Oceanic and Continental Blocks Distribution during Neoproterozoic Early Qingbaikouan Period (1 000-820 Ma) in China
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摘要: 约1 000~820 Ma的新元古代青白口纪早期，全球罗迪尼亚超大陆汇聚的构造环境是中国该时期洋陆分布的主控因素；华北、扬子和塔里木三大陆块均位于当时地球的北半球，三大陆块的外围被边缘海和洋环绕.华北陆块周缘以稳定型的滨浅海沉积为主；而扬子陆块周缘表现为沟-弧-盆体系；塔里木西北缘发育阿克苏活动陆缘，塔里木北东缘和西南缘分别发育库鲁克塔格被动陆缘浅海碎屑岩建造和铁克里克被动陆缘碳酸盐岩建造.环绕华北、扬子和塔里木三大陆块的边缘海和洋内分布有众多裂离地块，多数地块亲扬子和塔里木陆块，如伊宁、敦煌、阿拉善、松潘、罗霄和武夷等；少数亲华北和西伯利亚陆块，如宝音图、锡林浩特、额尔古纳、韩家园、佳木斯和阿勒泰等.Abstract: During Early Qingbaikouan Period, Neoproterozoic (1 000-820 Ma), the structural background of global assembly of the Rodinia supercontinent is the key factor on the pattern of ocean and block in China. The three big blocks, North China, Tarim and Yangtze, located in the Northern Hemisphere at that time and were surrounded by marginal sea/ocean. There occurred several passive continental marginal seas at the periphery of the North China block; the Yangtze block was characterized by arc-basin sediments around the western, northern and southeastern margins; it was active continental margin at the Aksu area developed around the northwestern Tarim block, and passive continental margin at the Kuluketage (clast) and at the Tiekelike (carbonate) grew around the nrotheastern and southwestern part of the block, respectively. In the continental marginal sea and ocean surrounding the three blocks, many massifs had a relationship with the Yangtze and Tarim cratons, such as Yining, Dunhuang, Alxa, Songpan, Luoxiao and Wuyi, and so on. A few massifs had been related to the North China and Siberian cratons, such as Baoyintu, Xilinhot, Ergun, Hanjiayuan, Jiamusi and Altay blocks.
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Key words:
- distribution of ocean and block /
- marginal sea /
- oceanic basin /
- Neoproterozoic /
- stratigraphy
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图 1 中国新元古代青白口纪地层分区、岩石地层序列及其对比
图中的[1] ~ [66]是测年数据文献的编号：[1] 郭灵俊等，2005; [2] 颉颃强等，2008; [3] 李东津等，1997; [4] 李文国等，1996; [5] 李声之，1996; [6] 刘燕学等，2005; [7] 山东省地质调查院，2017; [8] 杜风军等，2015; [9] 陆松年等，2017; [10] Xu et al., 2009; [11] Chen et al., 2004; [12] Zhang et al., 2007; [13] Zhu et al., 2011; [14] 杨雨等，1997; [15] 何世平等，2010; [16] 陆松年等，2017; [17] 徐学义等，2008; [18] 张克信等，2001; [19] 张海迪等，2012; [20] 魏启荣等，2007; [21] 闫全人等，2003; [22] 张宗清等，2002; [23] 闫全人等，2007; [24] 陕西省地质调查院，2017; [25] Geng，2010; [26] 李怀坤等，2003; [27] 湖北省地质调查院，2017; [28] 张国伟等，2003; [29] 陈隽璐等，2008; [30] 第五春荣等，2010; [31] 王宗起等，2009; [32] 陆松年等，2009; [33] 何世平等，2013; [34] 夏代祥等，1997; [35] 辜学达等，1997; [36] 辜平阳等，2012; [37] 何世平等，2012; [38] 谢尧武等.2007; [39] 任光明等.2017; [40] 高林志等，2015; [41] 辜学达等.1997; [42] 张宗清等.1996; [43] 赵风清等.2006; [44] 凌文黎等，2010; [45] 薛怀民等，2011; [46] Peng et al., 2012; [47] 胡正祥等, 2015; [48] 徐学思等，1997; [49] Zhou et al., 2009; [50]张传恒等，2015; [51] 湖南省地质调查院，2017; [52] 汪正江等，2015; [53] 李源等，2017; [54] Li et al., 2009; [55] 张彦杰等，2010; [56] 张恒等，2015; [57] 高林志等，2016; [58] 浙江省地质调查院，2017; [59]本文；[60] 田洋等，2015; [61] Wan et al., 2007; [62] 福建省地质调查院，2017; [63] 彭松柏等，2006; [64] 海南省地质调查院，2017
Fig. 1. The stratigraphic division, sequence and comparison in China during the Neoproterozoic Qingbaikouan Period
图 2 中国新元古代青白口早期(1 000~820Ma)禅陆与盆地分布简图
图 2主要据陆松年等(2014, 2015)、潘桂棠等(2016)和张克信等(2015)资料编绘.图中蓝色的数字编号(1)~(27)是蛇绿岩分布点的测年值，其测年方法与文献出处简要列述如下：(1)Sm-Nd法，李卫东等(2003); (2)SHRIMP法，潘桂棠等(2013); (3)Sm-Nd法，张克信等(2001); (4)Rb-Sr法，殷鸿福和张克信(2003)；(5)SHRIMP法，闫全人等(2007); (6)LA-ICP-MS法，Xiao et al.(2007); (7)Sm-Nd法，董云鹏等(1997); (8)40At/39Ar法，贾承造等(1988)；(9)LA-ICP-MS法，Dong et al.(2012)；(10)LA-ICP-MS法，Penge et al., (2012)；(11)SHRIMP法，Shi et al.(2007); (12)IA-ICP-MS法，Xu et al.(2016)；(13)LA-ICP-MS法，胡正祥等(2015); (14)SHRIMP法，Zhao et al.(2017); (15)LA-ICP-MA法，任光明等(2017); (16)LA-ICP-MS法，Zhou et al.(2009)；(17)LA-ICP-MS法，薛怀民等(2012)；(18)SHRIMP法，Wang et al.(2007); (19)SIMS法，Wang et al.(2015); (20)Sm-Nd法，徐备(1990); (21)SHRIMP法，丁炳华等(2008); (22)SHRIMP法, Zhang et al.(2013)；(23)LA-ICP-MS法，Zhou et al.(2013); (24)LA-ICP-MS法，Yao et al.(2014); (25)SHRIMP法，Wang et al.(2013); (26)SIMS法，Wang et al.(2013); (27)Sm-Nd法，彭松柏等(2006).图中的红色圆圈内的数字编号1~96为青白口纪地层剖面; 1和2.新疆精河县和伊宁市开尔塔斯群剖面；3.特克斯县科克苏林场库什台群剖面；4.新疆巧克逊桑树园巴伦台群剖面；5.新疆都善县帕尔岗塔格西坡帕尔岗塔格群剖面；6.黑龙江呼玛县落马湖店房铁帽山组剖面；7.黑龙江依兰县愚公乡涌泉村黑龙江岩群剖面：8.黑龙江省佳木斯兴东岩群剖面；9.黑龙江海林县东风林场正询正御组剖面；10.吉林省九台市机房沟机房沟岩群剖面；11.新疆乌什县奇格布拉克水泉阿克苏岩群剖面：12.新疆叶城县阿克其克-乌斯坦河咎博查特塔格组剖面：13和14.新疆尉犁县榆树沟和塔里木六场塞纳尔塔格组剖面：15.甘肃肃北县平头山野马街组剖面；16.内蒙古额济纳旗大王山野马街组削面；17.新疆若弟县冰沟南乱石山组剖面；18.新疆且未吐拉万保沟岩群剖面；19.甘肃肃南县祁青乡北大河北大河岩群剖面；20.甘肃肃北县石包城乡虎洞淘其它大坂组剖面；21.内蒙古脚拉善左旗希尼乌索狼山群剖面；22.青海格尔木市野马泉狼牙山组剖面；23.青海省天峻县苏里乡花儿地其它大坂组剖面；24.青海渔源县湟源岩群剖面；25.甘肃榆中县兴隆山兴隆山群剖面；26.青海格尔木万保沟万保沟岩群剖面；27.青海都兰县冰沟狼牙山组剖面；28.青海都兰县沟里乡加嗡门万保淘岩群剖面；29.内蒙古乌海市桌子山西勒图西勒图组剖面；30.内蒙古达尔罕茂明安联合旗白音宝格拉组剖面；31.内蒙古四子王旗巴彦敖包艾勒格庙组剖面；32.山西省广灵县望狐乡望狐村望狐组剖面；33.北京市昌平龙山长龙山组剖面；34.河北任丘长龙山组钻孔剖面；35.江宁凌源县老庄户村长龙山组剖面；36.吉林省白山市红主崖乡二道阳岔马达略组剖面；37.辽宁瓦房店市驼山乡大顶山永宁组削面；38.山东栖霞县寨里于家-陡崖豹山口组剖面.39.山东昌乐县五图镇黑山官庄黑山官组削面；40.山东苍山县黑山官组剖面：41河南卢氏县化关乡步沟-石板上冯家湾组剖面；42.河南栾山县三川白术沟白术沟组剖面；43.安徽凤阳县曹店大郞山曹店组剖面；44.甘肃康县巧河沙湾里-周家坪阳坝岩组剖面；45.陕西略阳县乔子沟乔子沟火山岩剖面：46.陕西商南甚大水沟-涧水沟-马蹄店耀岭河岩组剖面：47.安微金寨县龚店乡郑堂子佛子岭岩群剖面；48.西藏双湖县北西约15 km处阿木岗群剖面；49.西藏东巧县兹格塘错阿木岗群剖面；50.西藏聂荣县聂荣岩群剖面；51.西藏昌都宁多岩群剖面：52.西藏察雅县吉塘区多穷沟酉西岩组剖面；53.西藏昌都县面达乡草曲沟草曲群剖面；54.西藏察隅县古玉乡雅久波密群剖面；55.云南维西县塔城石鼓岩群剖面；56.云南勐海县西定-南勒澜沧群剖面；57.陕西南郑县碑坝马炉沟铁船山组剖面；58.陕西西乡县桥埃沟-戴家河西乡群(兰花石群)剖面；59.陕西南郑县碑坝-四川南江县古玉乡鸭久波密群剖面；60.湖北房县杨坪武当岩群剖面；61.湖北省神农架林区新华乡郑家垭郑家垭组剖面；62.湖北郝归庙湾庙湾岩沮(庙湾蛇绿岩)剖面；63.湖北随州市大洪山花山群(大洪山蛇绿混杂岩)剖面；64.安徽滁州市张八岭张八岭岩群剖面；65.安徽滁州市施家集西冷村张八岭岩群剖面；66.四川芦山甚黄铜尖子黄水河群剖面；67.四川峨边县金水河区烂包坪-金河峨边群剖面；68.四川喜德县冕山登相营群剖面；69.四川盐边甚新街田-新坪盐边群剖面；70.四川会理县菜子园-通安镇菜子园蛇绿混杂岩(通安群/会理群)剖面；71.云南晋宁县柳坝塘村柳坝塘组剖面；72.贵州印江县梵净山梵净山群剖面；73.贵州从江甲路村甲路组剖面；74.广西蘭水县蜂山-罗城红岗山四堡群剖面；75.湖南省桂阳县桥市乡大江边村大江边组剖面：湖南沅陵县马底择冷家溪群剖面；77.湖南石门县杨家坪冷家溪群剖面；78.江西修水县观音阁双桥山群剖面；79.湖南浏阳市冷家溪群剖面；80.安徽休宁县狂柯溪口群剖面；81.浙江萧山市高洪尖-直坞上墅组剖面；82.浙江金华罗店弧火成岩剖面；83.浙江富阳县沈巧双溪坞群剖面；84.浙江陈蔡镇陈蔡水库陈蔡群剖面；85.江西戈阳县周潭乡周潭-洪山尚源岩群剖面；86.江西新余市神山山田村神山组(神山构造混杂岩)剖面；87.江西宜黄县相山陈蔡群剖面；88.江西永丰县潭头乡潭头群剖面：89.福建建廊市马面山群剖面；90.福建戴云山马面山群剖面；91.广西贺州市大宁镇鹰扬关鹰扬关组剖面；92.广西博白县三滩乡白流村山坑顶-门口岭射广组剖面：93.广西北流市石窝镇云开群剖面；94.广东信宜市贵子镇坑坪柯蛇绿混杂岩(云开群)剖面；95.广东信宜市旺沙独墩-怀乡牛下云开群沙湾坪组剖面；96.海南昌江县金牛岭石碌群剖面
Fig. 2. The Distribution diagram of Early Neoproterozoic (1 000-820 Ma) ocean and block in China
图 3 新元古代青白口早期从伊宁地块向南经塔里木陆块至甜水海地块的构造-层序岩相联合剖面
Fig. 3. Jointed profile of tectonic, sequence and facies during the Early Qingbaikouan Period from the Yining massif southward to the Tarim block and Tianshuihai massif
图 4 新元古代青白口早期从明水地块向南经扬子陆块至琼中地块的构造-层序岩相联合剖面
Fig. 4. JoiMed profile of tectonic, sequence and facies during the Early Qingbaikouan Period from the Mingshui massif southward to the Yangtze block and Central Hainan massif
图 5 新元古代早期全球洋陆分布示意
图中黄色的陆块和地块示古中国陆域; 据Li et al.(2008)和陆松年等(2014)修改.图中的沉积和火山建造组合岩性花纹图例详见图 2
Fig. 5. Simplified general paleogeographic diagram of early Neoproterozoic
表 1 对接带与叠接带的区别
Table 1. The differences between convergent and accretional consumption zones
序号 对接带 叠接带 都发育有蛇绿岩带、弧岩浆岩带、双变质带与俯冲增生杂岩带，并行分布 1 缝合带所含蛇绿岩以MORB型为主 缝合带所含蛇绿岩以SSZ型为主 2 蛇绿岩时代分布约2~10亿a 蛇绿岩时代分布约小于2亿a，常小于1亿a 3 缝合带呈狭带状分布数千千米 缝合带呈狭带状分布一般仅数百千米 4 远洋沉积(无陆源碎屑混入的极细粒的硅、灰、锰、炭、凝灰质)发育好 远洋沉积(无陆源碎屑混入的极细粒的硅、灰、锰、炭、凝灰质)发育差 5 缝合带两侧无统一的基底，两侧的陆块基底与盖层组成长期不同 两侧有统一的基底，分隔的两个大陆边缘沉积序列短期内不同 6 分隔的陆块古地磁位置长期各自处于不同位置，并相距远 分隔的陆块古地磁位置相距不大 7 是生物大区(底栖类)的长期分界线，后期混生 不是生物大区(底栖类)分界线 
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表 2 沿江绍-郴州-钦防对接带两侧扬子与华夏青白口纪-志留纪(约1 000~419 Ma)地层特征对比
Table 2. Comparison of the Yangtze and Cathaysian stratigraphic characteristics along the Jiangshao-Chenzhou-Qinfang suture zone during the Qingbaikouan to the Silurian (1 000-419 Ma)
序号 对比点 扬子构造-地层大区 华夏构造-地层大区 1 基底与盖层 晋宁期形成的基底，青白口晚期(约820 Ma)开始沉积盖层发育阶段 加里东期形成的基底，泥盆纪开始沉积盖层发育阶段 2 岩石组合与地层序列 震旦纪-奥陶纪以碳酸盐岩建造为主；含火山物质稀少 青白口纪-早志留世以含凝灰质的板岩、千枚岩、硅质岩、碳质板岩等(原岩为浊积岩和远洋沉积)为主，富含火山物质 以江绍-郴州-钦防大断裂为界，前泥盆纪前扬子和华夏的海相地层序列相差很大；从泥盆纪开始，扬子和华夏的海相地层序列基本相同，对比性好，表明从泥盆纪开始，扬子和华夏才结合成统一的华南陆块 3 地层类型 青白口纪晚期以来为史密斯地层(成层有序) 青白口纪-早志留世以非史密斯地层或洋板块地层发育，发育了活动陆缘地层系统和洋盆地层系统，并发育俯冲增生杂岩 4 地层厚度 小 巨大 5 南华纪裂谷 发育裂谷的双峰式火山岩组合及沉积充填序列 不存在裂谷火山岩组合及沉积充填序列，同期的火山岩主要为活动陆缘弧火山岩或洋岛-海山型火山岩 6 南华纪冰碛建造与震旦纪盖帽白云岩 发育冰碛物及冰水沉积 未发现确切的冰碛物及冰水沉积 发育震旦纪初期回暖的盖帽白云岩 无 7 火成岩建造 除南华纪裂谷期火山岩发育外，震旦纪-志留纪火山建造极少 南华纪-志留纪火山物质多而复杂，主要有：由辉橄岩、橄辉岩、辉石岩、堆晶辉长岩、辉绿岩和玄武岩等构成的洋壳残迹；玄武岩和高镁安山岩构成的洋内弧；洋内地幔热点形成的玄武岩(海山)；基性-中酸性火山岩构成的岛弧和广泛分布的凝灰岩等 8 物源 青白口纪-奥陶纪的物源来自扬子本区；以约820 Ma的碎屑锆石年龄峰值为主；不存在约960 Ma和440 Ma的碎屑锆石年龄峰值 青白口纪-奥陶纪的物源不来自扬子陆块, 而来自南部的活动大陆边缘；不以约820 Ma的碎屑锆石年龄峰值为主，而以960 Ma和440 Ma的碎屑锆石年龄峰值为主 9 化石组合 底栖类为主，类型多而复杂 浮游类为主，类型单调 10 沉积环境 滨浅海为主 半深海-深海为主 11 变质程度 无或极低级变质 低-中级变质 12 构造形变 弱变形 强变形，表现为强劈理化、同斜-紧闭褶皱和叠瓦状逆冲-走滑断层组合 13 地壳特征 青白口纪晚期以来为陆壳 青白口纪-早志留世洋壳发育 14 盆地类型 青白口纪晚期以来主要发育裂谷、陆表海、陆棚-被动陆缘斜坡 青白口纪-早志留世北侧为被动陆缘, 南部为活动陆缘, 之间为多岛洋盆 15 构造环境 青白口纪晚期以来为统一的陆块(克拉通) 新元古代-早古生代不存在统一的“华夏古陆”或“华夏板块”，而是由多岛洋逐步形成的增生造山带
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