
赵 强12汤静如1*杨恒毅1张学琳1罗林菊1
(1. 桂林理工大学 地球科学学院,广西 桂林 541006; 2. 合肥工业大学 资源与环境工程学院,安徽 合肥 230009)
Author(s):
ZHAO Qiang12 TANG Jing-ru1* YANG Heng-yi1 ZHANG Xue-lin1 LUO Lin-ju1
(1. College of Earth Sciences, Guilin University of Technology, Guilin 541006, Guangxi, China; 2. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, Anhui, China)
关键词:
埃达克岩 地球化学 晚三叠世 锆石U-Pb年龄 花岗岩 佳木斯地块
Keywords:
adakite geochemistry Late Triassic zircon U-Pb age granite Jiamusi block
分类号:
P597
DOI:
10.19814/j.jese.2022.02007
文献标志码:
A
摘要:
大八浪岩体位于佳木斯地块中部的桦南隆起区,岩性为中细粒黑云母花岗闪长岩,其侵入到晚二叠世白云母二长花岗岩中。岩石 LA-ICP-MS锆石U-Pb年龄为(234±1)Ma,属于晚三叠世早期。大八浪岩体具有较高的SiO2含量(质量分数,下同)(62.04%~64.30%)、Al2O3含量(15.68%~16.95%)、Sr/Y值(23.38~36.15)、(La/Yb)N值(18.57~33.04),较低的MgO含量(0.91%~1.20%)和中等Mg#值(34.03~37.27),以及低Yb含量((1.18~1.52)×10-6,平均值为1.30×10-6)、Y含量((15.43~20.50)×10-6,平均值为16.94×10-6),同时Na2O/K2O值为0.77~1.06,平均值为0.94,显示与C型埃达克岩相似的地球化学特征。结合佳木斯地块东缘二叠世处在活动大陆边缘弧环境以及佳木斯地块晚三叠世周缘增生杂岩的分布特点,认为大八浪岩体可能是晚三叠世在古太平洋板块向佳木斯地块下部俯冲,造成佳木斯地块不断缩短加厚,其下地壳发生部分熔融的产物。
Abstract:
The Dabalang pluton, located in Huanan uplift area of the central Jiamusi block, is lithologically medium-to-fine-grained biotite granodiorites, which intrude into Late Permian muscovite monzogranites. LA-ICP-MS zircon U-Pb age is(234±1)Ma, the biotite granodiorites are in early Late Triassic. The Dabalang pluton has high SiO2 content(62.04%-64.30%), Al2O3 content(15.68%-16.95%), Sr/Y ratio(23.38-36.15)and(La/Yb)N ratio(18.57-33.04), containing low MgO content(0.91%-1.20%), moderate Mg# value(34.03-37.27), as well as low Yb content((1.18-1.52)×10-6 with an average of 1.30×10-6)and Y content((15.43-20.50)×10-6 with an average of 16.94×10-6), Na2O/K2O is 0.77-1.06 with an average of 0.94. The above geochemical characteristics are similar to the C-type adakites. Considering the active continental margin arc setting of Permian in the eastern margin of Jiamusi block and the distribution characteristics of Late Triassic peripheral accretionary complexes, it is found that the Dabalang pluton may be a product of partial melting of crust below Jiamusi block, which is continuously shortened and thickened due to the subduction of Paleo-Pacific plate towards the lower part of Jiamusi block in Late Triassic.

参考文献/References:

[1] 许文良,王 枫,裴福萍,等.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J].岩石学报,2013,29(2):339-353.
XU Wen-liang,WANG Feng,PEI Fu-ping,et al.Me-sozoic Tectonic Regimes and Regional Ore-forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations[J].Acta Petrologica Sinica,2013,29(2):339-353.
[2] 李伟民,刘永江,赵英利,等.佳木斯地块构造演化[J].岩石学报,2020,36(3):665-684.
LI Wei-min,LIU Yong-jiang,ZHAO Ying-li,et al.Tectonic Evolution of the Jiamusi Block,NE China[J].Acta Petrologica Sinica,2020,36(3):665-684.
[3] ZHOU J B,WILDE S A,ZHANG X Z,et al.The Onset of Pacific Margin Accretion in NE China:Evidence from the Heilongjiang High-pressure Metamorphic Belt[J].Tectonophysics,2009,478(3/4):230-246.
[4] ZHOU J B,WILDE S A.The Crustal Accretion History and Tectonic Evolution of the NE China Segment of the Central Asian Orogenic Belt[J].Gondwana Research,2013,23(4):1365-1377.
[5] TANG Z Y,SUN D Y,GOU J.Triassic Magmatism in Northeast China:Implications for Spatiotemporal Distribution,Continental Crustal Accretion,and Geodynamic Evolution[J].International Geology Review,2022,64(6):770-798.
[6] LIANG Y,ZHENG H,LI H,et al.Late Paleozoic-Mesozoic Subduction and Accretion of the Paleo-Pacific Plate:Insights from Ophiolitic Rocks in the Wandashan Accretionary Complex,NE China[J].Geoscience Frontiers,2021,12(6):101242.
[7] GUAN Q B,LIU Z H,LIU Y J,et al.A Tectonic Transition from Closure of the Paleo-Asian Ocean to Subduction of the Paleo-Pacific Plate:Insights from Early Mesozoic Igneous Rocks in Eastern Jilin Pro-vince,NE China[J].Gondwana Research,2022,102:332-353.
[8] LIU J,LI W M,FENG Z Q,et al.A Review of the Paleozoic Tectonics in the Eastern Part of Central Asian Orogenic Belt[J].Gondwana Research,2017,43:123-148.
[9] LIU J,ZHANG J,LIU Z H,et al.Petrogenesis of Permo-Triassic Intrusive Rocks in Northern Liaoning Province,NE China:Implications for the Closure of the Eastern Paleo-Asian Ocean[J].International Geo-logy Review,2020,62(6):754-780.
[10] JING Y,GE W C,SANTOSH M,et al.Generation of Nb-enriched Mafic Rocks and Associated Adakitic Rocks from the Southeastern Central Asian Orogenic Belt:Evidence of Crust-mantle Interaction[J].Geoscience Frontiers,2022,13(2):101341.
[11] YAO X F,YAN T J,LV Z C,et al.Ore-forming Age and Tectonic Setting of the Linjiasandaogou Gold Deposit in the Liaodong Peninsula,Northeast China:Constraints from Geochronology and Geochemistry[J].Acta Geochimica,2022,41(2):244-266.
[12] 王 博,赵国春.古亚洲洋的最终闭合时限:来自白乃庙岛弧带东段二叠纪—三叠纪岩浆作用的证据[J].西北大学学报(自然科学版),2021,51(6):1019-1030.
WANG Bo,ZHAO Guo-chun.Final Closure of the Paleo-Asian Ocean:Constraints from Permian-Triassic Magmatism in the Eastern Segment of the Bainai-miao Arc Belt[J].Journal of Northwest University(Natural Science Edition),2021,51(6):1019-1030.
[13] YANG H,GE W C,ZHAO G C,et al.Early Permian-Late Triassic Granitic Magmatism in the Jiamusi-Khanka Massif,Eastern Segment of the Central Asian Orogenic Belt and Its Implications[J].Gondwana Research,2015,27(4):1509-1533.
[14] 曹 熹,党增欣,张兴洲,等.佳木斯复合地体[M].长春:吉林科学技术出版社,1992.
CAO Xi,DANG Zeng-xin,ZHANG Xing-zhou,et al.Jianusi Complex Terrain[M].Changchun:Jilin Science and Technology Press,1992.
[15] 周建波,韩 杰,WILDE S A,等.吉林—黑龙江高压变质带的初步厘定:证据和意义[J].岩石学报,2013,29(2):386-398.
ZHOU Jian-bo,HAN Jie,WILDE S A,et al.A Primary Study of the Jilin-Heilongjiang High-pressure Metamorphic Belt:Evidence and Tectonic Implications[J].Acta Petrologica Sinica,2013,29(2):386-398.
[16] 许文良,王 枫,孟 恩,等.黑龙江省东部古生代—早中生代的构造演化:火成岩组合与碎屑锆石U-Pb年代学证据[J].吉林大学学报(地球科学版),2012,42(5):1378-1389.
XU Wen-liang,WANG Feng,MENG En,et al.Paleozoic-Early Mesozoic Tectonic Evolution in the Eastern Heilongjiang Province,NE China:Evidence from Igneous Rock Association and U-Pb Geochronology of Detrital Zircons[J].Journal of Jilin University(Earth Science Edition),2012,42(5):1378-1389.
[17] 郭 冶.黑龙江省东部跃进山杂岩的性质及构造演化[D].长春:吉林大学,2016.
GUO Ye.The Nature of the Yuejinshan Complex in the Eastern Part of Heilongjiang Province and Its Evolution[D].Changchun:Jilin University,2016.
[18] 曾 振.佳木斯地块与完达山杂岩的构造性质及其演化[D].长春:吉林大学,2017.
ZENG Zhen.The Tectonic Characteristics and Evolution of Jiamusi Massif and Wandashan Complex[D].Changchun:Jilin University,2017.
[19] 周建波.增生杂岩:从大洋俯冲到大陆深俯冲的地质记录[J].中国科学:地球科学,2020,50(12):1709-1726.
ZHOU Jian-bo.Accretionary Complex:Geological Records from Oceanic Subduction to Continental Deep Subduction[J].Science China:Earth Sciences,2020,50(12):1709-1726.
[20] 赵 强.佳木斯地块中部晚二叠—晚三叠世花岗岩地球化学特征及意义[J].桂林:桂林理工大学,2022.
ZHAO Qiang.Geochemical Characteristics and Signi-ficance of Late Permian-Late Triassic Granites in the Central Jiamusi Block[J].Guilin:Guilin University of Technology,2022.
[21] 赵 强,汤静如,姜迎久.佳木斯板块安山岩及花岗闪长斑岩成岩时代及意义[J].云南地质,2020,39(3):359-364.
ZHAO Qiang,TANG Jing-ru,JIANG Ying-jiu.The Dating and Significance of Andesite and Granodiorite in Jiamusi Plate[J].Yunnan Geology,2020,39(3):359-364.
[22] 曾 振,孙 雷,张兴洲,等.黑龙江跃进山杂岩中砾岩的碎屑锆石年代学及其大地构造意义[J].地质与资源,2019,28(3):215-222.
ZENG Zhen,SUN Lei,ZHANG Xing-zhou,et al.Detrital Zircon Chronology of Conglomerate in Yuejin-shan Complex,Heilongjiang Province:Geotectonic Implications[J].Geology and Resources,2019,28(3):215-222.
[23] ZHANG D,LIU Y J,LI W M,et al.Marginal Accretion Processes of Jiamusi Block in NE China:Evidences from Detrital Zircon U-Pb Age and Deformation of the Wandashan Terrane[J].Gondwana Research,2020,78:92-109.
[24] 周建波,曹嘉麟,韩 伟,等.长春—延吉缝合带:性质与意义[J].岩石学报,2020,36(3):635-643.
ZHOU Jian-bo,CAO Jia-lin,HAN Wei,et al.The Changchun-Yanji Suture Zone:Nature and Tectonic Implications[J].Acta Petrologica Sinica,2020,36(3):635-643.
[25] CAO J L,ZHOU J B,LI L.The Tectonic Evolution of the Changchun-Yanji Suture Zone:Constraints of Zircon U-Pb Ages of the Yantongshan Accretionary Complex(NE China)[J].Journal of Asian Earth Sciences,2020,194:104110.
[26] 周建波,张兴洲,WILDE S A,等.中国东北~500 Ma泛非期孔兹岩带的确定及其意义[J].岩石学报,2011,27(4):1235-1245.
ZHOU Jian-bo,ZHANG Xing-zhou,WILDE S A,et al.Confirming of the Heilongjiang ~500 Ma Pan-African Khondalite Belt and Its Tectonic Implications[J].Acta Petrologica Sinica,2011,27(4):1235-1245.
[27] 姜继圣.麻山群孔兹岩系的地球化学特征[J].地球化学,1993,22(4):363-372.
JIANG Ji-sheng.Geochemistry of Mashan-group Khondalite Series[J].Geochimica,1993,22(4):363-372.
[28] 姜继圣.麻山群孔兹岩系主期区域变质作用及演化[J].岩石矿物学杂志,1992,11(2):97-110.
JIANG Ji-sheng.Regional Metamorphism and Evolution of Mashan Khondalite Series[J].Acta Petrologica et Mineralogica,1992,11(2):97-110.
[29] 赵亮亮,王宗起,张兴洲.黑龙江省东部马家街群碎屑锆石年代学及其大地构造意义[J].岩石学报,2014,30(6):1769-1779.
ZHAO Liang-liang,WANG Zong-qi,ZHANG Xing-zhou.Detrital Zircon U-Pb Dating of Majiajie Group and Its Tectonic Implications[J].Acta Petrologica Sinica,2014,30(6):1769-1779.
[30] 周建波,张兴洲,WILDE S A,等.黑龙江杂岩的碎屑锆石年代及其大地构造意义[J].岩石学报,2009,25(8):1924-1936.
ZHOU Jian-bo,ZHANG Xing-zhou,WILDE S A,et al.Detrital Zircon U-Pb Dating of Heilongjiang Complex and Its Tectonic Implications[J].Acta Petrologica Sinica,2009,25(8):1924-1936.
[31] 张兴洲.黑龙江群中放射虫的首次发现及意义[J].长春地质学院学报,1991,21(2):156.
ZHANG Xing-zhou.The First Discovery and Significance of Radiolarians from Heilongjiang Group[J].Journal of Changchun University of Earth Science,1991,21(2):156.
[32] 赵亮亮.黑龙江杂岩构造演化的岩石学与年代学证据[D].长春:吉林大学,2011.
ZHAO Liang-liang.The Evidence of Petrology and Geochronology on Tectonic Evolution of Heilongjiang Complex in Eastern Heilongjiang Province,China[D].Changchun:Jilin University,2011.
[33] 黄映聪,张兴洲,张宏宾,等.黑龙江东部马家街群的岩石地球化学特征及其沉积时代[J].地质学报,2009,83(2):295-303.
HUANG Ying-cong,ZHANG Xing-zhou,ZHANG Hong-bin,et al.Geochemical Characteristics and Sedimentation Age of the Majiajie Group in Eastern Heilongjiang Province,China[J].Acta Geologica Sinica,2009,83(2):295-303.
[34] 黄映聪,任东辉,张兴洲,等.黑龙江省东部桦南隆起美作花岗岩的锆石U-Pb定年及其地质意义[J].吉林大学学报(地球科学版),2008,38(4):631-638.
HUANG Ying-cong,REN Dong-hui,ZHANG Xingzhou,et al.Zircon U-Pb Dating of the Meizuo Granite and Geological Significance in the Huanan Uplift,East Heilongjiang Province[J].Journal of Jilin University(Earth Science Edition),2008,38(4):631-638.
[35] JAHN B M.The Central Asian Orogenic Belt and Growth of the Continental Crust in the Phanerozoic[J].Geological Society,London,Special Publications,2004,226:73-100.
[36] WU F Y,ZHAO G C,SUN D Y,et al.The Hulan Group:Its Role in the Evolution of the Central Asian Orogenic Belt of NE China[J].Journal of Asian Earth Sciences,2007,30(3/4):542-556.
[37] ANDERSEN T.Correction of Common Lead in U-Pb Analyses That Do Not Report 204Pb[J].Chemical Geology,2002,192(1/2):59-79.
[38] LUDWIG K R.User's Manual for Isoplot 3.00:A Geochronological Toolkit for Microsoft Excel[R].Berkeley:Berkeley Geochronology Center,2003.
[39] 丛智超,孙丰月,王 冠,等.佳木斯地块中部岩浆岩锆石U-Pb年代学、地球化学及其大地构造意义[J].岩石学报,2016,32(4):1141-1152.
CONG Zhi-chao,SUN Feng-yue,WANG Guan,et al.Zircon U-Pb Age and Geochemistry of the Magmatic Rocks in the Jiamusi Massif,NE China and Their Tectonic Implications[J].Acta Petrologica Sinica,2016,32(4):1141-1152.
[40] SUN S S,MCDONOUGH W F,et al.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society,London,Special Publications,1989,42:313-345.
[41] XIE W,ZENG Q D,ZHOU L L,et al.Late Triassic Granitic Magmatism and Tungsten Mineralization in NE China:Geochronological and Geochemical Constraints from the Tantoushan Quartz-wolframite Vein-type Deposit[J].Journal of Geochemical Exploration,2022,241:107060.
[42] 王 涛,张建军,李 舢,等.东北亚晚古生代—中生代岩浆时空演化:多重板块构造体制范围及叠合的鉴别证据[J].地学前缘,2022,29(2):28-44.
WANG Tao,ZHANG Jian-jun,LI Shan,et al.Distinctive Spatial-temporal Evolution of Late Paleozoic to Mesozoic Magmatic Systems in Northeast Asia:Evidences for Identification of the Extent and Superposition of Multiple Plate Tectonic Regimes[J].Earth Science Frontiers,2022,29(2):28-44.
[43] 吴迪迪,李 舢,DAVID C,等.中亚造山带东南缘二叠纪—三叠纪花岗质岩浆演化对增生-碰撞过程的制约[J].中国科学:地球科学,2021,51(6):906-926.
WU Di-di,LI Shan,DAVID C,et al.Permian-Triassic Magmatic Evolution of Granitoids from the Southeastern Central Asian Orogenic Belt:Implications for Accretion Leading to Collision[J].Science China:Earth Sciences,2021,51(6):906-926.
[44] CHEN J S,TIAN D X,YANG H,et al.Triassic Granitic Magmatism at the Northern Margin of the North China Craton:Implications of Geochronology and Geochemistry for the Tectonic Evolution of the Central Asian Orogenic Belt[J].Acta Geologica Sinica(English Edition),2019,93(5):1325-1353.
[45] 许文良,孙晨阳,唐 杰,等.兴蒙造山带的基底属性与构造演化过程[J].地球科学,2019,44(5):1620-1646.
XU Wen-liang,SUN Chen-yang,TANG Jie,et al.Basement Nature and Tectonic Evolution of the Xing'an-Mengolian Orogenic Belt[J].Earth Science,2019,44(5):1620-1646.
[46] 周建波,石爱国,景 妍.东北地块群:构造演化与古大陆重建[J].吉林大学学报(地球科学版),2016,46(4):1042-1055.
ZHOU Jian-bo,SHI Ai-guo,JING Yan.The Combined NE China Blocks:Tectonic Evolution and Supercontinent Reconstructions[J].Journal of Jilin University(Earth Science Edition),2016,46(4):1042-1055.
[47] 周建波,蒲先刚,侯贺晟,等.东北中生代增生杂岩及对古太平洋向欧亚大陆俯冲历史的制约[J].岩石学报,2018,34(10):2845-2856.
ZHOU Jian-bo,PU Xian-gang,HOU He-sheng,et al.The Mesozoic Accretionary Complex in NE China and Its Tectonic Implications for the Subduction of the Paleo-Pacific Plate Beneath the Eurasia[J].Acta Petrologica Sinica,2018,34(10):2845-2856.
[48] ZHOU J B,CAO J L,WILDE S A,et al.Paleo-Pacific Subduction-accretion:Evidence from Geochemical and U-Pb Zircon Dating of the Nadanhada Accretionary Complex,NE China[J].Tectonics,2014,33(12):2444-2466.
[49] HAN W,ZHOU J B,WILDE S A,et al.LA-ICPMS Zircon U-Pb Dating of the Heilongjiang Complex in the Luobei Area:New Constraints for the Late Pa-laeozoic-Mesozoic Tectonic Evolution of Jiamusi Blo-ck,NE China[J].Geological Journal,2020,55(3):1644-1669.
[50] KAY R W.Aleutian Magnesian Andesites:Melts from Subducted Pacific Ocean Crust[J].Journal of Volca-nology and Geothermal Research,1978,4(1/2):117-132.
[51] DEFANT M J,DRUMMOND M S.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere[J].Nature,1990,347:662-665.
[52] 王 强,许继峰,赵振华,等.埃达克质岩的构造背景与岩石组合[J].矿物岩石地球化学通报,2008,27(4):344-350.
WANG Qiang,XU Ji-feng,ZHAO Zhen-hua,et al.Tectonic Setting and Associated Rock Suites of Adakitic Rocks[J].Bulletin of Mineralogy,Petrology and Geochemistry,2008,27(4):344-350.
[53] 许继峰,邬建斌,王 强,等.埃达克岩与埃达克质岩在中国的研究进展[J].矿物岩石地球化学通报,2014,33(1):6-13.
XU Ji-feng,WU Jian-bin,WANG Qiang,et al.Research Advances of Adakites and Adakitic Rocks in China[J].Bulletin of Mineralogy,Petrology and Geochemistry,2014,33(1):6-13.
[54] 张 旗,王 焰,钱 青,等.中国东部燕山期埃达克岩的特征及其构造-成矿意义[J].岩石学报,2001,17(2):236-244.
ZHANG Qi,WANG Yan,QIAN Qing,et al.The Cha-racteristics and Tectonic-metallogenic Significances of the Adakites in Yanshan Period from Eastern China[J].Acta Petrologica Sinica,2001,17(2):236-244.
[55] 张 旗,王 焰,刘 伟,等.埃达克岩的特征及其意义[J].地质通报,2002,21(7):431-435.
ZHANG Qi,WANG Yan,LIU Wei,et al.Adakite:Its Characteristics and Implications[J].Geological Bulletin of China,2002,21(7):431-435.
[56] 王 强,郝露露,张修政,等.汇聚板块边缘的埃达克质岩:成分和成因[J].中国科学:地球科学,2020,50(12):1845-1873.
WANG Qiang,HAO Lu-lu,ZHANG Xiu-zheng,et al.Adakitic Rocks at Convergent Plate Boundaries:Compositions and Petrogenesis[J].Science China:Earth Sciences,2020,50(12):1845-1873.
[57] 张 旗.埃达克岩研究的回顾和前瞻[J].中国地质,2008,35(1):32-39.
ZHANG Qi.Adakite Research:Retrospect and Pro-spect[J].Geology in China,2008,35(1):32-39.
[58] MARTIN H.Adakitic Magmas:Modern Analogues of Archaean Granitoids[J].Lithos,1999,46(3):411-429.
[59] 张宏飞,王 婧,徐旺春,等.俯冲陆壳部分熔融形成埃达克质岩浆[J].高校地质学报,2007,13(2):224-234.
ZHANG Hong-fei,WANG Jing,XU Wang-chun,et al.Derivation of Adakitic Magma by Partial Melting of Subducted Continental Crust[J].Geological Journal of China Universities,2007,13(2):224-234.
[60] GUO F,NAKAMURU E,FAN W M,et al.Generation of Palaeocene Adakitic Andesites by Magma Mixing; Yanji Area,NE China[J].Journal of Petrology,2007,48(4):661-692.
[61] 李 印,凌明星,丁 兴,等.中国东部埃达克岩及成矿作用[J].大地构造与成矿学,2009,33(3):448-464.
LI Yin,LING Ming-xing,DING Xing,et al.Adakites or Adakitic Rocks and Associated Metallogenesis in Eastern China[J].Geotectonica et Metallogenia,2009,33(3):448-464.
[62] 姜子琦,王 强,WYMAN D A,等.西藏冈底斯南缘冲木达约30 Ma埃达克质侵入岩的成因:向北俯冲的印度陆壳的熔融?[J].地球化学,2011,40(2):126-146.
JIANG Zi-qi,WANG Qiang,WYMAN D A,et al.Origin of ~30 Ma Chongmuda Adakitic Intrusive Rocks in the Southern Gangdese Region,Southern Tibet:Partial Melting of the Northward Subducted In-dian Continent Crust?[J].Geochimica,2011,40(2):126-146.
[63] 张 旗,钱 青,王二七,等.燕山中晚期的中国东部高原:埃达克岩的启示[J].地质科学,2001,36(2):248-255.
ZHANG Qi,QIAN Qing,WANG Er-qi,et al.An East China Plateau in Mid-Late Yanshanian Period:Implication from Adakites[J].Chinese Journal of Geology,2001,36(2):248-255.
[64] 赵永久,袁 超,周美夫,等.松潘甘孜造山带早侏罗世的后造山伸展:来自川西牛心沟和四姑娘山岩体的地球化学制约[J].地球化学,2007,36(2):139-152.
ZHAO Yong-jiu,YUAN Chao,ZHOU Mei-fu,et al.Post-orogenic Extension of Songpan-Garze Orogen in Early Jurassic:Constraints from Niuxingou Monzodiorite and Siguniangshan A-type Granite of Western Sichuan,China[J].Geochimica,2007,36(2):139-152.
[65] SYLVESTER P J.Post-collisional Strongly Peraluminous Granites[J].Lithos,1998,45(1/2/3/4):29-44.
[66] 周建波,曾维顺,曹嘉麟,等.中国东北地区的构造格局与演化:从500 Ma到180 Ma[J].吉林大学学报(地球科学版),2012,42(5):1298-1316,1329.
ZHOU Jian-bo,ZENG Wei-shun,CAO Jia-lin,et al.The Tectonic Framework and Evolution of the NE China from ~500 Ma to ~180 Ma[J].Journal of Jilin University(Earth Science Edition),2012,42(5):1298-1316,1329.
[67] YANG H,GE W C,DONG Y,et al.Permian Subduction of the Paleo-Pacific(Panthalassic)Oceanic Lithosphere Beneath the Jiamusi Block:Geochronological and Geochemical Evidence from the Luobei Mafic Intrusions in Northeast China[J].Lithos,2019,332/333:207-225.
[68] 张 旗,许继峰,王 焰,等.埃达克岩的多样性[J].地质通报,2004,23(增2):959-965.
ZHANG Qi,XU Ji-feng,WANG Yan,et al.Diversity of Adakite[J].Geological Bulletin of China,2004,23(S2):959-965.
[69] 李伟民,刘永江,TAKASU A,等.黑龙江依兰地区蓝片岩的变质演化P-T-t轨迹[J].岩石学报,2014,30(10):3085-3099.
LI Wei-min,LIU Yong-jiang,TAKASU A,et al.Pressure(P)-temperature(T)-time(t)Paths of the Blueschists from the Yilan Area,Heilongjiang Pro-vince[J].Acta Petrologica Sinica,2014,30(10):3085-3099.
[70] ZHU Y L,GAO R,ZHAO G C.Permian to Cretaceous Tectonic Evolution of the Jiamusi and Songliao Blocks in NE China:Transition from the Closure of the Paleo-Asian Ocean to the Subduction of the Paleo-Pacific Ocean[J].Gondwana Research,2022,103:371-388.
[71] 张兴洲,曾 振,高 锐,等.佳木斯地块与松嫩地块俯冲碰撞的深反射地震剖面证据[J].地球物理学报,2015,58(12):4415-4424.
ZHANG Xing-zhou,ZENG Zhen,GAO Rui,et al.The Evidence from the Deep Seismic Reflection Profile on the Subduction and Collision of the Jiamusi and Songnen Massifs in the Northeastern China[J].Chinese Journal of Geophysics,2015,58(12):4415-4424.
[72] 梁宏达,金 胜,魏文博,等.松嫩地块东缘和佳木斯地块西缘电性结构[J].地球物理学报,2017,60(4):1511-1520.
LIANG Hong-da,JIN Sheng,WEI Wen-bo,et al.Deep Electrical Structures of the Eastern Margin of the Songnen Massif and the Western Margin of the Jiamusi Massif[J].Chinese Journal of Geophysics,2017,60(4):1511-1520.
[73] 杨 浩,张彦龙,陈会军,等.兴凯湖花岗杂岩体的锆石U-Pb年龄及其地质意义[J].世界地质,2012,31(4):621-630.
YANG Hao,ZHANG Yan-long,CHEN Hui-jun,et al.Zircon U-Pb Ages of Khanka Lake Granitic Complex and Its Geological Implication[J].Global Geology,2012,31(4):621-630.
[74] WANG Y N,XU W L,WANG F,et al.Late Paleo-zoic-Mesozoic Tectonic Evolution of the Northeastern Asian Continental Margin Revealed by Sedimentary Formations and Fossil Accretionary Complexes[J].Earth-science Reviews,2022,225:103908.
[75] XU Z J,KONG J T,CHENG R H,et al.The Subduction of the Paleo-Pacific Plate to the Jiamusi Block:Evidence from the Early Mesozoic Sedimentary Rocks of the Eastern Jiamusi Block[J].Island Arc,2020,29(1):12364.
[76] 张 磊,李秋根,史兴俊,等.佳木斯地块中部二叠纪永清花岗闪长岩的锆石U-Pb年龄、地球化学特征及其地质意义[J].岩石矿物学杂志,2013,32(6):1022-1036.
ZHANG Lei,LI Qiu-gen,SHI Xing-jun,et al.Zircon U-Pb Age and Geochemistry of the Permian Yongqing Granodiorite Intrusion in Jiamusi Massif of Northeast China and Their Implications[J].Acta Petrologica et Mineralogica,2013,32(6):1022-1036.
[77] 赵立国,王建民,王 磊,等.黑龙江省东部依兰地区金沟花岗岩的锆石U-Pb定年及其地质意义[J].地质与资源,2016,25(5):436-442.
ZHAO Li-guo,WANG Jian-min,WANG Lei,et al.Zircon U-Pb Dating and Geological Implication of the Jingo Granite in Yilan Area,Eastern Heilongjiang Province[J].Geology and Resources,2016,25(5):436-442.
[78] 王建民,颜秉超.黑龙江省东部佳木斯地区八角山岩体形成时代探讨[J].吉林地质,2020,39(3):65-71.
WANG Jian-min,YAN Bing-chao.Discussion on the Age of Bajiaoshan Pluton in Jiamusi Area,Eastern Heilongjiang Province[J].Jilin Geology,2020,39(3):65-71.
[79] 吴福元,WILDE S A,孙德有.佳木斯地块片麻状花岗岩的锆石离子探针U-Pb年龄[J].岩石学报,2001,17(3):443-452.
WU Fu-yuan,WILDE S A,SUN De-you.Zircon SH-RIMP U-Pb Ages of Gneissic Granites in Jiamusi Massif,Northeastern China[J].Acta Petrologica Sinica,2001,17(3):443-452.
[80] 毕君辉,葛文春,张彦龙,等.佳木斯地块东部二叠纪锦山花岗杂岩体的成因及其地质意义[J].地球科学与环境学报,2014,36(4):16-31.
BI Jun-hui,GE Wen-chun,ZHANG Yan-long,et al.Petrogenesis of Permian Jinshan Granitic Complex in the Eastern Jiamusi Massif and Its Geological Implications[J].Journal of Earth Sciences and Environment,2014,36(4):16-31.
[81] 孟 恩,许文良,杨德彬,等.佳木斯地块东缘及东南缘二叠纪火山作用:锆石U-Pb年代学、地球化学及其构造意义[J].科学通报,2008,53(8):956-965.
MENG En,XU Wen-liang,YANG De-bin,et al.Permian Volcanisms in Eastern and Southeastern Margins of the Jiamusi Massif,Northeastern China:Zircon U-Pb Chronology,Geochemistry and Its Tectonic Implications[J].Chinese Science Bulletin,2008,53(8):956-965.
[82] CHU Y,LIN W,FAURE M,et al.Cretaceous Episodic Extension in the South China Block,East Asia:Evidence from the Yuechengling Massif of Central South China[J].Tectonics,2019,38(10):3675-3702.
[83] 于介江,侯雪刚,葛文春,等.佳木斯地块东北缘早二叠世六连岩体的岩浆混合成因:岩相学、年代学和地球化学证据[J].岩石学报,2013,29(9):2971-2986.
YU Jie-jiang,HOU Xue-gang,GE Wen-chun,et al.Magma Mixing Genesis of the Early Permian Liulian Pluton at the Northeastern Margin of the Jiamusi Massif in NE China:Evidences from Petrography,Geochronology and Geochemistry[J].Acta Petrologica Sinica,2013,29(9):2971-2986.
[84] 蒲建彬,张兴洲,郭 冶,等.佳木斯地块东部二叠纪方山花岗岩体的锆石U-Pb年代学、地球化学特征及其地质意义[J].世界地质,2015,34(4):903-913.
PU Jian-bin,ZHANG Xing-zhou,GUO Ye,et al.Geological Implications of Permian Fangshan Granitic Rocks in Eastern Jiamusi Massif:Evidences from U-Pb Chronology and Geochemistry[J].Global Geology,2015,34(4):903-913.
[85] 张 旗,王 焰,李承东,等.花岗岩的Sr-Yb分类及其地质意义[J].岩石学报,2006,22(9):2249-2269.
ZHANG Qi,WANG Yan,LI Cheng-dong,et al.Gra-nite Classification on the Basis of Sr and Yb Contents and Its Implications[J].Acta Petrologica Sinica,2006,22(9):2249-2269.

相似文献/References:

[1]杨晓勇,古黄玲,严志忠,等.安徽贵池地区燕山期岩浆岩与铜金钼成矿关系:来自地质-地球化学-地球物理证据[J].地球科学与环境学报,2016,38(04):444.
 YANG Xiao-yong,GU Huang-ling,YAN Zhi-zhong,et al.Metallogenic Relationship Between Yanshanian Magmatic Rocks and Cu-Au-Mo Deposits in Guichi Area of Anhui: Evidences from Geological-geochemical-geophysical Characteristics[J].Journal of Earth Sciences and Environment,2016,38(02):444.
[2]李沛刚,王登红,雷志远,等.贵州大竹园大型铝土矿稀土元素地球化学特征及其意义[J].地球科学与环境学报,2012,34(02):31.
 LI Pei-gang,WANG Deng-hong,LEI Zhi-yuan,et al.Geochemical Characteristic of Rare Earth Element in Dazhuyuan Large-scale Bauxite Deposit of Guizhou Province and Its Significance[J].Journal of Earth Sciences and Environment,2012,34(02):31.
[3]王永,周赤华,姚培毅,等.内蒙古中部必鲁图晚更新世晚期环境演变的沉积记录[J].地球科学与环境学报,2012,34(03):62.
 WANG Yong,ZHOU Chi-hua,YAO Pei-yi,et al.Sedimentary Record of Environmental Evolution Since Late Stage of Late Pleistocene in Bilutu of Central Inner Mongolia[J].Journal of Earth Sciences and Environment,2012,34(02):62.
[4]闫盼盼,梁婷*,徐生发,等.皖南竹溪岭花岗闪长岩的岩浆源区:来自矿物学、地球化学证据[J].地球科学与环境学报,2019,41(02):141.
 YAN Pan-pan,LIANG Ting*,XU Sheng-fa,et al.Tracer Origin of Zhuxiling Granodiorite in the Southern Anhui, China: Evidence from Mineralogical and Geochemical Characteristics[J].Journal of Earth Sciences and Environment,2019,41(02):141.
[5]毛龙江,郭爱鹏,杜吉净,等.湖南澧水下游表层沉积物稀土元素特征[J].地球科学与环境学报,2019,41(03):352.
 MAO Long-jiang,GUO Ai-peng,DU Ji-jing,et al.REE Characteristics of the Surface Sediments in the Lower Reaches of Lishui River, Hunan, China[J].Journal of Earth Sciences and Environment,2019,41(02):352.
[6]李强,杨富全*,杨成栋.新疆阿尔泰大喀拉苏花岗岩年代学、地球化学特征及其构造意义[J].地球科学与环境学报,2019,41(04):396.
 LI Qiang,YANG Fu-quan*,YANG Cheng-dong.Geochronology and Geochemical Characteristics of Dakalasu Granite in Altay of Xinjiang, China and Their Tectonic Significance[J].Journal of Earth Sciences and Environment,2019,41(02):396.
[7]马涛,鲁有朋,代俊峰*,等.西秦岭多哇地区萨日加岩体LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义[J].地球科学与环境学报,2020,42(02):231.[doi:10.19814/j.jese.2019.10052]
 MA Tao,LU You-peng,DAI Jun-feng*,et al.LA-ICP-MS Zircon U-Pb Ages and Geochemical Characteristics of Sarijia Intrusion in Duowa Area of West Qinling, China and Their Geological Implications[J].Journal of Earth Sciences and Environment,2020,42(02):231.[doi:10.19814/j.jese.2019.10052]
[8]陈贵民,刘俊辰,王义天*,等.西昆仑苏纳克早古生代花岗岩锆石U-Pb年龄、地球化学特征及其地质意义[J].地球科学与环境学报,2020,42(04):427.[doi:10.19814/j.jese.2020.03026]
 CHEN Gui-min,LIU Jun-chen,WANG Yi-tian*,et al.Zircon U-Pb Dating and Geochemical Characteristics of Early Paleozoic Granite in the Southern Sunake of West Kunlun, Northwest China and Their Geological Significances[J].Journal of Earth Sciences and Environment,2020,42(02):427.[doi:10.19814/j.jese.2020.03026]
[9]周北昱,李盼,曾雯*,等.湖北峡东地区奥陶系南津关组灰岩中硅质岩地球化学特征及其沉积环境意义[J].地球科学与环境学报,2020,42(04):464.[doi:10.19814/j.jese.2020.01028]
 ZHOU Bei-yu,LI Pan,ZENG Wen*,et al.Geochemistry Characteristics of Cherts from Ordovician Nanjinguan Formation Limestone in the Eastern Yangtze Gorges Area of Hubei, China and Their Implications for Sedimentary Environment[J].Journal of Earth Sciences and Environment,2020,42(02):464.[doi:10.19814/j.jese.2020.01028]
[10]封铿,李瑞保*,裴先治,等.东昆仑造山带东段大格勒花岗岩锆石U-Pb年代学、地球化学特征及其构造意义[J].地球科学与环境学报,2020,42(04):442.[doi:10.19814/j.jese.2020.05009]
 FENG Keng,LI Rui-bao*,PEI Xian-zhi,et al.Zircon U-Pb Dating and Geochemical Characteristics of Dagele Granite in the Eastern Margin of East Kunlun Orogenic Belt, China and Their Tectonic Implications[J].Journal of Earth Sciences and Environment,2020,42(02):442.[doi:10.19814/j.jese.2020.05009]

备注/Memo

备注/Memo:
收稿日期:2022-02-10; 修回日期:2022-08-27
基金项目:黑龙江省财政拨款项目(HLJKD2015-28); 国家自然科学基金项目(41662009)
作者简介:赵 强(1992-),男,黑龙江龙江人,合肥工业大学理学博士研究生,E-mail:hljzq2020@163.com。
*通讯作者:汤静如(1977-),男,湖北监利人,教授,理学博士,E-mail:tjr118@glut.edu.cn。
更新日期/Last Update: 2023-05-20