必须声明标量变量 "@Script_ID"。 安徽庐枞盆地黄屯地区岩浆侵入活动时限及元素地球化学特征-《地球科学与环境学报》
|本期目录/Table of Contents|

[1]张靖怡,张 舒*,张赞赞,等.安徽庐枞盆地黄屯地区岩浆侵入活动时限及元素地球化学特征[J].地球科学与环境学报,2020,42(05):584-602.[doi:10.19814/j.jese.2020.05030]
 ZHANG Jing-yi,ZHANG Shu*,ZHANG Zan-zan,et al.Geochronology and Geochemistry Characteristics of Magmatic Intrusive Rocks in Huangtun Area of Luzong Basin, Anhui, China[J].Journal of Earth Sciences and Environment,2020,42(05):584-602.[doi:10.19814/j.jese.2020.05030]
点击复制

安徽庐枞盆地黄屯地区岩浆侵入活动时限及元素地球化学特征(PDF)
分享到:

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

卷:
第42卷
期数:
2020年第05期
页码:
584-602
栏目:
基础地质与矿产地质
出版日期:
2020-09-15

文章信息/Info

Title:
Geochronology and Geochemistry Characteristics of Magmatic Intrusive Rocks in Huangtun Area of Luzong Basin, Anhui, China
文章编号:
1672-6561(2020)05-0584-19
作者:
张靖怡12张 舒123*张赞赞12蔡晓兵12岳运华12魏国辉12
1. 安徽省地质调查院,安徽 合肥 230001; 2. 安徽省地质科学研究所,安徽 合肥 230001; 3. 合肥工业大学土木与水利工程学院,安徽 合肥 230009
Author(s):
ZHANG Jing-yi12 ZHANG Shu123* ZHANG Zan-zan12 CAI Xiao-bing12 YUE Yun-hua12 WEI Guo-hui12
1. Geological Survey of Anhui Province, Hefei 230001, Anhui, China; 2. Anhui Institute of Geological Sciences, Hefei 230001, Anhui, China; 3. College of Civil Engineering, Hefei University of Technology, Hefei 230009, Anhui, China
关键词:
地球化学 岩浆岩 锆石U-Pb年龄 演化机制 岩石成因 侵入岩 庐枞盆地 安徽
Keywords:
geochemistry magmatic rock zircon U-Pb age evolution mechanism petrogenesis intrusive rock Luzong Basin Anhui
分类号:
P581; P595; P597
DOI:
10.19814/j.jese.2020.05030
文献标志码:
A
摘要:
庐枞矿集区是长江中下游成矿带重要的铜铁多金属矿集区之一,近期勘查工作在矿集区北部的黄屯地区取得找矿突破,发现了数个与岩浆侵入活动有关的铅锌铜金矿床。对安徽庐枞盆地黄屯地区的侵入岩开展了较为系统的LA-ICP-MS锆石U-Pb定年及全岩地球化学分析,旨在确定黄屯地区岩浆侵入活动时限和揭示岩浆演化过程。结合前人年代学数据及侵入体之间的接触关系,明确黄屯闪长玢岩最早侵位(135.0~134.4 Ma),岳山二长斑岩次之(132.7~132.1 Ma),焦冲正长岩最晚形成(131.5~129.6 Ma),均属于庐枞盆地内部砖桥旋回末期岩浆侵入活动的产物。黄屯地区的侵入岩具有Si近饱和、富Al、高碱、富K、低Ti的特征,富集Rb、K等大离子亲石元素,亏损Nb、Ta等高场强元素,为典型的橄榄玄粗岩系列。结合Sr-Nd同位素特征,推测岩浆源区可能为富集型扬子板块岩石圈地幔。主量、微量元素的演化趋势显示,矿物分离结晶作用控制了本区岩浆演化过程,从闪长质岩浆至二长质岩浆主要发生角闪石的分离结晶作用,而从二长质岩浆至正长质岩浆则主要发育斜长石的分离结晶作用。
Abstract:
Luzong ore district located at northern margin of Yangtze block is one of important iron-copper polymetallic ore districts in the middle-lower Yangtze river metallogenic belt. The porphyry-type iron and copper deposits are the dominant types in Luzong ore district. Recently, several medium-sized lead-zinc-copper-gold deposits, which are genetically related with regional magmatic intrusive rocks, are discovered in Huangtun area, the northern margin of Luzong Basin, Anhui. Petrological observations, LA-ICP-MS zircon U-Pb dating and geochemical analysis were carried out for intrusive rocks in Huangtun area with the aims to determine the temporal framework of magmatic intrusions and to reveal the magmatic evolution process. Huangtun dioritic porphyrite, Yueshan monzonitic and Jiaochong syenitic intrusive rocks form at 135.0-134.4, 132.7-132.1 and 131.5-129.6 Ma, respectively, which belong to the products of intrusive magmatism at the end of Zhuanqiao volcanic cycle in Luzong Basin. The intrusive rocks in Huangtun area are characterized by high SiO2(mean content is 61.67%), Al2O3(16.95%), alkaline(10.25%)and low TiO2(0.66%), enriched in large ion lithophile elements such as Rb, K as well as light rare earth elements, and depleted in high strength field elements such as Nb and Ta. Geochemical features suggest that the intrusive rocks belong to typical shoshonite series. Combined with Sr-Nd isotopic compositions, the primary magma is probably derived from enriched lithospheric mantle of Yangtze block. Geochemical variations reveal that fractional crystallization controls the evolution process of the magma, during which the fractionation of hornblende dominates the differentiation from diorite to monzonite, and plagioclase dominates the fractional crystallization from monzonite to syenite.

参考文献/References:

[1] 常印佛,刘湘培,吴言昌.长江中下游铜铁成矿带[M].北京:地质出版社,1991.
CHANG Yin-fo,LIU Xiang-pei,WU Yan-chang.The Copper-iron Belt of the Lower and Middle Reaches of the Changjiang River[M].Beijing:Geological Publishing House,1991.
[2] 翟裕生,姚书振,林新多,等.长江中下游地区铁铜(金)成矿规律[M].北京:地质出版社,1992.
ZHAI Yu-sheng,YAO Shu-zhen,LIN Xin-duo,et al.Fe-Cu-Au Metallogenic Regularity of the Middle-lower Changjiang River[M].Beijing:Geological Publishing House,1992.
[3] ZHOU T F,WANG S W,FAN Y,et al.A Review of the Intracontinental Porphyry Deposits in the Middle-lower Yangtze River Valley Metallogenic Belt,Eastern China[J].Ore Geology Reviews,2015,65:433-456.
[4] 周涛发,范 裕,王世伟,等.长江中下游成矿带成矿规律和成矿模式[J].岩石学报,2017,33(11):3353-3372.
ZHOU Tao-fa,FAN Yu,WANG Shi-wei,et al.Metallogenic Regularity and Metallogenic Model of the Middle-lower Yangtze River Valley Metallogenic Belt[J].Acta Petrologica Sinica,2017,33(11):3353-3372.
[5] LIU Y N,FAN Y,ZHOU T F,et al.Geochemical Characteristics of Pyrite in the Dabaozhuang Deposit in the Middle-lower Yangtze River Metallogenic Belt,Eastern China[J].Ore Geology Reviews,2020,124:103662.
[6] LIU Y N,FAN Y,ZHOU T F,et al.In-situ LA-ICP-MS Trace Element Analysis of Magnetite from Mesozoic Iron Oxide Apatite(IOA)Deposits in the Luzong Volcanic Basin,Eastern China[J].Journal of Asian Earth Sciences,2018,166:233-246.
[7] 赵新福,曾丽平,廖 旺,等.长江中下游成矿带玢岩铁矿研究新进展及对矿床成因的启示[J].地学前缘,2020,27(2):197-217.
ZHAO Xin-fu,ZENG Li-ping,LIAO Wang,et al.An Overview of Recent Advances in Porphyrite Iron(Iron Oxide-apatite,IOA)Deposits in the Middle-lower Yangtze River Valley Metallogenic Belt and Its Implication for Ore Genesis[J].Earth Science Frontiers,2020,27(2):197-217.
[8] 葛宁洁,李 平,黄宪安,等.安徽庐江岳山银铅锌矿的成矿物质来源及物理化学条件探讨[J].中国科学技术大学学报,1989,19(3):365-374.
GE Ning-jie,LI Ping,HUANG Xian-an,et al.Research on Physical Chemistry Condition and Materials Source of Mineralization of Ag-Pb-Zn Ore Deposit in Yueshan[J].Journal of China University of Science and Techonolgy,1989,19(3):365-374.
[9] 张 矿,许强平.安徽铜盘山—岳山地区铅锌矿地质特征及找矿方向[J].安徽地质,2019,29(2):94-97.
ZHANG Kuang,XU Qiang-ping.Geological Features and Prospecting Direction of Lead and Zinc Deposits in the Tongpanshan-Yueshan Area,Anhui Province[J].Geology of Anhui,2019,29(2):94-97.
[10] 蔡晓兵,汪 晶,岳云华.安徽省庐江县朱岗铅锌矿床地质特征及找矿方向[J].安徽地质,2015,25(3):161-166.
CAI Xiao-bing,WANG Jing,YUE Yun-hua.Geological Features of the Zhugang Pb-Zn Ore Deposit and Ore-prospecting Direction in Lujiang County,Anhui Pro-vince[J].Geology of Anhui,2015,25(3):161-166.
[11] WANG B,ZHOU T F,FAN Y,et al.Breccia,Hydrothermal Alteration and Structural Geology of the Huangtun Porphyry Au-Cu Deposit in the Middle-lower Yangtze Metallogenic Belt,Eastern China[J].Ore Geology Reviews,2020,120:103414.
[12] 张燕群.安徽西湾铅锌矿床地球化学特征及矿床成因探讨[D].南昌:东华理工大学,2019.
ZHANG Yan-qun.Research on the Geochemical Characteristics and Genesis of the Xiwan Lead-zinc Deposit in Anhui Province[D].Nanchang:East China University of Techonogy,2019.
[13] 周涛发,范 裕,袁 峰,等.安徽庐枞(庐江—枞阳)盆地火山岩的年代学及其意义[J].中国科学:D辑,地球科学,2008,38(11):1342-1353.
ZHOU Tao-fa,FAN Yu,YUAN Feng,et al. Geochronology of the Volcanic Rocks in Lu-Zong Basin and Its Significance[J].Science in China:Series D,Earth Science,2008,38(11):1342-1353.
[14] 周涛发,范 裕,袁 峰,等.庐枞盆地侵入岩的时空格架及其对成矿的制约[J].岩石学报,2010,26(9):2694-2714.
ZHOU Tao-fa,FAN Yu,YUAN Feng,et al.Temporal-spatial Framework of Magmatic Intrusions in Luzong Volcanic Basin in East China and Their Constrain to Mineralization[J].Acta Petrologica Sinica,2010,26(9):2694-2714.
[15] 周涛发,范 裕,袁 峰.长江中下游成矿带成岩成矿作用研究进展[J].岩石学报,2008,24(8):1665-1678.
ZHOU Tao-fa,FAN Yu,YUAN Feng.Advances on Petrogensis and Metallogeny Study of the Mineralization Belt of the Middle and Lower Reaches of the Yangtze River Area[J].Acta Petrologica Sinica,2008,24(8):1665-1678.
[16] 周涛发,范 裕,袁 峰,等.长江中下游成矿带火山岩盆地的成岩成矿作用[J].地质学报,2011,85(5):712-730.
ZHOU Tao-fa,FAN Yu,YUAN Feng,et al.Petrogensis and Metallogeny Study of the Volcanic Basins in the Middle and Lower Yangtze Metallogenic Belt[J].Acta Geologica Sinica,2011,85(5):712-730.
[17] 袁 峰,周涛发,范 裕,等.庐枞盆地中生代火山岩的起源、演化及形成背景[J].岩石学报,2008,24(8):1691-1702.
YUAN Feng,ZHOU Tao-fa,FAN Yu,et al.Source,Evolution and Tectonic Setting of Mesozoic Volcanic Rocks in Luzong Basin,Anhui Province[J].Acta Petrologica Sinica,2008,24(8):1691-1702.
[18] 周涛发,宋明义,范 裕,等.安徽庐枞盆地中巴家滩岩体的年代学研究及其意义[J].岩石学报,2007,23(10):2379-2386.
ZHOU Tao-fa,SONG Ming-yi,FAN Yu,et al.Chronology of the Bajiatan Intrusion in the Luzong Basin,Anhui,and Its Significance[J].Acta Petrologica Sinica,2007,23(10):2379-2386.
[19] TANG M,WANG X L,XU X S,et al.Neoproterozoic Subducted Materials in the Generation of Mesozoic Luzong Volcanic Rocks:Evidence from Apatite Geochemistry and Hf-Nd Isotopic Decoupling[J].Gondwana Research,2012,21(1):266-280.
[20] XUE H M,MA F,CAO G Y.Geochronology and Petrogenesis of Shoshonitic Igneous Rocks,Luzong Volcanic Basin,Middle and Lower Yangtze River Reaches,China[J].Journal of Asian Earth Sciences,2015,110:123-140.
[21] CHEN L,ZHAO Z F,ZHENG Y F.Origin of Andesitic Rocks:Geochemical Constraints from Mesozoic Volcanics in the Luzong Basin,South China[J].Lithos,2014,190/191:220-239.
[22] WANG Q,WYMAN D A,XU J F,et al.Petrogenesis of Cretacous Adakitic and Shoshonitic Igneous Rocks in the Luzong Area,Anhui Province(Eastern China):Implications for Geodynamics and Cu-Au Mineralization[J].Lithos,2006,89(3/4):424-446.
[23] 陈 龙,郑永飞.长江中下游中生代安山质火山岩记录的新元古代大洋板片-地幔相互作用[J].地球科学,2019,44(12):4144-4151.
CHEN Long,ZHENG Yong-fei.Neoproterozoic Ocea-nic Slab-mantle Interaction:Geochemical Evidence from Mesozoic Andesitic Rocks in the Middle and Lower Yangtze Valley[J].Earth Science,2019,44(12):4144-4151.
[24] 任启江,王德滋,徐兆文,等.安徽庐枞火山-构造洼地的形成、演化及成矿[J].地质学报,1993,67(2):131-145.
REN Qi-jiang,WANG De-zi,XU Zhao-wen,et al.Formation and Development of the Mesozoic Lujiang-Zongyang Volcanic-structural Depression in Anhui Province and Their Relation to Mineralization[J].Acta Geologica Sinica,1993,67(2):131-145.
[25] 徐晓春,安昱华,许心悦,等.安徽南陵-宣城地区岩浆岩锆石U-Pb年龄及元素地球化学特征[J].地球科学与环境学报,2020,42(1):15-35.
XU Xiao-chun,AN Yu-hua,XU Xin-yue,et al.Zircon U-Pb Ages and Element Geochemistry Characteristics of Magmatic Rocks in Nanling-Xuancheng Area of Anhui,China[J].Journal of Earth Sciences and Environment,2020,42(1):15-35.
[26] 张赞赞,吴明安,杜建国,等.庐枞矿集区与钨矿床有关的花岗岩的年代学及地球化学特征:岩石成因及其对长江中下游晚白垩世成矿的启示[J].岩石学报,2018,34(1):217-240.
ZHANG Zan-zan,WU Ming-an,DU Jian-guo,et al.Geochronology and Geochemistry of the Tungsten Deposit-related Granites in the Luzong Orefield:Petrogensis and Insights for Late Cretaceous Metallogeny in the Middle and Lower Reaches of Yangtze River Metallogenic Belt[J].Acta Petrologica Sinica,2018,34(1):217-240.
[27] 吕庆田,刘振东,汤井田,等.庐枞矿集区上地壳结构与变形:综合地球物理探测结果[J].地质学报,2014,88(4):447-465.
LV Qing-tian,LIU Zhen-dong,TANG Jing-tian,et al.Upper Crustal Structure and Deformation of Lu-Zong Ore District:Constraints from Integrated Geophysical Data[J].Acta Geologica Sinica,2014,88(4):447-465.
[28] 张 舒,周涛发,吴明安,等.长江中下游成矿带庐枞盆地科学深钻中侵入岩年代学及地球化学研究[J].地质学报,2017,91(7):1483-1505.
ZHANG Shu,ZHOU Tao-fa,WU Ming-an,et al.Geochronology and Petrological Geochemistry of Intrusions in the Lujiang-Zongyang Basin in the Mineralization Belt of the Middle and Lower Reaches of Yangtze River Revealed by Scientific Drilling[J].Acta Geolo-gica Sinica,2017,91(7):1483-1505.
[29] 张 舒,吴明安,赵文广,等.安徽庐江泥河铁矿矿床地球化学特征及其对成因的制约[J].岩石学报,2014,30(5):1382-1396.
ZHANG Shu,WU Ming-an,ZHAO Wen-guang,et al.Geochemistry Characteristics of Nihe Iron Deposit in Lujiang,Anhui Province and Their Constrains to Ore Genesis[J].Acta Petrologica Sinica,2014,30(5):1382-1396.
[30] 宁芜研究项目编写小组.宁芜玢岩铁矿[M].北京:地质出版社,1978.
Group of Ningwu Research Project.The Porphyrite Iron Deposit of Ningwu[M].Beijing:Geological Publishing House,1978.
[31] 覃永军,曾键年,王思源,等.安徽庐枞盆地井边铜(金)矿床成矿特征及控矿地质因素探讨[J].矿床地质,2010,29(5):915-930.
QIN Yong-jun,ZENG Jian-nian,WANG Si-yuan,et al.Metallogenic Characteristics and Ore-control Factors of Jingbian Copper(Gold)Deposit in Luzong Basin,Anhui Province[J].Mineral Deposits,2010,29(5):915-930.
[32] 张乐骏,周涛发,范 裕,等.安徽庐枞盆地井边铜矿床的成矿时代及其找矿指示意义[J].岩石学报,2010,26(9):2729-2738.
ZHANG Le-jun,ZHOU Tao-fa,FAN Yu,et al.Dating of Copper Mineralization in Jingbian Deposit and Its Prospecting Significance in Luzong Basin,Anhui Province[J].Acta Petrologica Sinica,2010,26(9):2729-2738.
[33] 李怀坤,朱士兴,相振群,等.北京延庆高于庄组凝灰岩的锆石U-Pb定年研究及其对华北北部中元古界划分新方案的进一步约束[J].岩石学报,2010,26(7):2131-2140.
LI Huai-kun,ZHU Shi-xing,XIANG Zhen-qun,et al.Zircon U-Pb Dating on Tuff Bed from Gaoyuzhuang Formation in Yanqing,Beijing:Further Constrains on the New Subdivision of the Mesoproterozoic Stratigraphy in the Northern North China Craton[J].Acta Petrologica Sinica,2010,26(7):2131-2140.
[34] LIU Y S,GAO S,HU Z C,et al.Continental and Ocea-nic Crust Recycling-induced Melt-peridotite Interactions in the Trans-North China Orogen:U-Pb Dating,Hf Isotopes and Trace Elements in Zircons of Mantle Xenoliths[J].Journal of Petrology,2010,51(1/2):537-571.
[35] LUDWIG K R.Mathematical-statistical Treatment of Data and Errors for 230Th/U Geochronology[J].Reviews in Mineralogy and Geochemistry,2003,52(1):631-656.
[36] 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 Yuan-bao,ZHENG Yong-fei.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age[J].Chinese Science Bulletin,2004,49(16):1589-1604.
[37] VAVRA G,GEBAUER D,SCHMID R.Multiple Zircon Growth and Recrystallization During Polyphase Late Carboniferous to Triassic Metamorphism in Granulites of the Ivrea Zone(Southern Alps):An Ion Microprobe(SHRIMP)Study[J].Contributions to Mineralogy and Petrology,1996,122:337-358.
[38] WILSON M.Igneous Petrogenesis,A Global Tectonic Approach[M].New York:Oxford University Press,1989.
[39] MIDDLEMOST E A K.Naming Materials in the Magma/Igneous Rock System[J].Earth-science Reviews,1994,37(3/4):215-224.
[40] 李玉松,蔡晓兵,汪 晶,等.安徽庐枞盆地黄寅冲铅锌矿床闪长玢岩锆石U-Pb年龄及其地质意义[J].华东地质,2016,37(1):19-27.
LI Yu-song,CAI Xiao-bing,WANG Jing,et al.Zircon U-Pb Age of Diorite-porphyrites of the Huangyinchong Zn-Pb Deposit in the Luzong Basin,Anhui Province and Its Geological Implications[J].East China Geology,2016,37(1):19-27.
[41] 薛怀民,董树文,马 芳.长江中下游地区庐(江)—枞(阳)和宁(南京)—芜(湖)盆地内与成矿有关潜火山岩体的SHRIMP锆石U-Pb年龄[J].岩石学报,2010,26(9):2653-2664.
XUE Huai-min,DONG Shu-wen,MA Fang.Zircon U-Pb SHRIMP Ages of Sub-volcanic Bodies Related with Porphyritic Fe-deposits in the Luzong and Ningwu Basins,Middle and Lower Yangtze River Reaches,Central China[J].Acta Petrologica Sinica,2010,26(9):2653-2664.
[42] 贾丽琼,徐文艺,吕庆田,等.庐枞盆地砖桥地区科学深钻岩浆岩LA-MC-ICP MS锆石U-Pb年代学和岩石地球化学特征[J].岩石学报,2014,30(4):995-1016.
JIA Li-qiong,XU Wen-yi,LV Qing-tian,et al.LA-MC-ICP MS Zircon U-Pb Geochronology and Petrological Geochemistry of Scientific Drilling in Zhuanqiao,Lujiang-Zongyang Volcanic Basin[J].Acta Pe-trologica Sinica,2014,30(4):995-1016.
[43] 范 裕,邱 宏,周涛发,等.安徽庐枞盆地隐伏侵入岩的LA-ICP MS定年及其构造意义[J].地质学报,2014,88(4):532-546.
FAN Yu,QIU Hong,ZHOU Tao-fa,et al.LA-ICP MS Zircon U-Pb Dating for the Hidden Intrusions in the Lu-Zong Basin and Its Tectonic Significance[J].Acta Geologica Sinica,2014,88(4):532-546.
[44] 于学元,白正华.庐枞地区安粗岩系[J].地球化学,1981,10(1):57-65.
YU Xue-yuan,BAI Zheng-hua.Latitic Series in Lujiang-Zongyang Region[J].Geochimica,1981,10(1):57-65.
[45] 吴利仁,齐进英,王听渡,等.中国东部中生代火山岩[J].地质学报,1982,56(3):223-234.
WU Li-ren,QI Jin-ying,WANG Ting-du,et al.Mesozoic Volcanic Rocks in the Eastern Part of China[J].Acta Geologica Sinica,1982,56(3):223-234.
[46] 杨荣勇,任启江,徐兆文,等.安徽庐枞地区巴家滩火山-侵入岩体的岩浆来源[J].地球化学,1993,22(2):97-106.
YANG Rong-yong,REN Qi-jiang,XU Zhao-wen,et al.The Magma Source of Bajiatan Volcanic-intrusive Complex in the Lujiang-Zongyang Area,Anhui Pro-vince[J].Geochimica,1993,22(2):97-106.
[47] 薛怀民,董树文,马 芳.安徽庐枞火山岩盆地橄榄玄粗岩系的地球化学特征及其对下扬子地区晚中生代岩石圈减薄机制的约束[J].地质学报,2010,84(5):664-681.
XUE Huai-min,DONG Shu-wen,MA Fang.Geochemi-stry of Shoshonitic Volcanic Rocks in the Luzong Basin,Anhui Province(Eastern China):Constraints on Cretaceous Lithopheric Thinning of the Lower Yangtze Region[J].Acta Geologica Sinica,2010,84(5):664-681.
[48] MORRISON G W.Characteristics and Tectonic Setting of the Shoshonite Rock Association[J].Lithos,1980,13(1):97-108.
[49] GILL R C O,APARICIO A,EL AZZOUZI M,et al.Depleted Arc Volcanism in the Alboran Sea and Sho-shonitic Volcanism in Morocco:Geochemical and Isotopic Constraints on Neogene Tectonic Processes[J].Lithos,2004,78(4):363-388.
[50] LIEGEOIS J P,NAVEZ J,HERTOGEN J,et al.Constrasting Origin of Post-collisional High-K Calcalkaline and Shoshonitic Versus Alkaline and Peralkaline Granitoids:The Use of Sliding Normalization[J].Lithos,1998,45(1/2/3/4):1-28.
[51] SUN S S,MCDONOUGH W F.Chemical and Isoto-pic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society,London,Special Publications,1989,42:313-345.
[52] 陈江峰,郭新生,汤加富,等.中国东南地壳增长与Nd同位素模式年龄[J].南京大学学报(自然科学),1999,35(6):649-658.
CHEN Jiang-feng,GUO Xin-sheng,TANG Jia-fu,et al.Nd Isotopic Model Ages:Implications of the Growth of the Continental Crust of Southeastern China[J].Journal of Nanjing University(Natural Sciences),1999,35(6):649-658.
[53] 吴福元,孙德有.中国东部中生代岩浆作用与岩石圈减薄[J].长春科技大学学报,1999,29(4):313-318.
WU Fu-yuan,SUN De-you.The Mesozoic Magmatism and Lithospheric Thinning in Eastern China [J].Journal of Changchun University of Science and Technology,1999,29(4):313-318.
[54] 吴福元,葛文春,孙德有,等.中国东部岩石圈减薄研究中的几个问题[J].地学前缘,2003,10(3):51-60.
WU Fu-yuan,GE Wen-chun,SUN De-you.Discussions on the Lithospheric Thinning in Eastern China[J].Earth Science Frontiers,2003,10(3):51-60.
[55] 邓晋福,莫宣学,赵海玲,等.中国东部岩石圈根/去根作用与大陆“活化”[J].现代地质,1994,8(3):349-356.
DENG Jin-fu,MO Xuan-xue,ZHAO Hai-ling,et al.Lithosphere Root/De-rooting and Activation of the East China Continent[J].Geoscience,1994,8(3):349-356.
[56] LV Q T,YAN J Y,SHI D N,et al.Reflection Seismic Imaging of the Lujiang-Zongyang Volcanic Basin,Yangtze Metallogenic Belt:An Insight into the Crustal Structure and Geodynamics of an Ore District[J].Tectonophysics,2013,606:60-77.

相似文献/References:

[1]高林,陈斌.鲁西地块济南辉长岩岩石学、地球化学和Os-Nd-Sr同位素研究[J].地球科学与环境学报,2013,35(02):19.
 GAO Lin,CHEN Bin.Study on Petrology, Geochemistry and Os-Nd-Sr Isotopes of Jinan Gabbro in Luxi Block[J].Journal of Earth Sciences and Environment,2013,35(05):19.
[2]要梅娟,刘家军,翟德高,等.内蒙古道伦达坝铜多金属矿床微量元素地球化学特征[J].地球科学与环境学报,2013,35(01):24.
 YAO Mei-juan,LIU Jia-jun,ZHAI De-gao,et al.Geochemistry Characteristic of Trace Element in Daolundaba Copper-polymetallic Deposit of Inner Mongolia[J].Journal of Earth Sciences and Environment,2013,35(05):24.
[3]李云峰,李波,周亚楠,等.潜水质量安全评价指标体系的研建:以西安为例[J].地球科学与环境学报,2013,35(01):80.
 LI Yun-feng,LI Bo,ZHOU Ya-nan,et al.Establishment of Index System to Evaluate the Safety of Phreatic Water Quality: Taking Xi’an as an Example[J].Journal of Earth Sciences and Environment,2013,35(05):80.
[4]冯冲,邹华耀,郭彤楼,等.川东北及邻区上二叠统吴家坪组烃源岩评价[J].地球科学与环境学报,2013,35(04):18.
 FENG Chong,ZOU Hua-yao,GUO Tong-lou,et al.Evaluation of Source Rocks in Upper Permian Wujiaping Formation of Northeast Sichuan and Its Adjacent Area[J].Journal of Earth Sciences and Environment,2013,35(05):18.
[5]李艳,张秀颀,逯晓喻,等.松辽盆地上古生界烃源岩特征及有效性分析[J].地球科学与环境学报,2013,35(04):39.
 LI Yan,ZHANG Xiu-qi,LU Xiao-yu,et al.Characteristics and Validity Analysis of Hydrocarbon Source Rocks of Upper Paleozoic in Songliao Basin[J].Journal of Earth Sciences and Environment,2013,35(05):39.
[6]宁培松,龙群,程婷,等.鲁西地块晚中生代中—基性岩地球化学和Sr-Nd-Pb同位素组成特征[J].地球科学与环境学报,2013,35(04):62.
 NING Pei-song,LONG Qun,CHENG Ting,et al.Geochemistry and Sr-Nd-Pb Isotopic Composition of Late Mesozoic Intermediate-basic Rock in Western Shandong Block[J].Journal of Earth Sciences and Environment,2013,35(05):62.
[7]张嘉升,潘爱芳,樊会民,等.陕西柞水地区金盆梁金矿区水系沉积物地球化学特征与找矿方向[J].地球科学与环境学报,2014,36(04):55.
 ZHANG Jia-sheng,PAN Ai-fang,FAN Hui-min,et al.Geochemical Characteristics of Stream Sediment in Jinpenliang Gold Mining Area of ZhashuiArea, Shaanxi and Its Prospecting Direction[J].Journal of Earth Sciences and Environment,2014,36(05):55.
[8]曹军,钟宁宁,邓运华,等.下刚果盆地海相烃源岩地球化学特征、成因及其发育的控制因素[J].地球科学与环境学报,2014,36(04):87.
 CAO Jun,ZHONG Ning-ning,DENG Yun-hua,et al.Geochemical Characteristics, Origin and Factors Controlling Formation of Marine Source Rock in Lower Congo Basin[J].Journal of Earth Sciences and Environment,2014,36(05):87.
[9]姜常义,王子玺,杜玮,等.柴达木地块北缘南北沟岩体地球化学特征及成矿前景[J].地球科学与环境学报,2015,37(01):12.
 JIANG Chang-yi,WANG Zi-xi,DU Wei.Geochemical Characteristics of Nanbeigou Intrusion in the Northern Margin of Qaidam Massif and Its Prospecting Potential[J].Journal of Earth Sciences and Environment,2015,37(05):12.
[10]刘成林,徐韵,马寅生,等.柴达木盆地北部滩间山群碳沥青地球化学特征与成因[J].地球科学与环境学报,2015,37(01):85.
 LIU Cheng-lin,XU Yun,MA Yin-sheng,et al.Geochemical Characteristics and Origin of Anthraxolite of Tanjianshan Group in the Northern of Qaidam Basin[J].Journal of Earth Sciences and Environment,2015,37(05):85.

备注/Memo

备注/Memo:
收稿日期:2020-05-21; 修回日期:2020-07-16; 网络首发日期:2020-09-06投稿网址:http:∥jese.chd.edu.cn/
基金项目:中国地质调查局地质调查项目(1212011120862,1212011085435); 安徽省公益性地质调查项目(2016-g-2-16); 安徽省国土资源科技项目(2015-K-3)
作者简介:张靖怡(1987-),女,安徽蚌埠人,安徽省地质调查院工程师,E-mail:584064059@qq.com。
*通讯作者:张 舒(1986-),男,安徽蚌埠人,安徽省地质调查院高级工程师,理学博士,博士后,E-mail:zs-1638610@163.com。
更新日期/Last Update: 2020-09-20