«上一篇/Previous Article|本期目录/Table of Contents|下一篇/Next Article»

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

卷:

第44卷

期数:

2022年第05期

页码:

723-749

栏目:

基础地质与矿床地质

出版日期:

2022-09-15

文章信息/Info

Title:

Petrogenesis of Early Cretaceous Intrusive Rocks in Yinan Area of the Western Shandong, China: Implication for Crust-mantle Interaction Beneath North China Block

文章编号:

1672-6561(2022)05-0723-27

作者:

高明波¹; 2; 高继雷¹; 2; 张永明²; 3*; 张照录²; 3; 刘丽萍²; 3; 李亚东¹; 2; 马明¹; 2; 刘晓²; 3; 冯启伟¹; 2

(1. 山东省第一地质矿产勘查院,山东 济南 250014; 2. 山东省富铁矿勘查技术开发工程实验室,山东 济南 250014; 3. 山东理工大学 资源与环境工程学院,山东 淄博 255000)

Author(s):

GAO Ming-bo¹; 2;  GAO Ji-lei¹; 2;  ZHANG Yong-ming²; 3*;  ZHANG Zhao-lu²; 3;  LIU Li-ping²; 3;  LI Ya-dong¹; 2;  MA Ming¹; 2;  LIU Xiao²; 3;  FENG Qi-wei¹; 2

(1. No.1 Geological Team of Shandong Provincial Bureau of Geology and Mineral Resources, Jinan 250014, Shandong, China; 2. Shandong Engineering Laboratory for High-grade Iron Ore Exploration and Exploitation, Jinan 250014, Shandong, China; 3. School of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255000, Shandong, China)

关键词:

地球化学;  杂岩体;  锆石U-Pb年龄;  Sr-Nd-Pb同位素;  Hf同位素;  早白垩世;  壳幔作用;  山东

Keywords:

geochemistry;  igneous complex;  zircon U-Pb age;  Sr-Nd-Pb isotope;  Hf isotope;  Early Cretaceous;  crust-mantle interaction;  Shandong

分类号:

P588.12; P597

DOI:

10.19814/j.jese.2021.11053

文献标志码:

A

摘要:

鲁西沂南地区位于华北克拉通东南缘,区内出露的晚中生代岩浆岩是研究克拉通破坏和相关壳幔岩浆过程的理想对象。对区内典型侵入体开展了岩相学、年代学、全岩地球化学、Sr-Nd-Pb-Hf同位素研究。结果表明:石英闪长岩和二长花岗斑岩锆石U-Pb年龄分别为(130.4±0.7)Ma和(129.5±0.6)Ma,表明岩石均形成于早白垩世; 闪长质岩石属于富Na、贫K的钙碱性准铝质系列,表现出高镁安山岩/闪长岩和埃达克质岩石特征; 岩石富集大离子亲石元素,亏损高场强元素,球粒陨石标准化稀土元素配分模式为右倾型,重稀土元素配分模式相对平坦,具有弱的Eu正异常; 二长花岗斑岩高Si、富碱,贫TFe₂O₃、MgO和CaO,属于弱过铝质系列,具有强烈的Eu负异常,属于高分异I型花岗岩; 二长花岗斑岩比闪长质岩石的ε_Hf(t)值明显偏低,而闪长质岩石更加富集放射性成因Pb。结合区域地质资料分析认为:区内早白垩世侵入体可能形成于古太平洋板片回转形成的伸展背景; 软流圈的上涌促使上覆EM1+EM2型地幔发生部分熔融; 幔源岩浆底侵下地壳,与下地壳熔融的长英质岩浆在源区发生了不同程度混合,形成闪长质岩浆; 长英质岩浆吸收少量幔源基性岩浆并经历强烈的分异演化形成了二长花岗斑岩。

Abstract:

The Yinan area is located in the southeastern margin of North China Craton. There are lots of Late Mesozoic magmatic rocks in the area, which is an important case to study the North China Craton destruction and the intense crust-mantle interaction. Petrography, zircon U-Pb dating, geochemical and Sr-Nd-Pb-Hf isotope characteristics of the typical intrusive rocks in the area were carried out. The zircon U-Pb ages of quartz diorite and monzonite granite porphyry are(130.4±0.7)Ma and(129.5±0.6)Ma, respectively, indicating that the rocks form in Early Cretaceous. Geochemical characteristics show that the dioritic rocks are Na-rich but K-poor, belonging to cal-alkaline metaluminous series. The dioritic rocks are geochemically similar to high magnesian andesite/diorite and adakites. The rocks are enriched in LILEs and depleted in HFSEs. The chondrite-normalized REE patterns are right-inclined, LREE is steeper and HREE is gentler, there is no negative or weak Eu positive anomalies. The monzonitic granite porphyries are peraluminous and show high contents of Si and alkalis, low abundances of TFe₂O₃, MgO and CaO. The rocks are evidently depleted in Eu, belonging to highly differentiated I-type granite. Isotopic geochemical characteristics show that the ε_Hf(t)values of the monzonitic granite porphyries are obviously lower than those of dioritic rocks. The dioritic rocks are more enriched in Pb isotopes than the monzonitic granite porphyries. Combined with the regional geological data, it is considered that Early Cretaceous intrusion in the area likely forms in the extensional background of the rotation of paleo-Pacific plate. The upwelling of the asthenosphere promotes partial melting of the overlying EM1+EM2 enriched mantles. The basaltic magma intrudes into the lower crust and mixes with the felsic magma in varying degrees in the lower crust to form dioritic magma. Felsic magma absorbs a small amount of mantle-derived basic magma, and experiences strong differentiation and evolution to form the monzonitic granite porphyries.

参考文献/References:

[1] 林景仟,谭东娟,金 烨.鲁西地区中生代火成活动的⁴⁰Ar/³⁹Ar年龄[J].岩石矿物学杂志,1996,15(3):213-220.
LIN Jing-qian,TAN Dong-juan,JIN Ye.⁴⁰Ar/³⁹Ar Ages of Mesozoic Igneous Activities in Western Shandong[J].Acta Petrologica et Mineralogica,1996,15(3):213-220.
[2] XU Y G,HUANG X L,MA J L,et al.Crust-mantle Interaction During the Tectono-thermal Reactivation of the North China Craton:Constraints from SHRI-MP Zircon U-Pb Chronology and Geochemistry of Mesozoic Plutons from Western Shandong[J].Contributions to Mineralogy and Petrology,2004,147(6):750-767.
[3] XU Y G,MA J L,HUANG X L,et al.Early Cretaceous Gabbroic Complex from Yinan,Shandong Pro-vince:Petrogenesis and Mantle Domains Beneath the North China Craton[J].International Journal of Earth Sciences,2004,93(6):1025-1041.
[4] 杨承海,许文良,杨德彬,等.鲁西上峪辉长-闪长岩的成因:年代学与岩石地球化学证据[J].中国科学:D辑,地球科学,2008,38(1):44-55.
YANG Cheng-hai,XU Wen-liang,YANG De-bin,et al.The Origin of Gabbro-diorite in Shangyu,the Western of Shandong Province:Evidence from Chronology,Petrology and Geochemistry[J].Science in China:Series D,Earth Sciences,2008,38(1):44-55.
[5] 李 科.山东沂南金铜铁矿床同位素地球化学研究[D].北京:中国地质大学,2009.
LI Ke.Isotopic Geochemistry of the Yinan Au-Cu-Fe Deposit in Shandong Province,China[D].Beijing:China University of Geosciences,2009.
[6] 王 永,范宏瑞,胡芳芳,等.鲁西沂南铜井闪长质岩体锆石U-Pb年龄、元素及同位素地球化学特征[J].岩石矿物学杂志,2011,30(4):553-566.
WANG Yong,FAN Hong-rui,HU Fang-fang,et al.Zircon U-Pb Ages and Geochemistry of Elements and Isotopes of the Diorite from Tongjing,Yinan,Western Shandong Province[J].Acta Petrologica et Minera-logica,2011,30(4):553-566.
[7] GUO P,SANTOSH M,LI S R,et al.Crustal Evolution in the Central Part of Eastern NCC:Zircon U-Pb Ages from Multiple Magmatic Pulses in the Luxi Area and Implications for Gold Mineralization[J].Ore Geology Reviews,2014,60:126-145.
[8] 郭 谱.鲁西中生代金成矿的地球动力学背景研究[D].北京:中国地质大学,2014.
GUO Pu.Geodynamic Setting of Mesozoic Gold Me-tallogeny in the Western Shandong Province[D].Beijing:China University of Geosciences,2014.
[9] 徐金方,石玉臣,刘长春,等.鲁西金矿成因类型、空间分布及其致矿地质异常[J].地球科学,1999,24(5):468-471.
XU Jin-fang,SHI Yu-chen,LIU Chang-chun,et al.Genetic Type,Spatial Distribution and Ore-generating Geological Anomalies of Gold Deposits,Western Shandong Province,China[J].Earth Science,1999,24(5):468-471.
[10] 董树义.山东沂南金矿床成因与成矿规律和成矿预测[D].北京:中国地质大学,2008.
DONG Shu-yi.Metallogenesis,Metallogenic Laws and Metallogenic Prediction of the Yinan Gold Deposit,Shandong Province[D].Beijing:China University of Geosciences,2008.
[11] 顾雪祥,董树义,王银宏,等.不整合面控制内生金属成矿的新实例:山东沂南金铜铁矿床[J].现代地质,2008,22(2):151-161.
GU Xue-xiang,DONG Shu-yi,WANG Yin-hong,et al.A New Example of Unconformity-related Endogenic Metallization:The Yinan Au-Cu-Fe Deposit in Shandong Province,China[J].Geoscience,2008,22(2):151-161.
[12] 顾雪祥,董树义,刘 丽,等.山东沂南金-铜-铁矿床成矿条件分析:兼论不整合面的控矿作用[J].矿物岩石地球化学通报,2008,27(3):254-268.
GU Xue-xiang,DONG Shu-yi,LIU Li,et al.Ore-forming Conditions and Significance of Unconformity in the Mineralization of the Yinan Au-Cu-Fe Deposit,Shandong,China[J].Bulletin of Mineralogy,Petrology and Geochemistry,2008,27(3):254-268.
[13] 刘 丽,顾雪祥,李葆华,等.山东沂南金矿床流体包裹体特征及地质意义[J].地球与环境,2009,37(1):28-36.
LIU Li,GU Xue-xiang,LI Bao-hua,et al.The Characteristics of Fluid Inclusions from the Yinan Gold Deposit,Shandong Province and Their Geological Signi-ficance[J].Earth and Environment,2009,37(1):28-36.
[14] 胡芳芳,王 永,范宏瑞,等.鲁西沂南金场夕卡岩型金铜矿床矿化时代与成矿流体研究[J].岩石学报,2010,26(5):1503-1511.
HU Fang-fang,WANG Yong,FAN Hong-rui,et al.Geochronology and Ore-forming Fluids in the Jinchang Skarn Gold-copper Deposit,Yinan County,Western Shandong Province[J].Acta Petrologica Si-nica,2010,26(5):1503-1511.
[15] ZHANG Y M,GU X X,LIU L,et al.Fluid Inclusion and H-O Isotope Evidence for Immiscibility During Mineralization of the Yinan Au-Cu-Fe Deposit,Shandong,China[J].Journal of Asian Earth Sciences,2011,42(1/2):83-96.
[16] LIU Y,SANTOSH M,LI S R,et al.Stable Isotope Geochemistry and Re-Os Ages of the Yinan Gold Deposit,Shandong Province,Northeastern China[J].International Geology Review,2014,56(6):695-710.
[17] 李洪奎,耿 科,李逸凡,等.沂南县铜井金矿床锆石SHRIMP U-Pb年龄及其地质意义[J].矿床地质,2011,30(3):497-503.
LI Hong-kui,GENG Ke,LI Yi-fan,et al.Zircon SH-RIMP U-Pb Age of Tongjing Gold Deposit in Yinan County,Shandong and Its Geological Significance[J].Mineral Deposits,2011,30(3):497-503.
[18] 田京祥,李秀章,宋志勇,等.鲁西中生代金矿形成时代、物质来源及问题讨论[J].地质学报,2015,89(8):1530-1537.
TIAN Jing-xiang,LI Xiu-zhang,SONG Zhi-yong,et al.Environment,Formation Age and Material Sources of Mesozoic Gold Deposits in Western Shandong:A Synthesis[J].Acta Geologica Sinica,2015,89(8):1530-1537.
[19] DUAN Z,GLEESON S A,GAO W S,et al.Garnet U-Pb Dating of the Yinan Au-Cu Skarn Deposit,Luxi District,North China Craton:Implications for District-wide Coeval Au-Cu and Fe Skarn Mineralization[J].Ore Geology Reviews,2020,118:103310.
[20] 刘金友,高池兴,赵新峰.鲁中南地区燕山期侵入岩与金成矿[J].黄金地质,2002,8(2):54-57.
LIU Jin-you,GAO Chi-xing,ZHAO Xin-feng.Intrusive Rocks of Yanshan Period and Gold Mineralization in Middle-south of Shandong[J].Gold Geology,2002,8(2):54-57.
[21] 王 娟,李 宁,王继国,等.山东沂南龙头旺铜金矿床成矿地质条件及成因[J].地质学刊,2014,38(增1):146-148.
WANG Juan,LI Ning,WANG Ji-guo,et al.On Ore-forming Geological Condition and Origin of Longtouwang Cu-Au Deposit in Yinan of Shandong[J].Journal of Geology,2014,38(S1):146-148.
[22] ZHANG H F,SUN M,ZHOU X H,et al.Mesozoic Lithosphere Destruction Beneath the North China Craton:Evidence from Major-,Trace-element and Sr-Nd-Pb Isotopie Studies of Fangcheng Basalts[J].Contributions to Mineralogy and Petrology,2002,144(2):241-253.
[23] YANG D B,XU W L,PEI F P,et al.Spatial Extent of the Influence of the Deeply Subducted South China Block on the Southeastern North China Block:Constraints from Sr-Nd-Pb Isotopes in Mesozoic Mafic Igneous Rocks[J].Lithos,2012,136/137/138/139:246-260.
[24] 石文杰.山东沂沭断裂带及邻区晚中生代构造岩浆活动与金成矿作用[D].北京:中国地质大学,2014.
SHI Wen-jie.The Late Mesozoic Tectonic-magmatic Evolution Process in the Yishu Fault Zone and Adjacent Regions,Shandong Province:Implication for Gold Mineralization[D].Beijing:China University of Geosciences,2014.
[25] 陶 涛.山东沂南金矿床含矿杂岩体岩石学与地球化学研究[D].北京:中国地质大学,2009.
TAO Tao.Petrography and Geochemistry of Ore-bearing Complex of Yinan Gold Deposit,Shandong Province[D].Beijing:China University of Geoscienc-es,2009.
[26] 徐义刚,巫祥阳,罗震宇,等.山东中侏罗世-早白垩世侵入岩的锆石Hf同位素组成及其意义[J].岩石学报,2007,23(2):307-316.
XU Yi-gang,WU Xiang-yang,LUO Zhen-yu,et al.Zircon Hf Isotope Compositions of Middle Jurassic-Early Cretaceous Intrusions in Shandong Province and Its Implications[J].Acta Petrologica Sinica,2007,23(2):307-316.
[27] 邱检生,王德滋,任启江.山东沂南金场矽卡岩型金铜矿床地质地球化学特征及矿床成因[J].矿床地质,1996,15(4):330-340.
QIU Jian-sheng,WANG De-zi,REN Qi-jiang.Geolo-gical-geochemical Characteristics and Genesis of the Jinchang Skarn Type Gold-copper Deposit,Yinan County,Shandong Province[J].Mineral Deposits,1996,15(4):330-340.
[28] PATON C,WOODHEAD J D,HELLSTROM J C,et al.Improved Laser Ablation U-Pb Zircon Geochronology Through Robust Downhole Fractionation Correction[J].Geochemistry,Geophysics,Geosystems,2010,11(3):002618.
[29] CORFU F,HANCHAR J M,HOSKIN P W O,et al.Atlas of Zircon Textures[J].Reviews in Mineralogy and Geochemistry,2003,53(1):469-500.
[30] 吴福元,李献华,郑永飞,等.Lu-Hf同位素体系及其岩石学应用[J].岩石学报,2007,23(2):185-220.
WU Fu-yuan,LI Xian-hua,ZHENG Yong-fei,et al.Lu-Hf Isotopic Systematics and Their Applications in Petrology[J].Acta Petrologica Sinica,2007,23(2):185-220.
[31] YANG J H,WU F Y,CHUNG S L,et al.A Hybrid Origin for the Qianshan A-type Granite,Northeast China:Geochemical and Sr-Nd-Hf Isotopic Evidence[J].Lithos,2006,89(1/2):89-106.
[32] VERVOORT J D,PACHELT P J,GEHRELS G E,et al.Constraints on Early Earth Differentation from Hafnium and Neodymium Isotopes[J].Nature,1996,379:624-627.
[33] DEFANT M J,DRUMMOND M S.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere[J].Nature,1990,347:662-665.
[34] 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.
[35] 杨承海.鲁西中生代高镁闪长岩的年代学与地球化学:对华北克拉通岩石圈演化的制约[D].长春:吉林大学,2007.
YANG Cheng-hai.Chronology and Geochemistry of Mesozoic High-Mg Diorites in Western Shandong:Constraints on Lithospheric Evolution of the North China Craton[D].Changchun:Jilin University,2007.
[36] TATSUMI Y,ISHIKAWA N,ANNO K,et al.Tectonic Setting of High-Mg Andesite Magmatism in the SW Japan Arc:K-Ar Chronology of the Setouchi Volcanic Belt[J].Geophysical Journal International,2001,144(3):625-631.
[37] TSUCHIYA N,SUZUKI S,KIMURA J I.Evidence for Slab Melt/Mantle Reaction:Petrogenesis of Early Cretaceous and Eocene High-Mg Andesites from the Kitakami Mountains,Japan[J].Lithos,2005,79(1/2):179-206.
[38] 唐功建,王 强.高镁安山岩及其地球动力学意义[J].岩石学报,2010,26(8):2495-2512.
TANG Gong-jian,WANG Qiang.High-Mg Andesites and Their Geodynamic Implications[J].Acta Petrologica Sinica,2010,26(8):2495-2512.
[39] YANG C H,XU W L,YANG D B,et al.Petrogenesis of Mesozoic High-Mg Diorites in Western Shandong:Evidence from Chronology and Petro-geochemistry[J].Journal of Earth Science,2005,16(4):297-308.
[40] XU W L,WANG Q H,WANG D Y,et al.Mesozoic Adakitic Rocks from the Xuzhou-Suzhou Area,Eastern China:Evidence for Partial Melting of Delaminated Lower Continental Crust[J].Journal of Asian Earth Sciences,2006,27(4):454-464.
[41] 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.
[42] TAYLOR S R,MCLENNAN S M.The Geochemical Evolution of the Continental Crust[J].Reviews of Geophysics,1995,33(2):241-265.
[43] TAYLOR S R,MCLENNAN S M.The Continental Crust:Its Composition and Evolution[M].Oxford:Blackwell,1985.
[44] MIDDLEMOST E A K.Naming Materials in the Magma/Igneous Rock System[J].Earth-science Reviews,1994,37(3/4):215-224.
[45] RICKWOOD P C.Boundary Lines Within Petrologic Diagrams Which Use Oxides of Major and Minor Elements[J].Lithos,1989,22(4):247-263.
[46] WEDEPOHL K H.The Composition of the Continental Crust[J].Geochimica et Cosmochimica Acta,1995,59(7):1217-1232.
[47] LASSITER J C,DEPAOLO D J.Plume/Lithosphere Interaction in the Generation of Continental and Ocea-nic Flood Basalts:Chemical and Isotopic Constraints[M]∥MAHONEY J J,COFFIN M F.Large Igneous Provinces:Continental,Oceanic,and Planetary Flood Volcanism.Washington DC:American Geophysical Union,1997:335-355.
[48] YANG J H,CHUNG S L,ZHAI M G,et al.Geochemical and Sr-Nd-Pb Isotopic Compositions of Mafic Di-kes from the Jiaodong Peninsula,China:Evidence for Vein-plus-peridotite Melting in the Lithospheric Mantle[J].Lithos,2004,73(3/4):145-160.
[49] 李曙光,聂永红,HART S R,等.俯冲陆壳与上地幔的相互作用:Ⅱ.大别山同碰撞镁铁—超镁铁岩的Sr,Nd同位素地球化学[J].中国科学:D辑,地球科学,1998,28(1):18-22.
LI Shu-guang,NIE Yong-hong,HART S R,et al.Upper Mantle-deep Subducted Continental Crust Interaction:(Ⅱ)Sr and Nd Isotopic Constraints on the Syn-collisional Mafic to Ultramafic Intrusions in the Northern Dabieshan,Eastern China[J].Science in China:Series D,Earth Science,1998,28(1):18-22.
[50] 金子梁.矽卡岩型富铁矿成因研究:以鲁西淄博和莱芜铁矿为例[D].北京:中国地质大学,2017.
JIN Zi-liang.Genesis of High-grade Fe Skarns:A Case Study of Zibo and Laiwu Iron Deposits in Western Shandong[D].Beijing:China University of Geosciences,2017.
[51] WU F Y,ZHAO G C,WILDE S A,et al.Nd Isotopic Constraints on Crustal Formation in the North China Craton[J].Journal of Asian Earth Sciences,2005,24(5):523-545.
[52] 霍腾飞,杨德彬,师江朋,等.徐淮地区早白垩世丰山和蔡山高镁埃达克质岩:拆沉下地壳熔融的熔体与地幔橄榄岩的反应[J].岩石学报,2018,34(6):1669-1684.
HUO Teng-fei,YANG De-bin,SHI Jiang-peng,et al.Early Cretaceous Fengshan and Caishan High-Mg^# Adakitic Rocks from the Xuzhou-Huaibei Area,Central China:Interaction Between Mantle Peridotite and Melt Derived from Partial Melting of Delaminated Lower Continental Crust[J].Acta Petrologica Sinica,2018,34(6):1669-1684.
[53] 李曙光,杨 蔚.大别造山带深部地缝合线与地表地缝合线的解耦及大陆碰撞岩石圈楔入模型:中生代幔源岩浆岩Sr-Nd-Pb同位素证据[J].科学通报,2002,47(24):1898-1905.
LI Shu-guang,YANG Wei.Decoupling Between Suture Zone in the Deep of Dabie Orogenic Belt and on the Surface,and the Model of Lithospheric Wedge Continental Collision:Sr-Nd-Pb Isotopic Evidence of Mesozoic Mantle-derived Rocks[J].Chinese Science Bulletin,2002,47(24):1898-1905.
[54] BOYNTON W V.Cosmochemistry of the Rare Earth Elements:Meteorite Studies[J].Developments in Geochemistry,1984,2:63-114.
[55] WANG H,XU Z W,LU X C,et al.Two-types of Early Cretaceous Adakitic Porphyries from the Luxi Terrane,Eastern North China Block:Melting of Subducted Paleo-Pacific Slab and Delaminated Newly Underplated Lower Crust[J].Lithos,2016,240/241/242/243:140-154.
[56] 蔡剑辉,阎国翰,牟保磊,等.北京房山岩体锆石U-Pb年龄和Sr、Nd、Pb同位素与微量元素特征及成因探讨[J].岩石学报,2005,21(3):776-788.
CAI Jian-hui,YAN Guo-han,MOU Bao-lei,et al.Zircon U-Pb Age,Sr-Nd-Pb Isotopic Compositions and Trace Element of Fangshan Complex in Beijing and Their Petrogenesis Significance[J].Acta Petrologica Sinica,2005,21(3):776-788.
[57] PITCHER W S.The Nature and Origin of Granite[M].2nd ed.London:Chapman and Hall,1997.
[58] KING P L,WHITE A J R,CHAPPELL B W,et al.Characterization and Origin of Aluminous A-type Granites from the Lachlan Fold Belt,Southeastern Australia[J].Journal of Petrology,1997,38(3):371-391.
[59] WHALEN J B,CURRIE K L,CHAPPELL B W.A-type Granites:Geochemical Characteristics,Discrimination and Petrogenesis[J].Contributions to Minera-logy and Petrology,1987,95(4):407-419.
[60] WU F Y,JAHN B M,WILDE S A,et al.Highly Fractionated I-type Granites in NE China(Ⅰ):Geochronology and Petrogenesis[J].Lithos,2003,66(3):241-273.
[61] WU F Y,JAHN B M,WILDE S A,et al.Highly Fractionated I-type Granites in NE China(Ⅱ):Isotopic Geochemistry and Implications for Crustal Growth in the Phanerozoic[J].Lithos,2003,67(3/4):191-204.
[62] WATSON E B,HARRISON T M.Zircon Saturation Revisited:Temperature and Composition Effects in a Variety of Crustal Magma Types[J].Earth and Pla-netary Science Letters,1983,64(2):295-304.
[63] WATSON E B,HARRISON T M.Zircon Thermometer Reveals Minimum Melting Conditions on Earliest Earth[J].Science,2005,308:841-844.
[64] 吴福元,刘小驰,纪伟强,等.高分异花岗岩的识别与研究[J].中国科学:地球科学,2017,47(7):745-765.
WU Fu-yuan,LIU Xiao-chi,JI Wei-qiang,et al.Highly Fractionated Granites:Recognition and Research[J].Science China:Earth Sciences,2017,47(7):745-765.
[65] CHAPPELL B W,WHITE A J R.Two Contrasting Granite Types[J].Pacific Geology,1974,8(2):173-174.
[66] CHAPPELL B W,BRYANT C J,WYBORN D.Peraluminous I-type Granites[J].Lithos,2012,153:142-153.
[67] CLEMENS J D,STEVENS G,FARINA F.The Enigmatic Sources of I-type Granites:The Peritectic Connexion[J].Lithos,2011,126(3/4):174-181.
[68] LEE C T A,MORTON D M.High Silica Granites:Terminal Porosity and Crystal Settling in Shallow Magma Chambers[J].Earth and Planetary Science Letters,2015,409(1):23-31.
[69] HARRIS N B W,INGER S.Trace Element Modelling of Pelite-derived Granites[J].Contributions to Mine-ralogy and Petrology,1992,110(1):46-56.
[70] GRIFFIN W L,WANG X,JACKSON S E,et al.Zircon Chemistry and Magma Mixing,SE China:In-situ Analysis of Hf Isotopes,Tonglu and Pingtan Igneous Complexes[J].Lithos,2002,61(3/4):237-269.
[71] 胡芳芳,范宏瑞,杨进辉,等.胶东文登长山南花岗闪长岩体的岩浆混合成因:闪长质包体及寄主岩石的地球化学、Sr-Nd同位素和锆石Hf同位素证据[J].岩石学报,2005,21(3):569-586.
HU Fang-fang,FAN Hong-rui,YANG Jin-hui,et al.Magma Mixing for the Origin of Granodiorite:Geochemical,Sr-Nd Isotopic and Zircon Hf Isotopic Evidence of Dioritic Enclaves and Host Rocks from Changshannan Granodiorite in the Jiaodong Peninsula,Eastern China[J].Acta Pelrologica Sinica,2005,21(3):569-586.
[72] MARTIN H,SMITHIES R H,RAPP R,et al.An Overview of Adakite,Tonalite-trondhjemite-granodio-rite(TTG),and Sanukitoid:Relationships and Some Implications for Crustal Evolution[J].Lithos,2005,79(1/2):1-24.
[73] CHIARADIA M,MÜNTENER O,BEATE B,et al.Adakite-like Volcanism of Ecuador:Lower Crust Ma-gmatic Evolution and Recycling[J].Contributions to Mineralogy and Petrology,2009,158(5):563-588.
[74] CHEN B,JOHN B M,SUZUKI K.Petrological and Nd-Sr-Os Isotopic Constraints on the Origin of High-Mg Adakitic Rocks from the North China Craton:Tectonic Implications[J].Geology,2013,41(1):91-94.
[75] CHUNG S L,LIU D,JI J,et al.Adakites from Continental Collision Zones:Melting of Thickened Lower Crust Beneath Southern Tibet[J].Geology,2003,31(11):1021-1024.
[76] WANG Q,MCDERMOTT F,XU J F,et al.Cenozoic K-rich Adakitic Volcanic Rocks in the Hohxil Area,Northern Tibet:Lower-crustal Melting in an Intracontinental Setting[J].Geology,2005,33(6):465-468.
[77] HUANG X L,XU Y G,LAN J B,et al.Neoproterozoic Adakitic Rocks from Mopanshan in the Western Yangtze Craton:Partial Melts of a Thickened Lower Crust[J].Lithos,2009,112(3/4):367-381.
[78] YANG D B,XU W L,ZHAO G C,et al.Tectonic Implications of Early Cretaceous Low-Mg Adakitic Ro-cks Generated by Partial Melting of Thickened Lower Continental Crust at the Southern Margin of the Central North China Craton[J].Gondwana Research,2016,38:220-237.
[79] GAO S,RUDNICK R L,YUAN H L,et al.Recycling Lower Continental Crust in the North China Craton[J].Nature,2004,432:892-897.
[80] ATHERTON M P,PETFORD N.Generation of Sodium-rich Magmas from Newly Underplated Basaltic Crust[J].Nature,1993,362:144-146.
[81] 许文良,王冬艳,高 山,等.鲁西中生代金岭闪长岩中纯橄岩和辉石岩包体的发现及其意义[J].科学通报,2003,48(8):863-868.
XU Wen-liang,WANG Dong-yan,GAO Shan,et al.Discovery of Dunite and Pyroxenite Xenoliths in Me-sozoic Diorite at Jinling,Western Shandong and Its Significance[J].Chinese Science Bulletin,2003,48(8):863-868.
[82] 许文良,王冬艳,王清海,等.鲁西中生代闪长岩中两类幔源捕虏体的岩石学和地球化学[J].岩石学报,2003,19(4):623-636.
XU Wen-liang,WANG Dong-yan,WANG Qing-hai,et al.Petrology and Geochemistry of Two Types of Mantle-derived Xenoliths in Mesozoic Diorite from Western Shandong Province[J].Acta Petrologica Si-nica,2003,19(4):623-636.
[83] 杨承海,许文良,杨德彬,等.鲁西中生代高Mg闪长岩的成因:年代学与岩石地球化学证据[J].地球科学,2006,31(1):81-92.
YANG Cheng-hai,XU Wen-liang,YANG De-bin,et al.Petrogenesis of the Mesozoic High-Mg Diorites in West Shandong:Evidence from Chronology and Pe-trogeochemistry[J].Earth Science,2006,31(1):81-92.
[84] GREEN D H.Experimental Melting Studies on a Mo-del Upper Mantle Composition at High Pressure Under Water-saturated and Water-undersaturated Conditions[J].Earth and Planetary Science Letters,1973,19(1):37-53.
[85] WILSON B M.Igneous Petrogenesis:A Global Tectonic Approach[M].London:Unwin Hyman,1989.
[86] BAKER M B,HIRSCHMANN M M,GHIORSO M S,et al.Compositions of Near-solidus Peridotite Melts from Experiments and Thermodynamic Calculations[J].Nature,1995,375:308-311.
[87] FALLOON T J,GREEN D H,O'NEILL H S C,et al.Experimental Tests of Low Degree Peridotite Partial Melt Compositions:Implications for the Nature of Anhydrous Near-solidus Peridotite Melts at 1 GPa[J].Earth and Planetary Science Letters,1997,152(1/2/3/4):149-162.
[88] 许文良,王冬艳,王清海,等.鲁西纯橄岩捕虏体中富硅质熔(流)体的交代作用:对中生代岩石圈地幔减薄的意义[J].地质学报,2004,78(1):72-80.
XU Wen-liang,WANG Dong-yan,WANG Qing-hai,et al.Metasomatism of Silica-rich Melts(Liquids)in Dunite Xenoliths from Western Shandong,China:Implication for Mesozoic Lithospheric Mantle Thinning[J].Acta Geologica Sinica,2004,78(1):72-80.
[89] 陈 斌,刘超群,田 伟.太行山中生代岩浆作用过程中的壳幔岩浆混合作用:岩石学和地球化学证据[J].地学前缘,2006,13(2):140-147.
CHEN Bin,LIU Chao-qun,TIAN Wei.Magma-mixing Between Mantle- and Crustal-derived Melts in the Process of Mesozoic Magmatism,Taihangshan:Constraints from Petrology and Geochemistry[J].Earth Science Frontiers,2006,13(2):140-147.
[90] 陈 斌,陈长健,贺敬博,等.华北东部中生代高镁埃达克质岩浆的起源:岩石学和Nd-Sr-Os同位素证据[J].科学通报,2013,58(20):1941-1953.
CHEN Bin,CHEN Chang-jian,HE Jing-bo,et al.Origin of Mesozoic High-Mg Adakitic Rocks from Nor-theastern China:Petrological and Nd-Sr-Os Isotopic Constraints[J].Chinese Science Bulletin,2013,58(20):1941-1953.
[91] LAN T G,HU R Z,CHEN Y H,et al.Generation of High-Mg Diorites and Associated Iron Mineralization Within an Intracontinental Setting:Insights from Ore-barren and Ore-bearing Intrusions in the Eastern North China Craton[J].Gondwana Research,2019,72:97-119.
[92] SMITHIES R H,CHAMPION D C.The Archaean High-Mg Diorite Suite:Links to Tonalite-tondhjemi-te-granodiorite Magmatism and Implications for Early Archaean Crustal Growth[J].Journal of Petrology,2000,41(12):1653-1671.
[93] XU W L,YANG D B,GAO S,et al.Geochemistry of Peridotite Xenoliths in Early Cretaceous High-Mg^# Diorites from the Central Orogenic Block of the North China Craton:The Nature of Mesozoic Lithospheric Mantle and Constraints on Lithospheric Thinning[J].Chemical Geology,2010,270(1/2/3/4):257-273.
[94] MA Q,ZHENG J P,XU Y G,et al.Are Continental “Adakities” Derived from Thickened or Foundered Lower Crust?[J].Earth and Planetary Science Letters,2015,419(2):125-133.
[95] BOLHAR R,WEAVER S D,WHITEHOUSE M J,et al.Sources and Evolution of Arc Magmas Inferred from Coupled O and Hf Isotope Systematics of Plutonic Zircons from the Cretaceous Separation Point Suite(New Zealand)[J].Earth and Planetary Science Letters,2008,268(3/4):312-324.
[96] WANG J,GOU G N,WANG Q,et al.Petrogenesis of the Late Triassic Diorites in the Hoh Xil Area,Northern Tibet:Insights into the Origin of the High-Mg^# Andesitic Signature of Continental Crust[J].Lithos,2018,300/301:348-360.
[97] 张宏福,邵济安.辽西义县组火山岩:拆沉作用还是岩浆混合作用的产物?[J].岩石学报,2008,24(1):37-48.
ZHANG Hong-fu,SHAO Ji-an.Volcanic Lavas of the Yixian Formation in Western Liaoning Province,China:Products of Lower Crust Delamination or Magma Mixing?[J].Acta Petrologica Sinica,2008,24(1):37-48.
[98] MOYEN J F.High Sr/Y and La/Yb Ratios:The Meaning of the “Adakitic Signature”[J].Lithos,2009,112(3/4):556-574.
[99] MOORE G,CARMICHAEL I S E.The Hydrous Phase Equilibria(to 3 kbar)of an Andesite and Basaltic Andesite from Western Mexico:Constraints on Water Content and Conditions of Phenocryst Growth[J].Contributions to Mineralogy and Petrology,1998,130(3/4):304-319.
[100] KARSLI O,DOKUZ A,UYSAL I,et al.Relative Contributions of Crust and Mantle to Generation of Campanian High-K Calc-alkaline I-type Granitoids in a Subduction Setting,with Special Reference to the Harsit Pluton,Eastern Turkey[J].Contributions to Mineralogy and Petrology,2010,160(4):467-487.
[101] ZHU D C,MO X X,NIU Y L,et al.Geochemical Investigation of Early Cretaceous Igneous Rocks Along an East-west Traverse Throughout the Central Lhasa Terrane,Tibet[J].Chemical Geology,2009,268(3/4):298-312.
[102] TOPUZ G,ALTHERR R,SIEBEL W,et al.Carboni-ferous High-potassium I-type Granitoid Magmatism in the Eastern Pontides:The Gümüshane Pluton(NE Turkey)[J].Lithos,2010,116(1/2):92-110.
[103] CHEN B,ARAKAWA Y.Elemental and Nd-Sr Isotopic Geochemistry of Granitoids from the West Junggar Foldbelt(NWChina ),with Implications for Pha-nerozoic Continental Growth[J].Geochimica et Cosmochimica Acta,2005,69(5):1307-1320.
[104] WYBORN D,CHAPPELL BW,JAMES M.Examples of Convective Fractionation in High-temperature Granites from the Lachlan Fold Belt[J].Australian Journal of Earth Sciences,2001,48(4):531-541.
[105] VALLEY J W,LACKEY J S,CAVOSIE A J,et al.4.4 Billion Years of Crustal Maturation:Oxygen Isotope Ratios of Magmatic Zircon[J].Contributions to Mineralogy and Petrology,2005,150(6):561-580.
[106] SIMON L,LÉCUYER C.Continental Recycling:The Oxygen Isotope Point of View[J].Geochemistry,Geo-physics,Geosystems,2005,6(8):1-10.
[107] KEMPTON P D,HARMON R S.Oxygen Isotope Evidence for Large-scale Hybridization of the Lower Crust During Magmatic Underplating[J].Geochimica et Cosmochimica Acta,1992,56(3):971-986.
[108] 熊小林,刘星成,朱志敏,等.华北埃达克质岩与克拉通破坏:实验岩石学和地球化学依据[J].中国科学:地球科学,2011,41(5):654-667.
XIONG Xiao-lin,LIU Xing-cheng,ZHU Zhi-min,et al.Adakitic Rocks and Destruction of the North China Craton:Evidence from Experimental Petrology and Geochemistry[J].Science China:Earth Sciences,2011,41(5):654-667.
[109] DEPAOLO D J,DALEY E E.Neodymium Isotopes in Basalts of the Southwest Basin and Range and Lithospheric Thinning During Continental Extension[J].Chemical Geology,2000,169(1/2):157-185.
[110] MARTIN H,BONIN B,CAPDEVILA R,et al.The Kuiqi Peralkaline Granitic Complex(SE China):Petrology and Geochemistry[J].Journal of Petrology,1994,35(4):983-1015.
[111] HALLIDAY A N,DAVIDSON J P,HILDRETH W,et al.Modelling the Petrogenesis of High Rb/Sr Sili-cic Magmas[J].Chemical Geology,1991,92(1/2/3):107-114.
[112] SAMI M,NTAFLOS T,FARAHAT E S,et al.Petrogenesis and Geodynamic Implications of Ediacaran Highly Fractionated A-type Granitoids in the North Arabian-Nubian Shield(Egypt):Constraints from Whole-rock Geochemistry and Sr-Nd Isotopes[J].Lithos,2018,304/305/306/307:329-346.
[113] JIANG Y H,LING H F,JIANG S Y,et al.Petroge-nesis of a Late Jurassic Peraluminous Volcanic Complex and Its High-Mg Potassic Quenched Enclaves at Xiangshan,Southeast China[J].Journal of Petrology,2005,46(6):1121-1154.
[114] JIANG Y H,JIANG S Y,LING H F,et al.Petroge-nesis and Tectonic Implications of Late Jurassic Sho-shonitic Lamprophyre Dikes from the Liaodong Pe-ninsula,NE China[J].Mineralogy and Petrology,2010,100(3):127-151.
[115] WU F Y,LIN J Q,WILDE S A,et al.Nature and Significance of the Early Cretaceous Giant Igneous Event in Eastern China[J].Earth and Planetary Science Letters,2005,233(1/2):103-119.
[116] ZHAO Z F,ZHENG Y F,ZHANG J,et al.Syn-exhumation Magmatism During Continental Collision:Evidence from Alkaline Intrusives of Triassic Age in the Sulu Orogen[J].Chemical Geology,2012,328:70-88.
[117] YANG Q L,ZHAO Z F,ZHENG Y F.Slab-mantle Interaction in Continental Subduction Channel:Geochemical Evidence from Mesozoic Gabbroic Intrusives in Southeastern North China[J].Lithos,2012,155:442-460.
[118] YANG Q L,ZHAO Z F,ZHENG Y F.Modification of Subcontinental Lithospheric Mantle Above Continental Subduction Zone:Constraints from Geochemistry of Mesozoic Gabbroic Rocks in Southeastern North China[J].Lithos,2012,146/147:164-182.
[119] HUANG X L,ZHONG J W,XU Y G.Two Tales of the Continental Lithospheric Mantle Prior to the Destruction of the North China Craton:Insights from Early Cretaceous Mafic Intrusions in Western Shandong,East China[J].Geochimica et Cosmochimica Acta,2012,96:193-214.
[120] GAO S,RUDNICK R L,XU W L,et al.Recycling Deep Cratonic Lithosphere and Generation of Intraplate Magmatism in the North China Craton[J].Earth and Planetary Science Letters,2008,270(1/2):41-53.
[121] MA L,JIANG S Y,DAI B Z,et al.Multiple Sources for the Origin of Late Jurassic Linglong Adakitic Granite in the Shandong Peninsula,Eastern China:Zircon U-Pb Geochronological,Geochemical and Sr-Nd-Hf Isotopic Evidence[J].Lithos,2013,162/163:251-263.
[122] 董树文,张岳桥,龙长兴,等.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报,2007,81(11):1449-1461.
DONG Shu-wen,ZHANG Yue-qiao,LONG Chang-xing,et al.Jurassic Tectonic Revolution in China and New Interpretation of the Yanshan Movement[J].Acta Geologica Sinica,2007,81(11):1449-1461.
[123] YANG J H,WU F Y,CHUNG S L,et al.Rapid Exhumation and Cooling of the Liaonan Metamorphic Core Complex:Inferences from ⁴⁰Ar/³⁹Ar Thermochronology and Implications for Late Mesozoic Extension in the Eastern North China Craton[J].Geological Society of America Bulletin,2007,119(11/12):1405-1414.
[124] ZHU G,NIU M L,XIE C L,et al.Sinistral to Normal Faulting Along the Tan-Lu Fault Zone:Evidence for Geodynamic Switching of the East China Continental Margin[J].Journal of Geology,2010,118(3):277-293.
[125] 郑建平,戴宏坤.西太平洋板片俯冲与后撤引起华北东部地幔置换并导致陆内盆-山耦合[J].中国科学:地球科学,2018,48(4):436-456.
ZHENG Jian-ping,DAI Hong-kun.Subduction and Retreating of the Western Pacific Plate Resulted in Lithospheric Mantle Replacement and Coupled Basin-mountain Respond in the North China Craton[J].Science China:Earth Sciences,2018,48(4):436-456.
[126] 陈 斌,田 伟,翟明国,等.太行山和华北其它地区中生代岩浆作用的锆石U-Pb年代学和地球化学特征及其岩浆成因和地球动力学意义[J].岩石学报,2005,21(1):13-24.
CHEN Bin,TIAN Wei,ZHAI Ming-guo,et al.Zircon U-Pb Geochronology and Geochemistry of the Mesozoic Magmatism in the Taihang Mountains and Other Places of the North China Craton,with Implications for Petrogenesis and Geodynamic Setting[J].Acta Petrologica Sinica,2005,21(1):13-24.
[127] WU F Y,YANG J H,XU Y G,et al.Destruction of the North China Craton in the Mesozoic[J].Annual Review of Earth and Planetary Sciences,2019,47(1):173-195.
[128] 朱日祥,徐义刚.西太平洋板块俯冲与华北克拉通破坏[J].中国科学:地球科学,2019,49(9):1346-1356.
ZHU Ri-xiang,XU Yi-gang.The Subduction of the West Pacific Plate and the Destruction of the North China Craton[J].Science China:Earth Sciences,2019,49(9):1346-1356.
[129] 郭慧丽,徐佩芬,张福勤.华北克拉通及东邻西太平洋活动大陆边缘地区的P波速度结构:对岩石圈减薄动力学过程的探讨[J].地球物理学报,2014,57(7):2352-2361.
GUO Hui-li,XU Pei-fen,ZHANG Fu-qin.P Wave Velocity Structure of the North China Craton and West Pacific Active Continental Margin:Exploration for Dynamic Processes of Lithospheric Thinning[J].Chinese Journal of Geophysics,2014,57(7):2352-2361.
[130] 姜耀辉,王国昌.中国东南部晚中生代花岗岩成因与深部动力学机制:古太平洋板块反复俯冲-后退模式[J].矿物岩石地球化学通报,2016,35(6):1073-1081.
JIANG Yao-hui,WANG Guo-chang.Petrogenesis and Geodynamics of Late Mesozoic Granitoids in SE China:Tectonic Model Involving Repeated Slab-advance-retreat of the Paleo-Pacific Plate[J].Bulletin of Mineralogy,Petrology and Geochemistry,2016,35(6):1073-1081.
[131] JI W B,LIN W,FAURE M,et al.Origin of the Late Jurassic to Early Cretaceous Peraluminous Granitoids in the North-eastern Hunan Province(Middle Yangtze Region),South China:Geodynamic Implications for the Paleo-Pacific Subduction[J].Journal of Asian Earth Sciences,2017,141:174-193.
[132] 高明波,高继雷,张永明,等.鲁西莱芜矿山岩浆杂岩体源区及成因:地球化学、全岩Sr-Nd-Pb及锆石Hf同位素约束[J].矿物岩石地球化学通报,2022,41(2):287-306.
GAO Ming-bo,GAO Ji-lei,ZHANG Yong-ming,et al.Magma Source and Genesis of Kuangshan Complex in Laiwu County of Western Shandong:Constraints from Geochronology,Geochemistry,and Sr-Nd-Pb-Hf Isotopes[J].Bulletin of Mineralogy,Petrology and Geochemistry,2022,41(2):287-306.
[133] 杨德彬,杨进辉,许文良,等.大陆深俯冲作用对邻区岩石圈地幔影响的时空范围:以华北陆块东南部为例[J].科学通报,2013,58(23):2306-2309.
YANG De-bin,YANG Jin-hui,XU Wen-liang,et al.Spatial and Temporal Extents of the Influence of Deep Continental Subduction on the Adjacent Lithospheric Mantle:An Example from the Southeast North China Block[J].Chinese Science Bulletin,2013,58(23):2306-2309.
[134] 张 剑,李三忠,李玺瑶,等.鲁西地区燕山期构造变形:古太平洋板块俯冲的构造响应[J].地学前缘,2017,24(4):226-238.
ZHANG Jian,LI San-zhong,LI Xi-yao,et al.Yan-shanian Deformation of the Luxi Area:Tectonic Response to the Paleo-Pacifc Plate Subduction[J].Earth Science Frontiers,2017,24(4):226-238.
[135] 李三忠,王金铎,刘建忠,等.鲁西地块中生代构造格局及其形成背景[J].地质学报,2005,79(4):487-497.
LI San-zhong,WANG Jin-duo,LIU Jian-zhong,et al.Mesozoic Structure and Its Tectonic Setting in the Western Shandong Block[J].Acta Geologica Sinica,2005,79(4):487-497.
[136] 朱 光,牛漫兰,刘国生,等.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件[J].地质学报,2002,76(3):325-334.
ZHU Guang,NIU Man-lan,LIU Guo-sheng,et al.Structural,Magmatic and Sedimentary Events of the Tan-Lu Fault Belt During its Early Cretaceous Strike-slip Movement[J].Acta Geologica Sinica,2002,76(3):325-334.
[137] 朱 光,宋传中,牛漫兰,等.郯庐断裂带的岩石圈结构及其成因分析[J].高校地质学报,2002,8(3):248-256.
ZHU Guang,SONG Chuan-zhong,NIU Man-lan,et al.Lithospheric Textures of the Tan-Lu Fault Zone and Their Genetic Analysis[J].Geological Journal of China Universities,2002,8(3):248-256.
[138] 钟军伟,黄小龙.鲁西早白垩世基性侵入岩的锆石Hf同位素组成变化及其成因[J].大地构造与成矿学,2012,36(4):572-580.
ZHONG Jun-wei,HUANG Xiao-long.Spatial Variation of Zircon Hf Isotopes for the Early Cretaceous Mafic Intrusions in Western Shandong and Its Genesis[J].Geotectonica et Metallogenia,2012,36(4):572-580.

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:2021-11-27; 修回日期:2022-02-26投稿网址:http:∥jese.chd.edu.cn/
基金项目:山东省地质矿产勘查开发局局控项目(KC201901); 山东省第一地质矿产勘查院科技创新项目(KC202005,KC202102)
作者简介:高明波(1978-),男,山东昌乐人,山东省第一地质矿产勘查院研究员,E-mail:jngmb@126.com。
*通讯作者:张永明(1971-),男,安徽和县人,山东理工大学副教授,理学博士,E-mail:yongmzh@163.com。

常用功能

更新日期/Last Update: 2022-10-01