• 中文核心期刊
  • 中国科技核心期刊
  • 中国科学引文数据库核心期刊

胶北地体荆山群禄格庄组沉积时代与物源——来自山东沐浴店地区长石石英岩碎屑锆石U-Pb年龄与稀土元素的新证据

张连祥, 刘平华, 田忠华, 周万蓬, 王义龙, 王宏宇, 张文, 张传恒

张连祥, 刘平华, 田忠华, 周万蓬, 王义龙, 王宏宇, 张文, 张传恒. 2021: 胶北地体荆山群禄格庄组沉积时代与物源——来自山东沐浴店地区长石石英岩碎屑锆石U-Pb年龄与稀土元素的新证据. 地质通报, 40(1): 164-188. DOI: 10.12097/gbc.dztb-40-1-164
引用本文: 张连祥, 刘平华, 田忠华, 周万蓬, 王义龙, 王宏宇, 张文, 张传恒. 2021: 胶北地体荆山群禄格庄组沉积时代与物源——来自山东沐浴店地区长石石英岩碎屑锆石U-Pb年龄与稀土元素的新证据. 地质通报, 40(1): 164-188. DOI: 10.12097/gbc.dztb-40-1-164
ZHANG Lianxiang, LIU Pinghua, TIAN Zhonghua, ZHOU Wanpeng, WANG Yilong, WANG Hongyu, ZHANG Wen, ZHANG Chuanheng. 2021: Depositional timing and provenance of the Lugezhuang Formation in the Jingshan Group in the Jiaobei terrane: New evidence from detrital zircon U-Pb ages and rare earth elements of arkose-quartzite in Mayudian, Shandong Province. Geological Bulletin of China, 40(1): 164-188. DOI: 10.12097/gbc.dztb-40-1-164
Citation: ZHANG Lianxiang, LIU Pinghua, TIAN Zhonghua, ZHOU Wanpeng, WANG Yilong, WANG Hongyu, ZHANG Wen, ZHANG Chuanheng. 2021: Depositional timing and provenance of the Lugezhuang Formation in the Jingshan Group in the Jiaobei terrane: New evidence from detrital zircon U-Pb ages and rare earth elements of arkose-quartzite in Mayudian, Shandong Province. Geological Bulletin of China, 40(1): 164-188. DOI: 10.12097/gbc.dztb-40-1-164

胶北地体荆山群禄格庄组沉积时代与物源——来自山东沐浴店地区长石石英岩碎屑锆石U-Pb年龄与稀土元素的新证据

基金项目: 

国家自然科学基金项目《内蒙古西部东阿拉善-狼山前寒武纪变质杂岩多期变质事件》 41672191

《薄片原位独居石LASS与石榴子石微钻取样精细年代学研究:以弓长岭和鲁西孟家屯新太古代变质表壳岩为例》 41972205

中国地质调查局项目《华北陆块中部与东部前寒武纪基础地质调查》 DD20190003

《全国陆域及海区地质图件更新与共享》 DD20190370

详细信息
    作者简介:

    张连祥(1987-), 男, 在读博士生, 古生物学与地层学专业。E-mail: geoffreyzhang1105@163.com

    通讯作者:

    刘平华(1981-), 男, 博士, 副研究员, 从事变质地质学与早前寒武纪地质研究。E-mail: lph1213@126.com

  • 中图分类号: P534.3;P588.34+.1;P597+.3

Depositional timing and provenance of the Lugezhuang Formation in the Jingshan Group in the Jiaobei terrane: New evidence from detrital zircon U-Pb ages and rare earth elements of arkose-quartzite in Mayudian, Shandong Province

  • 摘要:

    荆山群禄格庄组是胶北地体古元古代变沉积岩系最重要的组成部分之一,准确测定其原岩沉积时代与物质源区,对进一步探讨荆山群与粉子山群之间的成因关系具有重要的地质意义。以山东莱阳沐浴店地区出露的禄格庄组长石石英岩为研究对象,通过对长石石英岩中碎屑锆石内部矿物包体、阴极发光图像、LA-ICP-MS U-Pb定年与稀土元素组成的综合研究发现,沐浴店地区禄格庄组长石石英岩的碎屑锆石207Pb/206Pb年龄介于2502~1970 Ma之间,其中最小一组碎屑锆石上交点年龄为2079 Ma,结合沐浴店地区禄格庄组记录了1934 Ma变质年龄,初步限定沐浴店地区荆山群禄格庄组的原岩沉积时代为2079~1934 Ma。综合以上研究及相关数据表明,荆山群禄格庄组、南辽河群里尔峪组和集安群蚂蚁河组的碎屑锆石都具有2200~2100 Ma的单峰年龄;而粉子山群小宋组-祝家夼组、北辽河群浪子山组与老岭群达台山组都以出现大于2500 Ma的峰值年龄为特征。结合胶-辽-吉带的其他地质数据,推测粉子山群小宋组与祝家夼组沉积时可能靠近被动大陆边缘的一侧,而荆山群禄格庄组可能更靠近岩浆岛弧的一侧,二者可能属于同时异相沉积的产物。

    Abstract:

    As the Lugezhuang Formation of Jingshan Group is one of the most important parts of the Paleoproterozoic meta-sedimentary rocks in the Jiaobei terrane, accurate determination of its depositional timing and provenance is of great geological significance for further exploring the genetic relationship between the Jingshan Group and the Fenzishan Group.A comprehensive study on mineral inclusions, cathodoluminescence(CL)images, LA-ICP-MS U-Pb dates, and in-situ rare earth element(REE)compositions of detrital zircons indicates that the age of detrital zircons of the arkose-quartzite of the Lugezhuang Formation in the Muyudian area ranges from 2502 Ma to 1970 Ma, of which the youngest group age of detrital zircons is circa 2079 Ma.Combined with its metamorphic age of circa 1934 Ma of the Lugezhuang Formation, it is preliminary determined that the depositional timing of the Lugezhuang Formation ranges from 2079 Ma to 1934 Ma.On the basis of above and published data, detrital zircons from the Lugezhuang Formation of Jingshan Group, Lieryu Formation of South Liaohe Group and Mayinghe Formation of the Ji'an Group all have a single peak of 2200~2100 Ma.The Xiaosong Formation and Zhujiakuang Formation of Fenzishan Group, Liangzishan Formatin of North Liaohe Group and Dataishan Formation of Laoling Group are all characterized by peak ages greater than 2500 Ma.Combining with geology of the Jiao-Liao-Ji belt, it is speculated that the Xiaosong Formation and Zhujiakuang Formation of the Fenzishan Group might be deposited close to the passive continental margin, while the Lugezhuang Formation of the Jingshan Group might be deposited closer to the magmatic island arc.Therefore, the rocks of Fenzishan Group and Jingshan Group might be simultaneously deposited in different sedimentary facies.

  • 关于国际地层年表中的侏罗系/白垩系界线年龄,在21世纪80年代初国际地学界分别提出了144Ma和130Ma两种方案。英国剑桥大学Harland等[1]提出了侏系系/白垩系界线年龄为144Ma,是用“年龄平摊法”算出的;法国居里大学Kennedy等[2]根据各国海相地层中海绿石年龄的测定结果提出侏罗系/白垩系界线年龄为130Ma [3](包括世界各国20个实验室、136位专家提供的研究成果)。

    对上述2种方案,144Ma(现在国际地层年表修改为145Ma)方案被认为不可取[4]。王思恩等[3]评述中国陆相生物地层的侏罗系/白垩系界线在河北滦平盆地;王思恩等[5]确认130.7Ma为中国陆相地层侏罗系/白垩系的界线年龄。本文依据全国地层委员会组织的滦平盆地中生代地层野外考察时采集的凝灰岩样品,对大北沟组顶部凝灰岩(斑脱岩)锆石实测年龄数据表明:侏罗系/白垩系界线的年龄应在129.9±1.1Ma,该数据与Odin为首的各国专家提出的130Ma方案一致,考虑了法国、英国、前苏联、瑞典、美国的侏罗系/白垩系界线附近地层中多国的海绿石测年数据,建议采用法国侏罗系/白垩系界线为标准[2]

    “国际地层表说明” [6]明确指出,“侏罗系—白垩系界线无疑是所有系(纪)中最成问题的界线之一”。究其原因,无论海相或陆相均未找到沉积连续和化石丰富的界线地层剖面,更未建立层型,使研究者讨论问题缺乏统一的标准。中国陆相侏罗纪—白垩纪地层发育得天独厚,自Grabau于1923年提出“热河生物群”开始,两系界线划分一直存在激烈争论,争论焦点是热河生物群的发展演化和层位归属[7-8]

    中国陆相侏罗系—白垩系相当发育,分布广泛。在中国东部地区主要分布于各种断陷盆地和山间小盆地中。中国侏罗纪和白垩纪的陆相地层中赋存丰富的煤、石油、天然气资源;火山岩地层中含有多种金属矿产,因此,对侏罗纪—白垩纪地层的研究有重要的意义。通过建立“陆相层型”工作[9-22],于冀北滦平盆地火斗山乡张家沟找到了大北沟组-大店子组-西瓜园组沉积连续剖面,该剖面出露完整、化石丰富、无后期构造干扰;该剖面属单一断陷湖盆沉积,以半深湖-深湖相夹扇三角洲相为特征,夹多层火山岩。剖面上发育丰富的多门类化石,富含三尾拟蜉蝣、介形虫、叶肢介、腹足类、双壳类、两栖类龟鳖类、节肢动物虾类、脊椎动物狼鳍鱼、鲟等。特别是张家沟下营榆树下剖面,大北沟组顶部—大店子组底部界线为典型的陆相地层剖面,属单一浅湖相泥岩夹砂岩沉积。经过多学科的综合研究,建立陆相侏罗系—白垩系界线层型,确定界线点位以介形虫Cypridea stenolonga的始现为标志。

    目前侏罗系/白垩系界线附近的生物地层学研究,对地层的划分和对比仍存在不同的意见,例如,以冀北—辽西地区为例,侏罗系/白垩系界线划在义县组底,还是划在义县组之中?这是依然需要研究与讨论的问题。

    陆相侏罗系—白垩系界线过渡地层在冀北滦平盆地分别称大北沟组和大店子组,发育于该地区南部,(从东到西)沿西沟—大北沟—大店子—张家沟—兴隆沟—柏砬沟一线呈带状出露(图 1)。大北沟组剖面位于榆树下村的西侧,起点坐标:北纬40o49' 20″、东经117o12'99″;终点坐标:北纬40o 49' 144″、东经117o 12' 50″,总厚226.95m。出露完好且化石丰富。笔者对冀北滦平盆地侏罗系/白垩系界线附近大北沟组顶部的凝灰岩进行了采样(图版Ⅰ)。

    图  1  冀北滦平县榆树下侏罗系与白垩系界线剖面[23]
    Figure  1.  The section of the boundary between Jurassic and Cretaceous in Yushuxia, Luanping County, Hebei Province
      图版Ⅰ 
    a.滦平县榆树下大北沟组剖面;b.滦平县榆树下土城子组砾岩;c、d.大北沟组采样点;e、f.大北沟组凝灰岩薄片;g、h.大北沟组凝灰岩锆石特征
      图版Ⅰ. 

    下白垩统义县阶(下部)大店子组一段(K1d1)黄褐色厚层细砾岩和含砾粗砂岩

    —————————整合—————————

    上侏罗统大北沟阶大北沟组三段(J3d3)

    27.黄绿色粉砂质泥岩、粉砂岩,夹大量小泥灰岩透镜体。含介形类Eoparacypris surriensis, E.jingshangensis, Torinina obesa, Darwinula leguminellaD.xiayingensis;叶肢介Nestoria pissovi                                                                          10.96m

    26.灰绿色泥岩、粉砂质泥岩,夹灰色薄层泥灰岩和黑色页岩。由下至上发育4个韵律,每一韵律下部为均一的泥岩,上部夹泥灰岩和黑色页岩。含丰富的介形类Luanpingella postacuta, L. dorsincurva, Torinina obesa, Eoparacypris surriensis, E. jingshangensis, E. aff. macroselina, Pseudoparacypridopsis luanpingensis, P. muntfieldensis, P. dorsalta, Limnocypridea subplana, Rhinocypris dadianziensis, R. subechinata, Djungarica sp. 1, Djungarica sp. 2, Darwinula xiayingensi, D. leguminella, D. dadianziensis等;叶肢介Nestoria pissovi, N. xishunjingensis, N. krasinetzi, Pseudograpta zhangjiagouensis, P.dadianziensis, Nestoria sp., Yanshania xishunjingensis, Y. subovata, N. latiovata, P. huodoushanensis;双壳类Arguniella lingyuanensis, A. yanshanensis                                                                                                                        18.27m

    25.厚层土黄色钙质泥岩为底,上覆灰绿色钙质粉砂岩和深灰色钙质泥岩,夹灰黑色钙质泥页岩和薄板状粉砂岩、泥灰岩。含丰富的介形类Luanpingella postacuta, L. dorsicurva, Eoparacypris jingshangensis, E. surriensis, Pseudoparacypridopsis luanpingensis, P. muntfieldensis, Rhinocypris dadianzienis, R. subechinata, Darwinula leguminella, D. dadianziensis, D. xiayingensis等;叶肢介Nestoria xishunjingensis, Keratestheria gigantea, K. longipoda, Pseudograpta zhangjiagouensis, P. dabeigouensis             21.23m

    24.灰绿色粉砂质泥岩和钙质粉-细砂岩,夹深灰色钙质页岩、硅质泥岩和薄层泥灰岩。向上粉砂岩增多。含丰富的介形类Luanpingella postacuta, L. dorsicurva, Eoparacypris jingshangensis, E. surriensis, Pseudoparacypridopsis luanpingensis, P. muntfieldensis, Rhinocypris dadianzienis, R. subechinata, Darwinula leguminella, D. dadianziensis, D. xiayingensis, Djungarica sp. 2等;叶肢介Nestoria xishunjingensis, Keratestheria gigantea, K. ovata                                                                             38.20m

    23.灰黄色、灰绿色中-厚层中-粗粒凝灰质砂岩,层理发育欠佳                                                                             7.94m

    22.灰紫色凝灰角砾岩。角砾粒径小,岩层内分布不均,具有流动构造,横向呈透镜状                                                        1.77m

    ————————整合—————————

    上侏罗统大北沟阶大北沟组二段(J3d2)

    21.黄褐色中薄层钙质粉砂岩、粉砂质泥岩                                                                                                5.43m

    20.黄褐色泥岩夹薄中层粉砂岩。产昆虫Ephemeropsis trisetailis;叶肢介Nestoria pissovi, N. xishunjingensisYanshania xishunjingensis, N. cf. krasinetzi, Pseudograpta cf. dadianziensis                                                          20.18m

    19.灰色中-薄层钙质泥岩,夹黑色页岩和灰黄色粉砂岩。含叶肢介Nestoria pissovi, N. xishunjingensis                                                                                                                      1.39m

    18.黄褐色粉砂岩,夹灰色薄层钙质泥岩。含叶肢介Nestoria pissovi, N. xishunjingensis, N. krasinetzi, N. karaica, N. Rotalaria 11.88m

    17.黄褐色粉砂岩,夹灰色薄层泥灰岩                                                                                                   5.28m

    16.灰褐色硅质页岩和钙质页岩。含叶肢介Nestoria pissovi, N.karaica, N. xishunjingensis, N. rotalaria, N. mirififormis, N. oblongaJibeilimnadia ovata, Yanshania cf. xishunjingensis, Pseudograpta cf. zhangjiagouensis                                                                                                                     1.92m

    15.黄褐色中-厚层中-粗粒长石石英砂岩、块状粉砂岩                                                                                                                                      0.96m

    14.深灰色钙质泥岩和土黄褐色粉砂岩、粉砂质泥岩,夹褐黑色钙质页岩和硅质页岩。含叶肢介Jibeilimnadia ovata, J. curtiovata, J. latiovata, J. elliptica, Nestoria pissoviN. karaica, N. krasinetziN. xishunjingensisYanshania zhangjiagouensis               5.28m

    13.灰黄色中-薄层粉砂岩,夹褐黑色钙质页岩和薄层泥灰岩。含叶肢介Nestoria pissovi, Nestoria sp.及大量植物碎片                      7.25m

    12.褐黑色薄片状硅质泥页岩、褐黄色钙质页岩和灰绿色泥岩,夹粉砂质泥岩,泥灰岩透镜体和薄层凝灰质中粗砂岩。含叶肢介Nestoria xishunjingensis, N. pissovi, N. luanpingensis, N. karaica, N. krasinetzi, Yanshania xishunjingensis, Y. subovata, Y. zhangjiagouensis     7.25m

    11.黄褐色薄-中层粗粉砂岩,夹透镜状细砂岩和硅质泥岩                                                                                                                                           3.02m

    10.灰褐色薄-中层硅质泥岩,夹灰绿色薄层粉砂泥岩。含叶肢介N. pissovi, Yanshania xishunjingensis                                     6.04m

    9.浅灰黄色中-薄层状粗粉砂岩和细砂岩。形成下细上粗的5个旋回                                                                                4.23m

    8.灰褐色薄层状硅质泥岩、硅质页岩,顶部为浅灰色中层凝灰质细砂岩                                                                           2.42m

    7.灰褐色中-厚层状硅质泥岩和黄绿色粉砂质泥岩互层。含叶肢介Yanshania xishunjingensis, Y. subovata, Nestoria cf. reticulata, N. pissovi, N. xishunjingensis, Jibeilimnadia ovata                                                                                                4.23m

    —————————整合————————

    上侏罗统大北沟阶大北沟组一段(J3d1)

    6.灰绿色中-厚层凝灰质砂岩、含砾砂岩与粉砂岩、泥岩互层                                                                                     12.90m

    5.灰绿色厚层含砾粗砂岩与粗砾岩,砾石分布不均,局部透镜状,岩层横向变化较大                                                                                                                                            2.20m

    4.灰绿色中-厚层凝灰质中细粒砂岩、含砾粗夹凝灰质粉砂岩、泥岩,发育斜层理层                                                                                                                                            6.20m

    3.灰绿色砂屑沉凝灰岩,层理发育                                                                                                             3.50m

    2.褐灰色中薄层凝灰质中细粒砂岩、含砾粗夹凝灰质粉砂岩、泥岩互层                                                                                                                                            8.80m

    1.灰绿色、褐灰色中薄层夹厚层凝灰质含砾砂岩、夹薄层沉凝灰岩                                                                                1.50m

    ——————火山喷发不整合——————

    下伏地层:上侏罗统待建阶张家口组灰绿色凝灰岩

    锆石U-Th-Pb同位素测定在北京离子探针中心的SHRIMP-Ⅱ上进行,参照分析流程[24]。原始数据的处理[24-25]和锆石U-Pb谐和图的绘制采用Ludwig博士编写的Squid和Isoplot程序[26]。所扣除普通铅的组成根据Stacey等给出的模式计算得出[27](表 1),同位素比值和年龄的误差为1σ相对误差,206Pb/238U年龄加权平均值为95%的置信度误差。

    表  1  滦平盆地侏罗纪—白垩纪斑脱岩样品(2PDBG-2-1) SHRIMP锆石U-Th-Pb测定结果
    Table  1.  SHRIMP U-Th-Pb results for zircons bentonate(2PDBG-2-1) from the Luanping Basin, Hebei Province
    测点 206Pbc/% U/10-6 Th/10-6 232Th/
    238U
    206Pb*/10-6 206Pb/238U
    年龄/Ma
    207Pb*/235U 206Pb*/238U 误差相关系数
    比值 ±1 比值 ±1σ
    2PDBG-2-1-1.1 0.64 825 446 0.56 14.4 129.0±2.2 0.1136 7.6 0.02022 1.7 0.229
    2PDBG-2-1-2.1 0.57 435 189 0.45 7.77 131.8±2.4 0.128 8.4 0.02066 1.8 0.215
    2PDBG-2-1-3.1 0.21 509 221 0.45 8.93 130.0±2.3 0.1299 7.1 0.02038 1.8 0.248
    2PDBG-2-1-4.1 0.00 545 327 0.62 9.49 130.6±2.4 0.151 9.4 0.02047 1.8 0.195
    2PDBG-2-1-5.1 1.24 595 366 0.64 10.5 129.6±2.2 0.0967 9.6 0.02031 1.8 0.183
    2PDBG-2-1-6.1 0.22 676 395 0.60 12.1 132.6±2.2 0.1311 3.9 0.02079 1.7 0.433
    2PDBG-2-1-7.1 3.45 432 184 0.44 7.52 125.0±2.7 0.054 51 0.01958 2.2 0.043
    2PDBG-2-1-8.1 0.00 836 556 0.69 14.9 132.4±2.2 0.1407 3.4 0.02075 1.7 0.482
    2PDBG-2-1-9.1 0.62 644 337 0.54 11.2 128.3±2.2 0.1128 8.7 0.02010 1.8 0.201
    2PDBG-2-1-10.1 9.71 848 696 0.85 16.3 128.8±3.9 0.074 76 0.02019 3.1 0.041
    2PDBG-2-1-11.1 0.51 789 540 0.71 13.6 127.0±2.1 0.1195 4.4 0.01990 1.7 0.385
    2PDBG-2-1-12.1 0.00 381 192 0.52 6.74 134.9±3.0 0.204 13 0.02115 2.2 0.175
    2PDBG-2-1-13.1 0.00 521 286 0.57 9.11 130.8±2.3 0.145 8.3 0.02049 1.8 0.217
    2PDBG-2-1-14.1 0.41 611 233 0.39 10.9 132.1±2.4 0.1325 4.3 0.02070 1.8 0.424
    2PDBG-2-1-15.1 1.66 744 437 0.61 12.8 126.2±2.2 0.091 15 0.01977 1.8 0.122
    2PDBG-2-1-16.1 0.00 745 430 0.60 13.1 131.1±2.2 0.1444 3.4 0.02054 1.7 0.490
    2PDBG-2-1-17.1 0.00 443 225 0.53 7.63 128.0±2.2 0.1448 4.7 0.02005 1.8 0.379
    2PDBG-2-1-18.1 0.00 940 767 0.84 16.3 129.2±2.1 0.1375 3.2 0.02024 1.6 0.510
    下载: 导出CSV 
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    样品中的锆石晶体呈无色透明-浅黄色自形,粒度多在150~200μm之间,长宽比为2~3。阴极发光图像(CL)显示,锆石具典型的岩浆生长环带,古锆石属于岩浆结晶的产物(图版Ⅰ-gh)。根据可见光图像和CL图像选择合适的位置进行测定,即根据可见光图像剔出裂隙发育和含包裹体较多的颗粒,选取无裂缝、无包裹体的区域;同时根据CL图像,避免测定位置跨越不同世代的混合区域。

    凝灰岩样品(2PDBG-2-1)共测试18颗锆石;其中U含量为381×10-6~848×10-6;个别可达940×10-6;Th含量为184×10-6~696×10-6;个别可达767×10-6;Th/U值为0.21~3.45,个别可到9.71(表 1)。样品2PDBG-2-1测试了18个数据点,15个数据点位于谐和线上(图 2),排除受后期普通铅影响的3个数据点(7.1、10.1、15.1)的年龄值。15个数据点的206Pb/238U年龄为129.9±1.1 Ma,MSWD=0.79,该年龄代表了大北沟组顶部凝灰岩的形成时代。

    图  2  侏罗系与白垩系界线(2PDBG-2-1)锆石U-Pb谐和图
    Figure  2.  Zircon U-Pb concordia diagrams of Jurassic and Cretaceous strata

    (1) 依据生物地层的研究,将中国陆相侏罗系/白垩系界线划在大北沟组与大店子组之间,由此结合前人资料推测,国际海相侏罗系/白垩系界线的年龄应接近130.7Ma。

    (2) 参考前人资料土城子组(后城组)下部年龄为142.6 ± 1.9Ma,中部为139.6 ± 1.5Ma,上部为136.4±1.9~137.3±1.1Ma;张家口组底部锆石年龄为133.7±1.1Ma,张家口组顶部锆石年龄为130.8± 0.7Ma;本文获得大北沟组顶部精确锆石年龄129.9±1.1M,建议将大北沟组顶部凝灰岩(斑脱岩)锆石年龄129.9±1.1Ma视为中国陆相侏罗系/白垩系界线年龄。

    (3) 冀北滦平盆地侏罗系—白垩系同位素年龄测定表明,侏罗系/白垩系界线年龄值可能接近130Ma,而非145Ma。

    致谢: 感谢南京聚谱检测科技有限公司李亮博士、南京宏创地质勘查技术服务有限公司袁秋云与李利博士在实验测试和数据处理过程中提供的帮助;感谢中国地质科学院地质研究所杜利林研究员在论文写作过程中的指导与帮助;感谢两位审稿专家认真审阅了本文,并提出了宝贵的修改意见。
  • 图  1   胶北前寒武纪变质地质简图

    (a据参考文献[1]修改;b据参考文献[24]修改)

    Figure  1.   Simplified geological map of the Jiaobei Precambrian metamorphic basement

    图  2   沐浴店地区前寒武纪地质简图

    Figure  2.   Simplified Precambrian geological map of the Muyudian area

    图  3   胶北地体荆山群与粉子山群地层柱状图

    (据参考文献[25]修改)

    Figure  3.   Stratigraphic column of the Jingshan Group and Fenzishan Group in Jiaobei terrane

    图  4   胶北沐浴店地区荆山群禄格庄组长石石英岩野外露头照片

    a、c—荆山群禄格庄组片理化长石石英岩露头远景照片;b、d—荆山群禄格庄组片理化长石石英中变余砂状构造的露头近照

    Figure  4.   Field photographs showing the outcrops of the arkose-quartzites from the Lugezhuang Formation of Jingshan Group in the Muyudian area of the Jiaobei terrane

    图版Ⅰ  

    a~d.荆山群禄格庄组长石石英岩主要矿物组合:石英+斜长石+微斜长石+白云母;e、f.长石石英岩局部微域石英亚颗粒化。a、c、e为单偏光,b、d、f为正交偏光;Mc—微斜长石;Ms—白云母;Pl—斜长石;Qz—石英

    图版Ⅰ.  

    图  5   胶北沐浴店地区荆山群禄格庄组长石石英岩锆石阴极发光图像与207Pb/206Pb年龄

    Figure  5.   Cathodoluminescence images and 207Pb/206Pb ages of zircons from the arkose-quartzites of the Lugezhuang Formation of Jingshan Group in the Muyudian area of the Jiaobei terrane

    图  6   胶北沐浴店地区荆山群禄格庄组长石石英岩中锆石U-Pb谐和图(a、c、e)、年龄频率直方图(b) 与稀土元素配分模式图

    (d、f,球粒陨石稀土元素数据据参考文献[63])

    Figure  6.   Concordia diagrams (a, c, e), histogram with frequency distribution diagram (b) and CI-normalized REE patterns (d, f) of zircons from the arkose-quartzite from the Lugezhuang Formation of Jingshan Group in the Muyudian area of the Jiaobei terrane

    图  7   胶北沐浴店地区荆山群禄格庄组碎屑锆石稀土元素成因图解

    (岩浆锆石与热液锆石数据据参考文献[71])

    Figure  7.   Genetic diagrams of rare earth elements of detrital zircons from the arkose-quartzites from the Lugezhuang Formation of Jingshan Group in the Muyudian area of the Jiaobei terrane

    图  8   胶-辽-吉带古元古代变沉积岩系碎屑锆石U-Pb年龄频率直方图

    Figure  8.   U-Pb age histogram of detrital zircons from the Paleoproterozoic metasedimentary rocks within Jiao-Liao-Ji Belt

    图版Ⅱ  

    a.碎屑锆石微区含有钾长石、钠长石、石英与磷灰石;b.碎屑锆石微区含有磁铁矿与独居石;c.锆石微区含有石英;d.碎屑锆石微区含有磷灰石;e.碎屑锆石微区含有磁铁矿;f.碎屑锆石边部发育细粒磷钇矿。a-1、b-1、c-1、d-1、e-1与f-1—锆石矿物相图;a-2、b-2、c-2、d-2、e-2与f-2—锆石阴极发光图像;矿物缩写:Kfs—钾长石;Qz—石英;Ab—钠长石;Ap—磷灰石;Mag—磁铁矿;Xt—磷钇矿;Mnt—独居石

    图版Ⅱ.  

    表  1   胶北沐浴店地区荆山群禄格庄组长石石英岩碎屑锆石LA-ICP-MS U-Th-Pb定年结果

    Table  1   LA-ICP-MS U-Th-Pb data of detrital zircons from the arkose-quartzite of the Lugezhuang Formation of Jingshan Group in the Muyudian area of the Jiaobei terrane

    样品分析点 含量/10-6 Th/U 同位素比值 年龄/Ma 谐和度/%
    TotalPb CommonPb Th U 207Pb/206Pb 207Pb/235U 206Pb/238U 207Pb/206Pb 207Pb/235U 206Pb/238U
    第一组(碎屑)锆石:上交点年龄为2459±50 Ma
    D0313-2-31 342.82 1.07 130.03 673.31 0.19 0.164304 0.002192 10.317578 0.183986 0.450324 0.004813 2502 22 2464 17 2397 21 95.80
    D0313-2-47 183.02 0.00 268.32 294.70 0.91 0.160619 0.001868 10.823730 0.167921 0.486757 0.005946 2462 21 2508 15 2557 26 96.16
    D0313-2-87 309.40 0.78 328.79 602.89 0.55 0.160444 0.001869 9.809649 0.140354 0.440455 0.005126 2460 20 2417 13 2353 23 95.63
    D0313-2-09 120.03 0.00 177.57 194.75 0.91 0.159908 0.002233 10.458022 0.175396 0.471245 0.006030 2455 24 2476 16 2489 26 98.60
    D0313-2-67 266.19 1.78 389.10 538.91 0.72 0.152276 0.001734 8.211756 0.105548 0.388657 0.003433 2372 19 2255 12 2117 16 89.24
    D0313-2-49 343.92 12.63 357.36 689.22 0.52 0.150658 0.002692 8.615182 0.259699 0.407798 0.005562 2353 30 2298 27 2205 25 93.69
    D0313-2-64 218.34 0.30 239.97 453.19 0.53 0.148075 0.001869 8.368172 0.129884 0.407292 0.004881 2324 22 2272 14 2203 22 94.78
    D0313-2-20 116.41 1.22 150.86 276.69 0.55 0.146187 0.001701 7.352002 0.118077 0.362078 0.004690 2302 19 2155 14 1992 22 86.55
    D0313-2-53 657.50 62.75 1934.90 2222.35 0.87 0.144087 0.001727 5.553087 0.117791 0.282464 0.006256 2277 20 1909 18 1604 31 70.44
    D0313-2-76 630.68 15.83 706.41 2212.25 0.32 0.143485 0.001546 5.119738 0.113832 0.257597 0.005375 2269 19 1839 19 1478 28 65.11
    第二组(碎屑)锆石:上交点年龄为2079±13 Ma
    D0313-2-52 235.93 3.98 273.76 590.81 0.46 0.137678 0.001501 7.128001 0.117417 0.374441 0.005313 2198 19 2128 15 2050 25 93.26
    D0313-2-81 642.18 54.24 1214.84 4161.04 0.29 0.136880 0.001785 2.846505 0.056165 0.149788 0.002535 2188 23 1368 15 900 14 41.12
    D0313-2-28 126.53 0.32 137.53 276.57 0.50 0.136602 0.001576 7.716779 0.111095 0.407669 0.004613 2184 21 2199 13 2204 21 99.08
    D0313-2-44 76.95 0.62 87.53 161.34 0.54 0.136302 0.001657 7.839649 0.127024 0.415081 0.004799 2181 20 2213 15 2238 22 97.36
    D0313-2-35 143.29 0.61 82.67 360.42 0.23 0.135889 0.001751 7.704244 0.135063 0.408459 0.005016 2176 22 2197 16 2208 23 98.52
    D0313-2-75 149.77 0.16 139.58 326.30 0.43 0.134562 0.001588 7.620064 0.117208 0.408957 0.004929 2158 25 2187 14 2210 23 97.60
    D0313-2-10 482.38 23.66 1317.80 2367.15 0.56 0.134330 0.001780 3.199582 0.080573 0.172532 0.004337 2155 29 1457 20 1026 24 47.61
    D0313-2-84 92.89 0.06 88.97 206.91 0.43 0.133970 0.001810 7.320846 0.112504 0.392638 0.004037 2151 23 2151 14 2135 19 99.26
    D0313-2-74 276.93 1.46 224.14 637.78 0.35 0.133864 0.001656 6.967157 0.100085 0.375887 0.003666 2150 22 2107 13 2057 17 95.68
    D0313-2-50 170.21 0.00 219.74 354.46 0.62 0.133160 0.001591 7.499542 0.116743 0.407521 0.005241 2140 20 2173 14 2204 24 97.02
    D0313-2-85 137.89 0.00 180.45 280.59 0.64 0.133053 0.001704 7.616683 0.123978 0.411433 0.004985 2139 22 2187 15 2221 23 96.12
    D0313-2-36 77.67 0.46 72.97 178.34 0.41 0.132250 0.001602 7.439639 0.122668 0.406332 0.005190 2128 22 2166 15 2198 24 96.71
    D0313-2-63 265.45 1.19 414.77 514.38 0.81 0.131761 0.001575 7.521773 0.130190 0.411246 0.005823 2121 20 2176 16 2221 27 95.32
    D0313-2-65 341.59 4.82 340.22 1137.84 0.30 0.131479 0.001782 5.187172 0.100385 0.284632 0.004460 2118 24 1851 17 1615 22 76.25
    D0313-2-32 152.78 0.00 264.39 315.19 0.84 0.131309 0.001768 7.371154 0.132991 0.405714 0.005864 2117 24 2157 16 2195 27 96.29
    D0313-2-98 457.23 11.00 1071.88 1309.60 0.82 0.130825 0.001408 5.193504 0.090757 0.286554 0.004341 2109 14 1852 15 1624 22 77.02
    D0313-2-71 234.06 2.68 297.62 515.68 0.58 0.130359 0.001431 7.034199 0.105083 0.389615 0.004627 2103 19 2116 13 2121 21 99.13
    D0313-2-82 124.41 0.00 123.98 270.96 0.46 0.130244 0.001897 7.336817 0.136052 0.404550 0.005274 2102 26 2153 17 2190 24 95.81
    D0313-2-58 136.50 0.25 141.51 288.91 0.49 0.129428 0.001591 7.334105 0.125839 0.408718 0.005297 2100 27 2153 15 2209 24 94.81
    D0313-2-01 312.38 1.81 280.30 720.87 0.39 0.130061 0.001780 6.855733 0.110357 0.379755 0.004191 2099 24 2093 14 2075 20 98.86
    D0313-2-23 654.42 26.25 1413.46 2977.29 0.47 0.129830 0.001441 3.474612 0.055092 0.193113 0.002782 2095 20 1521 13 1138 15 54.32
    D0313-2-13 186.54 0.00 216.04 394.58 0.55 0.129672 0.001984 6.992268 0.116930 0.387559 0.005001 2094 27 2110 15 2111 23 99.19
    D0313-2-96 182.33 0.67 131.03 404.27 0.32 0.129591 0.001446 7.400142 0.110540 0.412027 0.004890 2092 25 2161 13 2224 22 93.70
    D0313-2-66 304.14 1.36 279.22 719.83 0.39 0.129266 0.001521 6.781121 0.097513 0.377798 0.003931 2088 16 2083 13 2066 18 98.95
    D0313-2-61 170.17 0.68 119.20 407.20 0.29 0.129148 0.001418 6.853767 0.094391 0.383014 0.004164 2087 14 2093 12 2090 19 99.84
    D0313-2-97 187.33 0.56 287.15 397.07 0.72 0.129036 0.001408 6.998725 0.099370 0.391592 0.004412 2085 20 2111 13 2130 20 97.83
    D0313-2-55 139.88 0.93 124.42 340.33 0.37 0.128695 0.001601 6.690595 0.103271 0.375636 0.004237 2080 22 2071 14 2056 20 98.84
    D0313-2-60 190.80 0.79 339.37 408.51 0.83 0.128626 0.001459 6.813556 0.099223 0.381814 0.003972 2079 20 2087 13 2085 19 99.74
    D0313-2-14 167.57 0.24 177.51 383.14 0.46 0.128087 0.002184 6.822021 0.125776 0.382597 0.005345 2072 29 2089 16 2088 25 99.20
    D0313-2-59 167.79 0.00 154.81 361.52 0.43 0.127481 0.001505 7.168968 0.116551 0.405622 0.005139 2065 21 2133 15 2195 24 93.70
    D0313-2-86 105.78 1.15 150.81 211.31 0.71 0.127495 0.001616 7.677796 0.135224 0.432704 0.005931 2065 22 2194 16 2318 27 87.74
    D0313-2-11 70.37 0.88 72.99 159.44 0.46 0.127561 0.001885 6.759441 0.116143 0.381135 0.004736 2065 26 2080 15 2082 22 99.17
    D0313-2-57 287.93 4.04 218.00 878.11 0.25 0.127559 0.001591 5.610898 0.101228 0.318702 0.004993 2065 22 1918 16 1783 24 86.38
    D0313-2-56 149.98 0.74 97.65 360.03 0.27 0.127369 0.001620 6.851884 0.126089 0.388056 0.005366 2062 23 2092 16 2114 25 97.49
    D0313-2-08 94.77 0.00 89.06 218.67 0.41 0.127179 0.001845 6.779994 0.122767 0.385056 0.005452 2061 25 2083 16 2100 25 98.12
    D0313-2-34 150.44 1.31 146.87 394.73 0.37 0.127225 0.001534 6.106284 0.096410 0.346768 0.004222 2061 21 1991 14 1919 20 93.11
    D0313-2-72 119.08 1.41 114.30 267.10 0.43 0.127132 0.001499 6.904510 0.114025 0.392171 0.005135 2059 20 2099 15 2133 24 96.41
    D0313-2-100 100.66 0.56 117.49 279.20 0.42 0.126977 0.001679 5.634378 0.095122 0.320392 0.003908 2057 23 1921 15 1792 19 87.08
    D0313-2-29 150.98 0.46 170.14 346.40 0.49 0.126841 0.001422 6.707494 0.101827 0.381283 0.004578 2055 20 2074 13 2082 21 98.65
    D0313-2-04 141.22 0.00 111.80 325.40 0.34 0.126677 0.001490 6.795830 0.102651 0.387084 0.004778 2054 21 2085 13 2109 22 97.29
    D0313-2-46 109.47 0.16 139.71 247.76 0.56 0.126579 0.001489 6.545514 0.091722 0.373593 0.003739 2051 20 2052 12 2046 18 99.77
    D0313-2-30 236.30 4.63 268.59 673.96 0.40 0.126402 0.001438 5.520984 0.089065 0.315436 0.004342 2050 20 1904 14 1767 21 86.21
    D0313-2-45 163.68 0.00 307.96 337.33 0.91 0.126440 0.001414 6.755026 0.092084 0.386185 0.004080 2050 20 2080 12 2105 19 97.31
    D0313-2-06 271.95 0.00 378.25 543.49 0.70 0.126308 0.001517 7.121264 0.114679 0.407128 0.005662 2047 21 2127 14 2202 26 92.45
    D0313-2-38 227.49 1.08 217.63 561.20 0.39 0.125912 0.001374 6.269407 0.084963 0.359896 0.003793 2043 14 2014 12 1982 18 97.02
    D0313-2-70 227.69 2.18 239.07 609.93 0.39 0.125931 0.001357 5.928160 0.114806 0.339742 0.005867 2043 14 1965 17 1885 28 92.31
    D0313-2-93 230.47 0.20 135.39 553.11 0.24 0.125901 0.001545 6.932249 0.118064 0.396201 0.005016 2043 22 2103 15 2152 23 94.67
    D0313-2-43 192.75 6.41 94.68 558.26 0.17 0.125800 0.001452 5.605520 0.073844 0.322768 0.003438 2040 20 1917 11 1803 17 88.40
    D0313-2-94 116.16 0.54 133.97 301.64 0.44 0.125769 0.001544 6.366794 0.121898 0.366297 0.006317 2040 22 2028 17 2012 30 98.63
    D0313-2-24 263.74 2.54 269.95 605.95 0.45 0.125735 0.001521 6.697823 0.109861 0.383558 0.005133 2039 22 2072 15 2093 24 97.37
    D0313-2-03 263.55 0.56 337.63 572.38 0.59 0.125684 0.001461 6.588739 0.091199 0.377619 0.003743 2039 21 2058 12 2065 18 98.70
    D0313-2-33 163.85 1.88 243.52 479.73 0.51 0.125695 0.001676 5.660775 0.101356 0.326002 0.004807 2039 23 1925 16 1819 23 89.23
    D0313-2-83 152.72 0.94 216.45 334.60 0.65 0.125514 0.001772 6.663105 0.108612 0.381358 0.004242 2036 25 2068 14 2083 20 97.72
    D0313-2-12 189.03 0.74 236.44 467.08 0.51 0.125483 0.001790 6.044789 0.095650 0.346136 0.004068 2035 25 1982 14 1916 20 94.14
    D0313-2-99 225.47 0.00 224.56 561.57 0.40 0.125434 0.001433 6.446847 0.103639 0.370850 0.004686 2035 20 2039 14 2033 22 99.93
    D0313-2-16 216.90 0.88 310.68 461.83 0.67 0.125267 0.002527 6.830259 0.146509 0.390850 0.006089 2032 40 2090 19 2127 28 95.36
    D0313-2-54 120.61 0.22 134.69 267.34 0.50 0.125241 0.001484 6.769911 0.113505 0.391783 0.005974 2032 21 2082 15 2131 28 95.14
    D0313-2-19 485.14 1.97 472.12 1108.97 0.43 0.124790 0.001392 6.630677 0.101614 0.381643 0.004418 2026 25 2063 14 2084 21 97.12
    D0313-2-39 333.22 5.22 602.04 995.43 0.60 0.124503 0.001400 4.735219 0.073201 0.275088 0.003624 2022 21 1773 13 1567 18 77.48
    D0313-2-68 255.59 0.87 284.35 614.04 0.46 0.124453 0.001338 6.320617 0.091024 0.366225 0.004237 2021 19 2021 13 2012 20 99.52
    D0313-2-22 538.67 13.52 744.82 1810.12 0.41 0.124349 0.001344 4.708030 0.069562 0.272693 0.003374 2020 -14 1769 12 1554 17 76.94
    D0313-2-77 322.81 1.25 402.57 753.05 0.53 0.124305 0.001343 6.306371 0.091075 0.366007 0.004298 2020 20 2019 13 2011 20 99.52
    D0313-2-40 295.40 0.76 144.53 733.29 0.20 0.124216 0.001434 6.679566 0.109809 0.388573 0.005295 2018 20 2070 15 2116 25 95.11
    D0313-2-78 493.17 7.03 587.80 1329.41 0.44 0.124215 0.001348 5.552684 0.081716 0.322434 0.003977 2018 19 1909 13 1802 19 89.29
    D0313-2-92 260.64 0.24 351.51 588.17 0.60 0.124072 0.001615 6.502133 0.103632 0.377317 0.004235 2017 23 2046 14 2064 20 97.67
    D0313-2-07 209.67 0.25 234.60 476.51 0.49 0.123918 0.001557 6.397028 0.096097 0.372078 0.004066 2013 22 2032 13 2039 19 98.71
    D0313-2-91 308.56 0.00 277.66 772.20 0.36 0.123926 0.001649 6.267300 0.096644 0.364332 0.004066 2013 23 2014 14 2003 19 99.47
    D0313-2-25 236.40 0.53 327.02 514.24 0.64 0.123781 0.001528 6.911795 0.111973 0.402036 0.005062 2013 21 2100 14 2178 23 91.78
    D0313-2-95 355.39 2.18 304.76 936.07 0.33 0.123689 0.001384 6.061128 0.085724 0.353956 0.004139 2010 20 1985 12 1953 20 97.18
    D0313-2-02 169.33 0.89 85.77 397.42 0.22 0.123390 0.001556 6.873036 0.116824 0.400887 0.005039 2006 23 2095 15 2173 23 91.66
    D0313-2-79 98.70 0.00 87.82 234.79 0.37 0.123185 0.001539 6.697304 0.109733 0.390841 0.004509 2003 22 2072 15 2127 21 93.81
    D0313-2-89 250.71 0.00 223.02 593.71 0.38 0.123182 0.001450 6.501680 0.102729 0.379676 0.004719 2003 25 2046 14 2075 22 96.41
    D0313-2-21 383.32 1.28 532.27 841.00 0.63 0.122822 0.001358 6.617329 0.091791 0.388683 0.004702 1998 14 2062 12 2117 22 94.07
    D0313-2-17 177.99 0.05 161.26 400.71 0.40 0.122469 0.001633 7.065806 0.117527 0.415358 0.005215 1992 24 2120 15 2239 24 87.60
    D0313-2-73 149.26 0.50 48.18 443.34 0.11 0.121992 0.001520 5.636605 0.100329 0.334491 0.005079 1987 22 1922 15 1860 25 93.61
    D0313-2-18 221.22 0.14 122.81 555.86 0.22 0.121041 0.001451 6.519722 0.115591 0.388207 0.005997 1972 22 2049 16 2115 28 92.79
    D0313-2-80 389.76 2.48 206.56 987.50 0.21 0.120948 0.001443 6.193448 0.091613 0.368775 0.004247 1970 21 2004 13 2024 20 97.28
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    表  2   胶北沐浴店地区荆山群禄格庄组长石石英岩碎屑锆石稀土元素分析结果

    Table  2   Rare earth element composition of detrital zircons from the arkose-quartzite of the Lugezhuang Formation of Jingshan Group in the Muyudian area of the Jiaobei terrane 10-6

    样品分析点 La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu ∑REE Eu/Eu* Ce/Ce* LuN/SmN
    第一组(碎屑)锆石
    D0313-2-31 0.01 6.05 0.03 0.64 1.56 0.34 10.04 3.53 46.40 18.00 90.47 20.65 235.52 43.81 477.06 0.20 54.81 169.37
    D0313-2-47 0.01 42.05 0.18 3.58 6.60 2.13 29.67 8.19 85.86 27.89 120.76 23.70 242.29 40.93 633.84 0.39 71.65 37.36
    D0313-2-87 0.15 13.10 0.27 2.47 3.51 0.67 14.04 4.27 47.18 16.25 72.54 15.12 161.19 27.23 377.99 0.25 12.43 46.77
    D0313-2-09 0.02 50.76 0.30 5.24 8.06 2.77 31.76 8.01 76.60 23.89 96.66 19.92 200.95 34.27 559.21 0.46 50.35 25.61
    D0313-2-67 2.02 39.24 2.00 13.66 13.07 4.45 40.56 11.41 121.88 39.23 175.82 36.89 403.19 69.56 972.98 0.54 4.34 32.06
    D0313-2-49 1.55 22.09 1.77 11.68 13.34 2.86 50.31 14.88 165.78 55.81 245.61 48.77 484.74 79.41 1198.62 0.30 2.87 35.85
    D0313-2-64 3.76 25.26 1.64 11.08 12.83 4.78 60.21 18.06 200.38 65.64 272.90 50.67 498.14 79.75 1305.10 0.44 2.49 37.44
    D0313-2-20 152.38 343.49 35.52 150.74 23.19 1.93 37.63 9.82 98.32 32.82 140.93 27.91 280.91 46.61 1382.19 0.20 1.10 12.11
    D0313-2-53 38.52 486.37 54.03 320.64 227.66 93.49 475.29 135.02 1232.10 313.81 1144.30 212.92 2017.89 280.38 7032.42 0.85 2.17 7.42
    D0313-2-76 9.48 55.81 11.37 74.85 74.81 24.23 166.29 47.77 407.84 101.57 389.96 73.57 716.70 104.37 2258.63 0.64 1.14 8.40
    第二组(碎屑)锆石
    D0313-2-52 1.60 12.61 1.53 12.37 18.15 8.65 86.73 23.85 222.84 61.97 235.80 40.41 389.56 61.73 1177.79 0.55 1.80 20.49
    D0313-2-81 43.36 304.07 61.65 399.62 343.79 139.32 684.97 187.54 1615.76 391.68 1428.82 268.25 2676.41 402.44 8947.67 0.86 1.19 7.05
    D0313-2-28 0.01 11.81 0.05 0.92 2.27 0.27 15.45 5.63 73.19 28.60 137.18 28.49 304.79 50.69 659.35 0.10 64.91 134.27
    D0313-2-44 0.13 8.00 0.30 4.27 6.38 0.58 29.36 8.93 107.60 38.38 170.99 34.16 345.60 58.97 813.66 0.11 7.03 55.71
    D0313-2-35 0.12 9.93 0.14 1.50 2.37 0.47 13.77 5.11 68.84 25.76 117.79 23.85 251.02 43.49 564.15 0.20 16.16 110.67
    D0313-2-75 0.03 14.26 0.04 0.87 2.41 0.12 13.92 4.77 62.02 23.51 109.38 22.65 236.43 40.30 530.71 0.05 82.61 100.67
    D0313-2-10 15.32 130.09 21.09 142.24 146.79 56.42 350.47 98.19 868.72 221.59 796.79 148.57 1376.17 194.60 4567.05 0.73 1.48 7.99
    D0313-2-84 0.02 14.42 0.01 0.30 0.87 0.12 5.96 2.24 32.87 14.26 77.70 18.49 224.54 43.13 434.93 0.12 230.14 297.55
    D0313-2-74 0.23 4.03 0.16 1.28 1.56 0.67 6.72 2.18 27.52 11.41 60.73 14.09 175.17 36.79 342.52 0.54 5.07 142.07
    D0313-2-50 0.00 12.62 0.05 0.83 1.64 0.34 6.20 2.03 23.40 8.56 40.94 9.07 102.67 18.48 226.83 0.29 85.77 68.03
    D0313-2-85 3.51 15.17 1.43 10.85 12.89 2.89 57.58 17.06 198.12 69.52 303.36 58.06 592.11 100.08 1442.65 0.27 1.66 46.78
    D0313-2-36 0.89 16.41 0.52 4.78 8.38 4.76 38.56 10.75 105.20 31.85 133.79 24.82 250.00 41.59 672.30 0.68 5.80 29.88
    D0313-2-63 0.32 27.90 0.56 5.93 9.97 1.86 46.31 15.02 178.89 64.11 288.55 58.52 604.24 100.52 1402.70 0.22 12.59 60.74
    D0313-2-65 3.72 34.78 4.20 26.77 26.17 8.50 77.74 23.74 238.30 75.03 314.36 60.72 604.82 96.39 1595.23 0.53 1.90 22.19
    D0313-2-32 0.03 18.18 0.23 4.29 8.15 1.39 40.44 12.45 147.47 53.74 244.48 49.60 506.84 84.42 1171.72 0.19 23.69 62.38
    D0313-2-98 15.24 88.19 16.46 102.31 96.31 43.33 245.11 75.18 727.60 191.62 712.78 129.15 1230.12 181.47 3854.88 0.82 1.21 11.35
    D0313-2-71 0.74 25.35 1.30 12.77 16.52 3.65 66.36 19.68 227.39 80.00 350.92 67.07 660.40 107.95 1640.09 0.29 4.93 39.36
    D0313-2-82 2.08 18.76 0.78 4.92 4.02 0.22 16.90 5.22 63.27 23.84 111.54 23.27 247.28 42.69 564.79 0.07 3.60 63.90
    D0313-2-58 0.03 9.71 0.11 1.45 2.74 0.22 14.11 5.04 62.78 23.54 111.64 23.49 248.47 42.99 546.35 0.09 23.57 94.36
    D0313-2-01 0.67 10.57 0.69 6.02 9.00 1.66 35.96 11.61 129.72 45.33 197.53 39.83 389.26 62.36 940.21 0.24 3.40 41.74
    D0313-2-23 35.51 215.48 37.34 251.07 252.36 92.62 512.40 134.88 1090.44 256.33 904.34 162.36 1488.38 198.26 5631.77 0.77 1.30 4.73
    D0313-2-13 0.50 14.60 0.42 5.35 7.85 0.40 36.40 12.03 145.59 55.49 254.28 51.69 530.54 89.60 1204.74 0.06 7.35 68.72
    D0313-2-96 0.70 10.49 0.96 5.94 5.28 1.39 19.81 6.48 79.12 29.13 140.09 30.32 334.79 60.75 725.26 0.37 2.63 69.31
    D0313-2-66 0.27 14.46 0.43 4.58 6.60 1.74 28.81 9.47 115.36 42.29 199.54 41.51 439.96 74.57 979.58 0.33 8.36 68.08
    D0313-2-61 0.56 6.28 0.42 5.89 6.90 0.73 23.77 6.35 65.83 22.12 97.61 19.60 205.66 35.50 497.21 0.16 3.01 31.00
    D0313-2-97 2.41 21.84 1.29 9.18 8.95 1.43 37.82 11.67 141.51 53.23 250.64 52.47 561.09 98.95 1252.48 0.20 3.00 66.61
    D0313-2-55 0.66 7.72 0.40 2.77 3.26 0.74 13.93 4.50 55.48 20.67 97.56 20.32 218.25 38.49 484.75 0.29 3.63 71.04
    D0313-2-60 0.09 10.19 0.38 5.62 10.77 0.56 60.28 21.26 264.83 93.64 407.79 76.91 735.08 114.02 1801.43 0.05 7.54 63.79
    D0313-2-14 0.16 7.67 0.48 6.07 8.44 1.72 35.25 10.22 111.47 37.21 157.35 30.72 303.47 50.15 760.39 0.26 4.41 35.78
    D0313-2-59 3.32 21.46 1.50 9.21 5.99 0.89 21.56 5.98 66.10 23.48 110.58 23.75 265.78 50.19 609.77 0.21 2.36 50.49
    D0313-2-86 0.06 16.30 0.29 4.49 6.93 2.24 30.86 8.86 102.06 37.12 171.23 35.07 378.17 66.79 860.50 0.40 15.90 58.03
    D0313-2-11 0.00 4.06 0.05 1.07 2.35 0.04 15.63 5.47 68.95 26.60 119.92 25.10 250.80 41.21 561.26 0.02 25.37 105.54
    D0313-2-57 2.24 21.62 3.24 20.57 19.70 8.03 46.25 13.97 132.13 36.67 145.82 28.42 291.73 46.20 816.60 0.78 1.62 14.12
    D0313-2-56 0.28 3.29 0.37 3.03 6.47 1.19 39.92 15.82 212.78 82.83 394.24 80.56 850.30 141.77 1832.87 0.17 2.10 131.92
    D0313-2-08 0.10 4.75 0.36 5.02 7.84 0.53 35.37 10.25 110.92 38.36 160.51 30.24 286.66 47.37 738.28 0.08 3.68 36.41
    D0313-2-34 0.56 6.42 0.72 6.40 9.24 3.69 40.18 13.21 153.07 48.82 207.75 39.42 386.54 60.50 976.51 0.50 2.11 39.44
    D0313-2-72 0.00 9.46 0.05 1.15 2.96 0.25 19.31 7.16 95.51 37.66 177.81 36.79 380.69 63.86 832.68 0.08 52.60 129.81
    D0313-2-100 0.32 6.78 0.55 5.97 9.21 1.38 50.86 16.45 194.59 70.00 306.21 58.64 593.42 98.39 1412.77 0.15 3.12 64.38
    D0313-2-29 0.04 5.12 0.38 5.93 9.90 2.11 48.83 13.94 153.23 52.18 226.51 43.81 445.16 74.07 1081.20 0.24 4.06 45.09
    D0313-2-04 0.00 2.64 0.07 1.47 4.06 0.09 25.84 9.05 113.98 42.59 190.38 38.24 379.76 62.21 870.40 0.02 10.81 92.25
    D0313-2-46 0.01 19.07 0.09 1.66 3.64 0.18 19.66 6.57 77.38 28.36 128.68 25.73 265.19 44.42 620.62 0.05 66.18 73.46
    D0313-2-30 7.29 37.79 6.03 34.33 25.37 9.34 58.51 17.54 172.53 48.87 201.14 40.74 420.71 65.56 1145.74 0.71 1.31 15.57
    D0313-2-45 0.05 25.41 0.50 8.10 13.09 1.31 56.63 16.77 193.38 67.43 295.66 57.00 575.17 95.84 1406.34 0.13 15.28 44.10
    D0313-2-06 203.90 506.95 65.49 307.77 76.06 2.81 118.62 27.24 236.31 70.62 282.74 54.33 517.15 83.19 2553.19 0.09 1.07 6.59
    D0313-2-38 0.31 5.59 0.38 3.49 6.57 0.65 34.40 11.82 147.64 54.11 250.06 49.91 509.12 83.09 1157.16 0.11 3.40 76.16
    D0313-2-70 0.63 24.37 1.09 7.96 10.19 2.95 24.30 6.50 56.92 14.99 57.88 11.30 115.53 17.48 352.07 0.55 5.66 10.33
    D0313-2-93 0.10 3.72 0.17 1.87 3.38 0.59 18.66 6.36 82.80 32.63 159.81 35.24 400.40 75.32 821.07 0.18 5.40 134.10
    D0313-2-43 0.67 6.92 0.87 6.03 8.31 2.18 31.81 9.07 86.33 24.58 98.90 19.16 195.85 31.10 521.78 0.36 1.89 22.54
    D0313-2-94 1.54 16.63 0.96 6.62 7.85 1.73 35.67 11.78 141.38 51.80 240.16 49.50 523.66 90.04 1179.33 0.27 3.26 69.10
    D0313-2-24 0.20 16.34 0.37 4.45 5.78 0.93 24.29 6.99 74.94 24.97 107.36 21.01 215.95 35.43 539.03 0.21 11.18 36.92
    D0313-2-03 0.11 16.97 0.50 7.65 14.16 0.99 66.24 19.89 222.96 77.93 334.34 64.04 612.02 98.73 1536.52 0.08 9.73 42.00
    D0313-2-33 1.58 13.73 1.53 10.49 11.34 5.03 40.10 13.04 138.52 41.61 171.09 33.08 337.04 54.27 872.46 0.64 1.97 28.82
    D0313-2-83 0.01 18.81 0.11 2.41 5.57 0.45 32.46 11.11 139.97 52.39 237.94 45.88 459.10 74.92 1081.15 0.08 50.63 80.96
    D0313-2-12 0.78 13.94 0.73 6.22 8.54 2.32 36.19 11.41 127.42 44.64 200.03 40.82 417.54 70.77 981.34 0.34 4.13 49.91
    D0313-2-99 0.58 8.26 0.82 5.78 7.96 1.21 36.63 11.73 136.85 48.35 213.50 41.77 424.35 70.59 1008.39 0.18 2.45 53.39
    D0313-2-16 0.26 17.05 0.24 3.13 4.54 1.25 22.72 7.87 101.02 41.14 253.29 45.67 508.78 93.39 1100.34 0.31 15.38 123.97
    D0313-2-54 0.03 15.71 0.26 4.08 7.07 1.16 26.04 6.65 65.30 19.53 81.07 15.39 155.76 26.11 424.15 0.23 18.01 22.26
    D0313-2-19 1.84 20.02 2.64 19.92 22.40 4.35 86.80 25.66 285.16 96.90 431.15 85.42 888.21 145.78 2116.24 0.26 1.84 39.21
    D0313-2-39 4.49 60.44 6.22 40.47 37.70 14.98 94.09 28.31 271.42 75.09 289.58 55.31 549.78 82.56 1610.46 0.73 2.34 13.19
    D0313-2-68 0.80 20.91 0.42 3.52 4.12 0.54 17.27 5.20 57.70 19.68 87.77 18.36 194.73 33.16 464.20 0.17 8.72 48.51
    D0313-2-22 26.11 145.32 24.83 153.31 130.62 53.85 280.46 81.68 766.31 192.87 689.98 124.81 1166.42 157.16 3993.73 0.84 1.28 7.25
    D0313-2-77 0.11 13.94 0.50 7.99 14.73 1.63 66.12 19.28 214.08 71.21 306.08 59.28 587.59 96.85 1459.38 0.13 7.92 39.61
    D0313-2-40 0.24 4.61 0.23 1.82 2.84 0.43 15.28 5.01 62.95 24.08 118.50 26.36 300.89 53.94 617.19 0.16 4.38 114.48
    D0313-2-78 4.66 55.78 5.54 38.30 40.20 14.81 97.18 26.88 238.16 61.90 229.95 43.03 414.92 61.69 1333.01 0.69 2.34 9.24
    D0313-2-92 0.93 29.12 0.73 7.23 9.03 0.82 34.79 10.39 115.33 39.70 176.86 36.17 378.38 65.52 904.99 0.12 8.23 43.70
    D0313-2-07 0.02 12.36 0.25 4.56 9.42 1.08 49.45 15.46 176.36 62.04 267.92 52.08 503.04 83.23 1237.25 0.12 15.06 53.22
    D0313-2-91 0.15 9.22 0.23 2.84 6.05 0.35 36.95 12.67 153.67 56.11 251.50 48.65 484.36 79.33 1142.10 0.05 9.68 78.98
    D0313-2-25 0.47 21.11 0.51 6.22 9.76 1.19 43.36 12.12 130.54 43.36 188.55 36.14 362.50 58.51 914.33 0.15 9.45 36.12
    D0313-2-95 1.37 16.84 1.56 10.31 11.29 3.39 40.14 12.62 145.79 50.51 233.57 48.15 503.70 82.46 1161.69 0.43 2.48 44.01
    D0313-2-02 0.03 2.34 0.07 1.31 3.28 0.28 21.49 7.87 102.98 40.15 190.79 41.08 429.21 73.47 914.38 0.08 8.88 134.96
    D0313-2-79 0.92 9.49 0.39 2.76 2.79 0.25 15.38 4.93 59.97 22.45 101.72 20.91 218.36 36.81 497.14 0.09 3.89 79.40
    D0313-2-89 0.29 13.32 0.11 1.26 2.11 0.21 10.70 3.55 43.42 16.05 75.91 15.96 173.16 29.48 385.53 0.11 18.46 84.25
    D0313-2-21 1.43 42.41 1.29 8.82 8.43 3.27 26.82 7.69 86.13 29.46 135.73 29.77 337.82 60.12 779.18 0.61 7.08 42.94
    D0313-2-17 0.06 8.92 0.15 2.05 4.10 0.40 22.52 7.03 84.63 30.83 141.46 28.70 299.07 49.76 679.68 0.10 16.32 73.05
    D0313-2-73 0.25 1.83 0.29 1.80 1.25 0.58 3.41 1.01 8.68 2.24 8.58 1.63 15.42 2.01 48.97 0.81 1.44 9.72
    D0313-2-18 0.72 8.15 0.52 3.66 5.51 1.15 25.09 8.21 94.99 33.43 153.42 30.65 322.37 53.29 741.17 0.25 3.14 58.27
    D0313-2-80 3.76 20.71 2.97 16.69 12.02 3.77 36.27 11.32 121.60 39.42 174.84 37.11 395.39 65.74 941.63 0.51 1.44 32.93
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  • 刘福来, 刘平华, 王舫, 等. 胶-辽-吉古元古代造山/活动带巨量变沉积岩系的研究进展[J]. 岩石学报, 2015, 31(10): 2816-2846. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201510002.htm
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  • 收稿日期:  2020-08-09
  • 修回日期:  2020-10-04
  • 网络出版日期:  2023-08-15
  • 刊出日期:  2021-01-14

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