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作者简介:

石玉若,男,1975年生。博士,研究员,从事同位素地质年代学研究。E-mail: shiyuruo@bjshrimp.cn。

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目录contents

    摘要

    郯庐断裂带是中国东部规模最大的一条岩石圈断裂带,也是中国东部最重要的一条中、新生代岩浆、成矿和构造活动带。不能很好地认识郯庐断裂,就不能很好地认识中国东部中生代的构造演化,也就不能很好地理解欧亚大陆的当今格局。本文从我们近年来对郯庐断裂带沿线中生代岩浆岩的研究成果出发,以任纪舜先生主编的《国际亚洲地质图》为指导思想,提出郯庐断裂的大型走滑启动应与早白垩世(~143 Ma)洋底高原与欧亚大陆的碰撞有关。郯庐断裂这一切割岩石圈深度的大型断裂是导致华北克拉通发生破坏的关键因素,为深部幔源物质的上涌提供了通道。郯庐断裂带两侧有规律地成群成带分布金矿等多金属矿产,多形成于郯庐断裂大型挤压走滑后(~123 Ma)的伸展背景。

    Abstract

    The Tanlu Fault, the largest lithospheric fault zone in eastern China, is characterized by frequent tectonic activity and is a significant zone of magmatism and mineralization from the Mesozoic to the Cenozoic. A comprehensive understanding of the Tanlu Fault is important for comprehending the tectonic evolution of eastern China during the Mesozoic and the current configuration of the Eurasian continent. Based on our recent research on Mesozoic magmatic rocks along the Tanlu Fault, and guided by the International Geological Map of Asia edited by Prof. Ren Jishun, we propose that the initiation of the Tanlu Fault's large-scale strike-slip movement is linked to the collision between the oceanic plateau and the Eurasian continent in the early Cretaceous (~143 Ma). This profoundly deep fault, which dissects the lithosphere, is a critical factor in the destruction of the North China Craton, offering a pathway for the ascent of deep mantle-derived materials. The Tanlu Fault Zone hosts a systematic distribution of polymetallic mineral deposits, including gold fields, which formed in an extensional setting following a major compressional strike-slip event (~123 Ma) in eastern China.

  • 深断裂的存在是一个不容忽视的客观事实,深断裂影响深度大,延伸距离长,同时控制矿产的形成与分布(任纪舜等,1980)。中国出露有10多条超岩石圈断裂带和80余条岩石圈断裂带和为数更多的壳断裂带(任纪舜等,1980)。郯庐断裂带作为中国东部规模最大的一条岩石圈断裂带,最大位移量超过700 km(徐嘉炜,1980; Chen Peiji,1989; 徐嘉炜和马国锋,1992),是中国东部最重要的一条中、新生代岩浆、成矿和构造活动带。

  • 郯庐断裂大型走滑启动时间及机制一直存有争议。前人主要通过精确测定断裂带内的糜棱岩形成时间或者通过研究断裂带可能切割的盆地及其沉积中心的演变来约束走滑时间(梁光河,2018; 朱光等,2018)。关于郯庐断裂大型走滑的时间主要有以下几种观点:晚侏罗世—早白垩世(Xu Jiawei and Zhu Guang,1994)、早白垩世(朱光等,2016)、三叠纪(万天丰等,1996)以及中三叠世—侏罗纪(陈宣华等,2000)。另外,对于大型走滑的启动机制,则受古太平洋板块俯冲的影响(朱光等,20162018)或与欧亚板块在中—新生代板块漂移过程有关(梁光河,2018)等不同认识。

  • 另外,华北克拉通的破坏主要发生在中生代(朱日祥等,2012; Zhu Rixiang et al.,2017; 郑建平和戴宏坤,2018; Liu Jingao et al.,2019; Wu Fuyuan et al.,2019;朱日祥等和徐义刚),主要有以下模型:① 下陆壳拆沉(Gao Shan et al.,2004; Wu Fuyuan et al.,2005);② 热/化学侵蚀(Griffin et al.,1998; Xu Yigang et al.,2001; 张宏福,2009);③ 板块俯冲转换,主要是古太平洋板块俯冲作用(张宏福,2009; 郑永飞和吴福元,2009; 朱日祥和郑天愉,2009朱日祥等,2012; 2019)。郯庐断裂带作为岩石圈地幔转换和置换的优先区域(Zheng Jianping et al.,2007; Zheng Yongfei,2012; 郑建平和戴宏坤,2018),其与华北克拉通破坏的关系如何?

  • 本文从近年来对郯庐断裂带沿线中生代岩浆岩的研究成果出发,结合前人资料,针对上述问题进行初步探讨,进而起到抛砖引玉的作用,以引起更多优秀的地质学家重视。

  • 1 区域地质背景

  • 郯庐断裂带作为中国东部一条重要的强烈构造变形带,大致沿沈阳至广济一线展布(Xu Jiawei and Zhu Guang,1994),是濒西太平洋东亚大陆边缘上一条巨型断裂带,总体呈北北东向(25°~40°)延伸,在中国境内长达2400 km。不同的学者对该断裂带做了较多研究(牛漫兰等,2010; Zhu Guang et al.,2012; 朱光等,2016),尽管有诸多争议,但是众多研究表明郯庐断裂带是中生代岩石圈减薄的强减薄带,其岩浆活动峰期和华北地区一致(朱光等,2016)。从南到北,郯庐断裂带依次经过扬子板块、大别-苏鲁造山带、华北克拉通与中亚造山带东部的兴蒙造山带。该断裂带由多条平行或斜向的小型断裂带构成,在东北地区主要有三个断裂组成:长春-哈尔滨断裂、依兰-伊通断裂和抚顺-密山断裂;郯庐断裂在中国巢湖之南大致分成两支,一支中国沿广济—黎塘、宿松—灵山等地进入越南境内,另一支经中国安庆后沿赣江行进(任纪舜等,1980)。

  • 2 郯庐断裂带的岩浆岩活动期次

  • 郯庐断裂带沿线发育大量的中生代岩浆岩(图1)。约139个岩体的锆石U-Pb年龄数据显示郯庐断裂带附近中生代岩浆岩主要划分为三个阶段:晚三叠世(233~200 Ma)、侏罗纪中期(185~155 Ma)和早白垩世(145~105 Ma),并显示出不同的岩浆活动峰期。中酸性岩浆岩显示四个岩浆活动峰,分别在~219 Ma、~180 Ma、~159 Ma和~127 Ma;基性岩浆岩显示三个岩浆活动峰,分别在~213 Ma、~159 Ma和~124 Ma(图2)。

  • 三叠纪中酸性岩浆岩在辽宁地区分布广泛(吴福元等,2005; Ma Qiang et al.,2012; Duan Xiaoxia et al.,2014; 宋运红等,2015; Quan Yikang et al.,2020; Fang Wei et al.,2021; 彭游博等,2020),在胶东地区仅局部出露(Yang Kuifeng et al.,2012; Zhao Zifu et al.,2012),目前在华北克拉通东南部(安徽及大别地区)未曾发现该时期的岩浆作用,侏罗纪和白垩纪中酸性岩浆岩在上述三个地区均有分布(Wang Qiang et al.,2007; Xu Haijin et al.,2007; Tang Huayun et al.,2008; Goss et al.,2010; Liu Shengao et al.,2010; 牛漫兰等,2010; Zhang Chao et al.,2010; He Yongsheng et al.,2011; Yang Jinhui et al.,2012; Yang Kuifeng et al.,2012; Cai Yachun et al.,2013; 曹光跃等,2014; Kang Yuelan et al.,2021a2021b2024)。

  • 图1 郯庐断裂带沿线中生代岩浆岩时空分布简图(据Kang Yuelan et al.,2024改绘)

  • Fig.1 Temporal and spatial distribution of Mesozoic magmatic rocks along the Tanlu fault zone (modified after Kang Yuelan et al., 2024)

  • 岩石圈厚度据文献Liu Mingqi and Li Zhonghai,2018; 新生代玄武岩地幔橄榄岩捕虏体的位置据文献Wang Chunguang et al.,2018

  • lithospheric thickness of the NCC after Liu Mingqi and Li Zhonghai, 2019; the locations of the mantle peridotite xenoliths in Cenozoic basalts after Wang Chunguang et al., 2018

  • 中生代基性岩在郯庐断裂带附近分布有限,不同时代基性岩的分布范围也不同。三叠纪基性岩仅在辽宁和山东局部地区分布;侏罗纪基性岩除辽宁地区晚侏罗世的基性岩出现外,其他地区尚未发现;相比较而言,白垩纪的基性岩浆岩分布广泛。郯庐断裂带附近地区晚三叠世基性岩浆岩主要分布在辽东半岛的弟兄山岩体、于屯岩体、韩家岭岩体附近(Wu Fuyuan et al.,2005; Yang Jinhui et al.,2007; Ma Qiang et al.,2012; 彭游博等,2020; Quan Yikang et al.,2020; Fang Wei et al.,2021),最早为227 Ma的煌斑岩(Duan Xiaoxia et al.,2014)。在山东地区茬山岩体附近也有少量的三叠纪基性岩浆岩,岩性为辉长岩和玄武岩等(Zhao Zifu et al.,2012)。侏罗纪的基性岩仅在辽宁地区被发现,岩浆作用时间是162~155 Ma(Jiang Yaohui et al.,2010; Zhang Xiaohui et al.,2014; Wan Le et al.,2019)。从早白垩世开始,断裂带及邻区基性岩浆活动逐渐增多,在辽宁弟兄山、五龙和于屯等地均有发育(吴福元等,2005; Pei Fuping et al.,2011; Wan Le et al.,2019; Liu Yan et al.,2020),在山东省主要分布于济南、邹平、莱芜、沂南、威海、荣成、青岛、日照等地,其岩性主要为辉长岩及零星的玄武岩,其就位年龄为144~111 Ma(Liu Shen et al.,2008; 2009; Tang Huayun et al.,2008; Dai Liqun et al.,2012; Ma Liang et al.,2014a2014b; Ma Liang et al.,2016; Deng Jun et al.,2017)。

  • 图2 郯庐断裂带附近地区中生代岩浆岩年龄频率

  • Fig.2 Kernel density estimation and histograms for the ages of Mesozoic igneous rock around the Tanlu Fault zone

  • 图数据来源见附表1

  • Data source are from appendix 1

  • 3 郯庐断裂带沿线不同期次岩浆岩地球化学特征及其成因探讨

  • 郯庐断裂带的中生代岩浆岩SiO2含量范围变化大为43%~79 %(图3a)。大多数三叠纪岩浆岩具高K2O和Na2O含量特征(图3a),Al2O3含量较低,多属于准铝质;大部分属于高钾钙碱性或粗橄玄武岩系列(图3b),具有碰撞后岩浆岩特征。与三叠纪岩浆岩相比,侏罗纪岩浆岩的K2O和Na2O变化大(图3b),Al2O3含量更高,部分属过铝质。白垩纪岩浆岩则多为钙碱性系列(图3)。对于郯庐断裂带沿线中生代中酸性岩浆岩来说,根据Sr/Y比值、Sr、Y和Yb含量(使用Defant and Drummond(1990)对埃达克岩的定义)和Mg#值(Mg#=100×(MgO/40.31)/(MgO/40.31+TFeO/71.844),郯庐断裂带沿线中生代中酸性岩浆岩可分为四种类型:①高Mg#埃达克岩(HMA,通常Sr/Y>20,Y(×10-6)<18,Mg#>45)(玄武岩部分熔融的物质应具有低的Mg#值(通常<45))(Rapp et al.,2003);②低镁埃达克岩(LMA,通常Sr/Y>20,Y(×10-6)<18和Mg#<45);③正常的中酸性岩石(NIF,Sr/Y<20或Sr(×10-6)<400)和④A型花岗岩。

  • 图3 郯庐断裂带附近地区中生代样品(a,TAS图解据文献Middlemost,1994)和SiO2-K2O图解(b,据文献Peccerillo and Taylor,1976

  • Fig.3 TAS (a, after Middlemost, 1994) and SiO2-K2O (b, Peccerillo and Taylor, 1976) diagrams of Mesozoic magmatic rocks along the Tanlu Fault zone

  • 数据来源见附表2

  • Data source are from appendix 2

  • 对于郯庐断裂带沿线中生代基性岩,按照其地球化学特征不同可划分为两大类:一类为基性岩富集大离子亲石元素(LILE)、Pb和轻稀土元素(LREE),而亏损Nb和其他高场强元素(HFSE),同时还具有较低的Nb/U和Ce/Pb比值,总体上与岛弧玄武岩(IAB)特征类似,而该类基性岩从三叠纪到白垩纪均在研究区出现(Yang Jinhui et al.,20072012; Liu Shen et al.,2008; Ma Liang et al.,2014a2014b);另一类为基性岩富集大离子亲石元素(LILE)和轻稀土元素(LREE),但亏损K,并未显示Nb和其他高场强元素(HFSE)的亏损,具有较高的Nb/U和Ce/Pb比值,与洋岛玄武岩(OIB)特征相似,而该类基性岩在研究区仅在122 Ma之后才出现(Ma Liang et al.,2014a2016; Liu Yan et al.,2020)。

  • 三叠纪,辽宁和山东地区同时有埃达克岩和A型花岗岩的侵位。辽宁地区埃达克岩的年龄范围为219~224 Ma(Duan Xiaoxia et al.,2014; Ma Liang et al.,2016; 林波,2017; Quan Yikang et al.,2020; 彭游博等,2020; Fang et al.,2021),A型花岗岩的年龄约为215 Ma(Quan Yikang et al.,2020)。同样地,山东地区埃达克岩的年龄约为211 Ma(Zhao Zifu et al.,2012),A型花岗岩的年龄约为215 Ma(Yang Jinhui et al.,2005)。研究表明,三叠纪埃达克岩主要由克拉通下地壳部分熔融形成(Zhao Zifu et al.,2012; Duan Xiaoxia et al.,2014; Ma Liang et al.,2016)(图4)。A型花岗岩通常被认为是在高温低压的条件下形成,如辽宁地区三叠纪弟兄山岩体显示的A型花岗岩特征,具有高εHft)值(-3.4~+1.2)和较低的δ18O值(5.52‰~7.29‰)值,表明它是由新生大陆地壳部分熔融形成(Quan Yikang et al.,2020)。山东地区三叠纪显示A型花岗岩特征的岩体为甲子山岩体(215 Ma),岩性为正长岩,其Sr和Nd同位素组成与该地区同时代的镁铁质岩脉相似,表明其成因相似。结合正长岩的主微量元素及锆石Hf-O同位素,大别-苏鲁造山带正长岩-花岗岩和超高压变质火成岩在微量元素和放射性同位素特征上普遍相似,表明其成因与俯冲大陆地壳本身有关。因此,三叠纪正长岩来源于造山岩石圈地幔和俯冲大陆地壳在折返阶段的部分熔融,表明俯冲的大陆地壳在大陆碰撞过程中再循环到地幔深处,从而产生了地壳-地幔的相互作用(Zhao Zifu et al.,2012)。Yang Jinhui et al.(2005)对这些岩石进行了地球化学和同位素模拟,表明正长岩可能是由单斜辉石和橄榄石的早期分离结晶,叠加后续少量的地壳物质混染形成。三叠纪基性岩石显示出相对富集的Hf同位素成分,表明这些岩石主要来自克拉通古老的岩石圈地幔。

  • 侏罗纪岩浆的地球化学成分变化范围较大(图3),应该与这些岩石的不同岩浆源区和形成时期的构造背景有关。侏罗纪岩浆岩主要为高钾钙碱性和粗橄玄武岩系列岩石(图3),源区较复杂,包括古老的大陆地壳(李刚等,2019; Li Xinghui et al.,2019; Teng Guoxu et al.,2020)、下地壳底部(王栋,2012; Zhang Xiaohui et al.,2014; 李刚等,2019; Li Xinghui et al.,2019)、富集的岩石圈地幔和软流圈地幔(Jiang Yaohui et al.,2010; Lan Tingguang et al.,2012; Zhang Xiaohui et al.,2014)。

  • 白垩纪,岩浆作用广泛分布于郯庐断裂带附近甚至整个华北克拉通。高镁埃达克岩(HMA)最初产生于~143 Ma(图2、5),代表了拆沉下地壳和下伏地幔物质之间的相互作用(Kang Yuelan et al.,2021a2021b)。这些岩浆的εHft)值和δ18O值变化范围很大。早白垩世岩浆的源区可能是增厚的古老地壳、新生地壳、富集岩石圈或亏损软流圈地幔,但长英质岩浆主要来源于地幔物质上涌引起的地壳物质重熔(Ji Mo et al.,2015; 董洋等,2020; 豆世勇,2020; 宋运红等,2022; Kang Yuelan et al.,2021a2021b)。

  • 图4 郯庐断裂带中生代高Sr/Y比值花岗岩类 YbSN-(Sm/Yb)SN图(a,据文献Ma Qiang et al.,2015)和SiO2-Sr/Y图解(b)

  • Fig.4 YbSN versus (Sm/Yb) SN (a, Ma Qiang et al., 2015) and SiO2 versus Sr/Y diagrams (b) for Mesozoic high Sr/Ygranitoids in the Tanlu Fault

  • SN表示均一化来源的数据,假设岩浆来源于镁铁质下地壳(Yb=1.5×10-6; Sm/Yb=1.87)(Ma Qiang et al.,2015)数据见附表3

  • SN denotes source-normalized data, where the compositions of the assumed sources are mafic lower continental crust with Yb=1.5 ×10-6 and Sm/Yb=1.87 (Ma Qiang et al., 2015) Data source are from appendix 3

  • 在~125 Ma时(图2,图6),A型花岗岩开始产出。此外,~123 Ma之后,出现具有类似洋岛玄武岩(OIB)的基性岩石(Ma Liang et al.,2014a2016; Liu Yan et al.,2020)。这种差异表明,华北克拉通岩石圈地幔的地球化学性质在~123 Ma时发生了根本性转变。产生于三叠纪和早白垩世之间的类似于岛弧玄武岩的基性岩应该是三叠纪期间华南大陆地壳俯冲相关熔体与华北克拉通岩石圈地幔之间的反应形成(Zhao Zifu et al.,2012; Duan Xiaoxia et al.,2014),以及侏罗纪和白垩纪古太平洋板块俯冲产生流体与华北克拉通岩石圈地幔之间的反应产物(Jiang Yaohui et al.,2010; Zhang Xiaohui et al.,2014; Wan Le et al.,2019)。对于具有类似于洋岛玄武岩特征的基性岩石来说,它们可能是俯冲古太平洋板块产生的熔体参与交代、并使华北克拉通岩石圈地幔或软流圈部分熔融的产物(Ma Liang et al.,2016; 郑建平和戴宏坤,2018),因此这类岩石的产生表明华北克拉通的古老的岩石圈地幔开始被年轻新生的岩石圈地幔所取代。

  • 图5 郯庐断裂带附近地区中生代高Sr/Y岩石样品年龄-Mg#图(据Kang Yuelan et al.,2024改绘)

  • Fig.5 Age versus Mg# diagram of the Mesozoic high Sr/Y granitoids from the Tanlu Fault (modified after Kang Yuelan et al., 2024)

  • 数据来源于附表3

  • Data source are from appendix 3

  • 4 郯庐断裂的走滑启动时间与机制探讨

  • 郯庐断裂带的演化可视为同时期华北克拉通东部演化的缩影(朱光等,2018)。侏罗纪期间,仅断裂带南端的大别地区表现为左行走滑运动特征(Wang Yu,2006; Zhu Guang et al.,2012; 朱光等,2016)。该次运动与燕山运动A幕同时,是区域北西-南东向挤压的结果(Davis et al.,2001; Wang Tao et al.,2011; Zhang Changhou et al.,2011),表明华北克拉通东部开始受西太平洋俯冲作用影响。早白垩世初期,郯庐断裂带发生了一次大规模的左旋走滑运动(朱光等,20162018),这与燕山运动的B幕同时(朱光等,2016)。

  • 图6 郯庐断裂带沿线白垩纪A型花岗岩地球化学特征图解

  • Fig.6 Discrimination diagrams of the Cretaceous A-type granitoids from the Tanlu Fault

  • 数据来源于附表4

  • Data source are from appendix 4

  • 由任纪舜先生2013年主编的《国际亚洲地质图》可以看出,中国东部的琉球群岛-吕宋岛链明显被洋底高原压弯(图7),从而推断该洋底高原与欧亚大陆的碰撞是导致郯庐断裂大规模左行走滑的主要原因。该洋底高原火山岩年龄应大于等于郯庐断裂大规模走滑的时代。

  • 我们以白垩纪郯庐断裂沿线地区最早出现的高镁埃达克岩(~143 Ma)为起始,以区域上广泛出现A型花岗岩(~123 Ma)为大型走滑结束,来推算郯庐断裂在早白垩世时期的大型走滑平均运动速率约为3.5 cm/a。

  • 图7 欧亚构造格架简图(据任纪舜等,2013改绘)

  • Fig.7 Outline map showing tectonic framework of Eurasian (modified after Ren Jishun et al., 2013)

  • 5 郯庐断裂与华北克拉通破坏

  • 华北克拉通的破坏不仅指岩石圈变薄,还包含岩石圈地幔的置换,伴随着大规模岩浆作用,强烈的地壳变形(变质核杂岩、伸展和走滑构造)和频繁的地震活动(郑永飞和吴福元等,2009; 郑建平和戴宏坤,2018; 郑永飞等,2018; Liu Jingao et al.,2019; Wu Fuyuan et al.,2019)。华北克拉通的破坏主要发生在中生代(朱日祥等,2012; Zhu Rixiang et al.,2017; 郑建平和戴宏坤,2018; Wu Fuyuan et al.,2019; Liu Jingao et al.,2019),在此期间,至少经历了三个方向的俯冲和挤压(Metelkin et al.,2010; Windley et al.,2010; Pei Junling et al.,2011; 李献华等,2012; Kusky et al.,2014; Zhu Guang et al.,2015; 朱光等,2016; 张岳桥和董树文,2019)。板块俯冲对克拉通内产生的岩浆作用有明显的影响,尤其是在中生代晚期,整个克拉通都受到古太平洋俯冲的影响,这也是华北克拉通破坏的峰期(朱日祥等,20122019)。然而,如果华北克拉通的破坏主要受到板块俯冲改造从而破坏,那么破坏最严重的地方应该发生在最靠近华北克拉通边缘俯冲带的区域。与上述推断不同的是,通过对比新生代地幔橄榄岩在华北克拉通的分布及其地球化学特征,可以发现,离断裂带越近,难熔的古老的原始地幔残留的痕迹就越少(Zheng Jianping et al.,2007; Zheng Yongfei,2012; 郑建平和戴宏坤,2018)。因此,郯庐断裂带是岩石圈地幔转换和置换的优先区域。郯庐断裂这一切割岩石圈深度的大型断裂是导致华北克拉通发生破坏的关键因素,不但使整个华北克拉通东部发生了大规模错动,而且为深部幔源物质的上涌提供了通道(Kang Yuelan et al.,2021b2024),更加有利于热/化学侵蚀,并最后导致沿郯庐断裂大范围的下地壳拆沉(图8)。

  • 6 郯庐断裂带成矿作用

  • 郯庐断裂带两侧分布广泛的固体(金多金属、金刚石等)和能源(油气)矿产(郭文魁等,1982; 赫英等,199619982001; Mao Jingwen et al.,2011; 曾普胜等,2020),在空间上有规律地成群成带分布(图9)。郯庐断裂带在成矿作用中的主要表现为:错移更早期的成矿带(徐嘉炜和马国锋,1992)、控制大量早白垩世金等多金属矿床的分布及形成(宋明春等,2022)、控制中生代—新生代含油气盆地的发育和演化(胡望水等,2003)。

  • 安徽蚌埠—五河地区与山东玲珑地区金矿与晚侏罗世侵入岩有关,可作为被郯庐断裂走滑错移的代表(徐嘉炜和马国锋,1992; 朱光,1999),同时也表明郯庐断裂大型走滑的时间应晚于158.5 Ma(玲珑花岗岩的时代,林博磊和李碧乐,2013)。但胶东地区许多大型金矿多与早白垩世侵入岩有关,比如:郭家岭花岗岩、伟德山花岗岩和崂山花岗岩等多形成于132~109 Ma(图10),主要成矿期为122~105 Ma(宋明春等,2022),略晚于区域上大量A型花岗岩侵位时代(~123 Ma),相当于郯庐断裂大型挤压走滑后的伸展阶段。

  • 图8 中国东部中生代构造岩浆演化模式简图(据Kang Yuelan et al.,2021a改绘)

  • Fig.8 Magmatic-tectonic evolution cartoon of the eastern China during the Mesozoic (modified after Kang Yuelan et al., 2021a)

  • (a)—郯庐断裂带未走滑;(b)—古太平洋板块俯冲到华北克拉通之下,华北克拉通地壳不断增厚,部分岩浆源区受到俯冲板块衍生流体的影响;(c)—壳幔物质之间更频繁的相互作用。此后,郯庐断裂带进入伸展构造背景,形成了一些伸展盆地和正断层。华北克拉通岩石圈地幔逐渐被新的岩石圈地幔所取代

  • (a) —the Tanlu Fault has not experienced strike slip; (b) —the Paleo-Pacific Plate subducted beneath the North China Craton, and the crust of the North China Craton continued to thicken. some magma source areas were influenced by fluids derived from the subducting plate; (c) —there was more frequent interactions between crustal and mantle materials. Afterwards, the Tanlu Fault entered an extensional tectonic background, forming some extensional basins and normal faults. The lithospheric mantle of the North China Craton was gradually being replaced by new lithospheric mantle

  • 图9 郯庐断裂带沿线矿产分布简图(据郭文魁等,1982; 赫英等2002; Mao Jingwen et al.,2011; 曾普胜等,2020改绘)

  • Fig.9 Simplified map showing the distribution of mineral resources of the Tanlu Fault (modified from Guo Wenkui et al., 1982; He Ying et al., 2002; Mao Jingwen et al., 2011; Zeng Pusheng et al., 2020)

  • 图10 郯庐断裂沿线金矿有关的岩体及成矿时代频次图(数据来自宋明春等,2022及其中文献)

  • Fig.10 Kernel density estimation and histograms for the ages of plutons related to gold ore metallogenesis along the Tanlu Fault Zone (compiled from Song Mingchun et al., 2022 and references therein)

  • 7 结论

  • (1)郯庐断裂是中国东部规模最大的一条岩石圈断裂,其走滑启动应和早白垩世(~143 Ma)洋底高原与欧亚大陆的碰撞有关,并在早白垩世以~3.5 cm/y的速率左旋走滑;

  • (2)郯庐断裂这一切割岩石圈深度的大型断裂是导致华北克拉通发生破坏的关键因素,为深部幔源物质的上涌提供了通道;

  • (3)郯庐断裂带两侧有规律地成群成带分布的金矿等多金属矿产,与郯庐断裂大型挤压走滑后(~123 Ma)的伸展背景有关。

  • 致谢:感谢两位匿名审稿人对稿件的审查并提出的建设性意见!

  • 谨以此文庆贺任纪舜先生九十华诞!

  • 附件:本文附件(附表1~4)详见http://www.geojournals.cn/dzxb/dzxb/article/abstract/202501095?st=article_issue

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