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| 1 | 华南构造演化的基本特征显示文摘华南至少经历了4期区域规模的大陆动力学过程,除新元古代和晚中生代具有活动陆缘背景外,均在板块内部发生并完成。华夏块体是一个以新元古代岩石为主体构成的前南华纪基底,不是稳定的克拉通古陆,经历了聚合-裂解-再聚合的复杂构造演化。志留纪发生的板内碰撞-拼合事件使华夏块体与扬子块体再次缝合,形成真正统一的中国南方大陆。在震旦纪—早侏罗世期间,整个华南基本处于陆内滨海-浅海-斜坡环境,内部没有切穿岩石圈的断层,没有大规模幔源岩浆和火山喷发的记录,多次构造变形与岩浆活动均在统一的华南岩石圈之上进行。经过早—中侏罗世的构造体制转换,才演化成为晚中生代西太平洋活动大陆边缘的一部分。从早到晚,华南岩石圈经历了多期、幕式的生长,以侧向增生为主(块体拼合),垂向生长为辅(岩浆上侵)。到晚中生代,在古太平洋板块俯冲和陆内伸展的背景下,形成了独特的华南盆岭构造。长期的板内构造演化和多期的花岗岩浆活动使华南具有很好的成矿条件,成为各种矿产与资源的富集区。新元古代南华纪和晚中生代晚侏罗世—早白垩世是华南最有利的成矿期,尤以后者矿种最多、储量最大。 | 舒良树 | 2012 | 地质通报2012，31，7： | 640 |
| 2 | Tectonics of South China Continent and its implications显示文摘This paper aims at exploring the tectonic characteristics of the South China Continent(SCC)and extracting the universal tectonic rules from these characteristics,to help enrich the plate tectonic theory and better understand the continental dynamic system.For this purpose,here we conduct a multi-disciplinary investigation and combine it with the previous studies to reassess the tectonics and evolution of SCC and propose that the tectonic framework of the continent comprises two blocks,three types of tectonic units,four deformation systems,and four evolutionary stages with distinctive mechanism and tectonic characteristics since the Neoproterozoic.The four evolutionary stages are:(1)The amalgamation and break-up of the Neoproterozoic plates,typically the intracontinental rifting.(2)The early Paleozoic and Mesozoic intracontinental orogeny confined by plate tectonics,forming two composite tectonic domains.(3)The parallel operation of the Yangtze cratonization and intracontinental orogeny,and multi-phase reactivation of the Yangtze craton.(4)The association and differentiation evolution of plate tectonics and intracontinental tectonics,and the dynamic characteristics under the Meso-Cenozoic modern global plate tectonic regime. | ZHANG GuoWei GUO AnLin WANG YueJun LI SanZhong DONG YunPeng LIU ShaoFeng HE DengFa CHENG ShunYou LU RuKui YAO AnPing | 2013 | Science China Earth Sciences2013，56，11： | 88 |
| 3 | Late Mesozoic basin and range tectonics and related magmatism in Southeast China显示文摘在迟了的中生代中间的 JurassicLate 白垩纪期间,盆和范围 tectonics 和 extensional 的联系 magmatism 代表构造设定在由于和平的板 subduction 的东南的中国是普遍的。盆 tectonics 由 post-orogenic 组成(类型我) 并且 intra 大陆人 extensional 盆(类型 II ) 。类型我盆在山麓和 intraland 发展了在期间对早侏罗记,纹理粗糙的陆上的碎屑状的沉积在被扔晚三叠纪。在 intra 大陆人期间形成的类型 II 盆外壳的变瘦并且被 grabens 和 half-grabens 的发展描绘。Graben 盆主要在中间的侏罗记期间被产生并且与 bimodal 火山作用被联系。在 half-grabens 的沉积与 rhyolitic 凝灰岩和熔岩被设置并且近来是在有优势的年龄的早白垩纪 CretaceousPaleogene 红床。范围由 granitoids 和 bimodal 组成暴烈的岩石, A 类型花岗石和屋顶类型变形核心建筑群。作者分析了 lithological, geochemical 和迟了的中生代火的岩石集合的 geochronological 特征并且在形成华南的盆和范围 tectonics 上建议了一些地球动力学的限制。类似的比较和在东方、西方的岸之间的盆和范围 tectonics 的差别和平被做,并且东南中国块的地球动力学的进化模型在迟了的中生代期间被讨论。学习结果建议华南在合拢的中生代前上开发了的在内的盆和范围岩层系上带子从自从迟了的中生代,西方的和平的板的 subduction 主要抑制的多相的构造进化被导出,在一个背弧 extensional 背景导致各种各样的 magmatism 的形成。它的 geodynamic 机制能在东方岸与盆和范围 tectonics 的作比较和平。在两岸之间的盆和范围 tectonics 的差别和平例如披风羽毛形成, extensional 和火的岩石集合和盆和范围 tectonics 的年龄可伸缩,主要被 Yellowstone 披风羽毛在太平洋的东方岸引起。 | Dezi Wang Liangshu Shu | 2012 | Geoscience Frontiers2012，3，2： | 60 |
| 4 | 中上扬子地区晚奥陶世岩相古地理及其油气地质意义显示文摘中上扬子地区上奥陶统主要发育庙坡组、宝塔组、临湘组(涧草沟组)、五峰组和观音桥组。笔者通过对研究区野外露头及钻井剖面的考察,总结前人研究成果,利用岩石学、古生物学、生态学及室内分析等方法将其划分为潮坪相、浅海陆棚相和深水盆地相3种沉积相类型。潮坪相以沉积灰岩、白云岩、钙质粉砂岩和粉砂岩等为特征。浅海陆棚相主要沉积龟裂纹灰岩、瘤状灰岩、页岩和粉砂质页岩。深水盆地相主要岩性为黑色碳质页岩、粉砂质页岩与硅质页岩,产以营漂浮生活的笔石为主的生物组合。岩相古地理研究表明,晚奥陶世桑比—凯迪早中期,受加里东构造运动影响,华南板内碰撞挤压作用显著,汉南隆起、川中隆起、川西—滇中—黔中—雪峰隆起不断抬升扩大,中上扬子地区表现为海平面相对上升,原本镶边型碳酸盐台地被淹没,沉积了大范围的浅海陆棚相龟裂纹灰岩和瘤状灰岩。凯迪晚期—赫南特期,隆起面积继续扩大,构造围限作用加剧,中上扬子地区发育大面积黑色碳质页岩、粉砂质页岩和硅质页岩。尤其川东南宜宾—泸州,川北旺苍—南江及黔北渝东武隆道真地区五峰组黑色碳质和硅质页岩,具很好的生烃潜力,应视为下一步烃源岩及页岩气勘探开发的重点研究区域。 | 牟传龙 葛祥英 许效松 周恳恳 梁薇 王秀平 | 2014 | 古地理学报2014，16，4： | 50 |
| 5 | Onset of the Kwangsian Orogeny as evidenced by biofacies and lithofacies显示文摘The onset timing of the Kwangsian Orogeny might differ among localities across South China.Refined stratigraphic works at different localities are necessary to reveal the details of this likely distinction.Recently,we recollected some graptolite specimens from the Ordovician Shixing and Longtouzhai formations(corresponding to the Longxi Formation of southern Jiangxi Province) at many localities in Guangdong Province.The palaeontological and biostratigraphical studies of these graptolite faunas indicate that the facies change from graptolitic shale to nearshore shallow-water,coarse clastics in Guangdong is slightly earlier than that in southern Jiangxi.This timing difference may imply a northward progression of the Kwangsian Orogeny.Based on the biostratigraphy and palaeontology of the Ordovician in the Zhujiang Basin(western part) and Chiangnan Slope Belt(including western Fujian,eastern Guangdong,northern Guangxi,northern Hunan,northeastern Jiangxi,southern Anhui,and western Zhejiang),the Sandbian to late Katian distribution and replacement of biofacies and lithofacies in the two regions are proposed and discussed,which display distinct features at different stages of the Kwangsian Orogeny. | CHEN Xu ZHANG YuanDong FAN JunXuan TANG Lan SUN HaiQing | 2012 | Science China Earth Sciences2012，55，10： | 31 |
| 6 | 川南地区五峰组—龙马溪组页岩笔石带对比及沉积特征显示文摘四川盆地南部长宁与威远区块是我国页岩气主要产区之一,主要产气层上奥陶统五峰组—下志留统龙马溪组富有机质页岩厚度介于20~40 m,具有良好的可对比性,然而,从笔石地层的角度分析后发现,上述2个区块黑色富有机质页岩的沉积时间和沉积速率均存在着明显的差异。为此,应用沉积学、生物地层学、地球化学和矿物学等研究手段,开展了上述2个区块8口钻井的岩心描述和笔石生物地层划分等工作。研究结果表明:(1)长宁地区的富有机质页岩主要沉积于WF1—LM4笔石层段,而威远地区则主要沉积于LM1—LM8笔石层段,二者富有机质页岩的沉积时间差异较大;(2)受广西运动的影响,富有机质页岩的沉积中心不断向北(威远地区)迁移,越靠近南部的海岸线,富有机质页岩沉积结束的时间就越早;(3)威远地区局部缺失观音桥组下部和部分笔石带,发育水下古隆起(赫南特冰期或已隆出水面),其边界目前尚未明确,影响了富有机质页岩的沉积,在该区域进行页岩气勘探部署需格外谨慎。 | 梁峰 王红岩 拜文华 郭伟 赵群 孙莎莎 张琴 武瑾 马超 雷治安 | 2017 | 天然气工业2017，37，7： | 34 |
| 7 | 从板缘碰撞到陆内造山:华南东南缘早古生代造山作用演化显示文摘华南的广西运动被认为是发生在早古生代的陆内造山作用,然而触发陆内变形的地球动力学机制仍然不清.广西运动形成了泥盆系与下伏岩石之间广泛的不整合面以及分布在局部地区的下古生界内部的多个不整合面.广西运动期间的构造热事件和古生物响应时间在460~380Ma,时间上对应于奥陶系和泥盆系之间的多个不整合,而分布在华南南缘的寒武系和奥陶系之间的不整合面(郁南运动)仅与少量的530~480Ma之间的变质事件相当,但是却同步于广泛分布在东冈瓦纳北缘的造山事件.华南南部寒武系-奥陶系不整合面上下的碎屑锆石年代学研究表明,早古生代华南与印度北缘相连,而三亚地块在寒武纪是澳大利亚西缘的一部分,直到奥陶纪才与华南拼合,同步于冈瓦纳最终的聚合.郁南运动之后,华夏板块处于冈瓦纳内部,来自冈瓦纳东缘造山作用的应力向大陆内部传播,在具有弱流变学性质的南华盆地聚集,导致盆地构造反转,触发了广西运动.早古生代的华南经历了从板缘碰撞(郁南运动)到陆内造山(广西运动)的演化过程. | 徐亚军 杜远生 | 2018 | 地球科学2018，43，2： | 33 |
| 8 | Tracking shallow marine red beds through geological time as exemplified by the lower Telychian (Silurian) in the Upper Yangtze Region,South China显示文摘Marine red beds occur frequently in China through geological time.Despite their complex environments,the red beds are found in three depositional settings:1) oceanic,deep water,as in the Upper Cretaceous of southern Tibet;2) outer shelf,deeper water,as in the Lower-Middle Ordovician of South China;and 3) inner shelf,shallow water,as in the Silurian and Triassic in South China.The Silurian marine red beds are recurrent in the lower Telychian,upper Telychian,and upper Ludlow.This paper is to document the marine nature of the lower Telychian red beds (LRBs) in the Upper Yangtze Region and to discuss the spatial and temporal distribution of the LRBs and their depositional environments.The LRBs are best developed on the north side of the Cathaysian Oldland,which can be interpreted as the source area.It is inferred that they were deposited during a marine regression,characterized by the lack of upwelling,low nutrition and organic productivity with a decrease of biodiversity and a high rate of sedimentation.The iron-rich sediments may have been transported by rivers on the oldland into the Upper Yangtze Sea,as rates of deposition were rapid enough to counteract normal reducing effect around sediment-water interface.The LRBs are different from the off-shore,deeper water red beds of lower Telychian in Avalonia and Baltica and further from the oceanic,deep water red beds of Upper Cretaceous in southern Tibet chiefly in palaeogeographic settings,biotic assemblages and marine environments. | RONG JiaYu WANG Yi ZHANG XiaoLe | 2012 | Science China Earth Sciences2012，55，5： | 25 |
| 9 | 湖南NW向常德-安仁断裂的地质特征、活动历史及构造性质显示文摘常德-安仁断裂是湖南东部一条NW向大断裂,关于其地质特征、活动历史及构造性质等尚缺乏系统研究.基于区域地质调查和基础地质研究资料,总结了常德-安仁断裂的总体特征,重塑了断裂的活动历史,探讨了断裂的构造性质和变形机制.主要认识如下:常德-安仁断裂走向NW330°,为一基底隐伏断裂,地质上表现为一NW向岩浆隆起带.该断裂为贯穿中、下地壳并切入岩石圈地幔的深大断裂,断裂倾向NE,倾角约54°.断裂具有长期活动历史:新元古代冷家溪期作为转换断层具走滑活动;冷家溪末期武陵(晋宁)运动中在区域S-N向挤压下右行走滑;板溪期早期和南华纪早期均具伸展活动并控制沉积相带的展布;加里东运动中在区域S-N向挤压下右行走滑;中三叠世晚期印支运动中在区域NW-NWW向挤压下左行走滑兼逆冲;晚三叠世-早侏罗世在区域S-N向挤压下右行走滑;中侏罗世晚期早燕山运动中在区域NWW向挤压下左行走滑;白垩纪-古近纪产生伸展活动.常德-安仁断裂在冷家溪期可能为一横切扬子陆块东南缘弧后盆地、岛弧和华南洋的转换断层.印支运动中断裂带因深部逆冲活动而构造隆升.该断裂具隐伏特征的原因可能与冷家溪期-南华纪同沉积活动、震旦系底部滑脱层发育、多条NE-NNE向大断裂的截切以及断裂沿线花岗岩体和断陷盆地的发育等有关. | 柏道远 李银敏 钟响 李彬 黄乐清 伍贵华 李超 姜文 | 2018 | 地球科学2018，43，7： | 24 |
| 10 | 湖北恩施太阳河奥陶纪-志留纪之交沉积间断的研究显示文摘依据湖北恩施太阳河灯草坪奥陶系—志留系剖面的生物地层学和岩石学的研究,该剖面的沉积间断发生在Paraorthograptus pacificus带至Coronograptus cyphus带之间,共缺失5个笔石带。奥陶系、志留系之间黏土岩矿物分析显示,在奥陶系、志留系之间出现有高岭土,推断在其间可能上升为陆地。具体演变过程为:在晚奥陶世晚期P.pacificus带之前,该区属于黑色笔石页岩沉积环境;在P.pacificus带(也可能略早),该区抬升,形成水下高地,其沉积环境达到了水下风化面,出现了生物扰动现象,并伴有一定的水下动力作用;至奥陶纪最晚期—志留纪早期,该区进一步抬升,可能上升为陆地;至志留纪早期C.cyphus带,该区快速下降,恢复到黑色笔石页岩沉积环境。凯迪晚期的全球海平面下降和志留纪早期'华夏古陆'不断向西及西北扩展的耦合作用是导致该区上升为陆地的主要因素。对整个扬子地区奥陶纪-志留纪之交沉积间断的综合分析需要在多个剖面开展进一步的研究工作。 | 王怿 樊隽轩 张元动 徐洪河 M.J. Melchin | 2011 | 地层学杂志2011，35，4： | 21 |
| 11 | Texture and tectonic attribute of Cenozoic basin basement in the northern South China Sea显示文摘Based on the drilling data,the geological characteristics of the coast in South China,and the interpretation of the long seismic profiles covering the Pearl River Mouth Basin and southeastern Hainan Basin,the basin basement in the northern South China Sea is divided into four structural layers,namely,Pre-Sinian crystalline basement,Sinian-lower Paleozoic,upper Paleozoic,and Mesozoic structural layers.This paper discusses the distribution range and law and reveals the tectonic attribute of each structural layer.The Pre-Sinian crystalline basement is distributed in the northern South China Sea,which is linked to the Pre-Sinian crystalline basement of the Cathaysian Block and together they constitute a larger-scale continental block—the Cathaysian-northern South China Sea continental block.The Sinian-lower Paleozoic structural layer is distributed in the northern South China Sea,which is the natural extension of the Caledonian fold belt in South China to the sea area.The sediments are derived from southern East China Sea-Taiwan,Zhongsha-Xisha islands and Yunkai ancient uplifts,and some small basement uplifts.The Caledonian fold belt in the northern South China Sea is linked with that in South China and they constitute the wider fold belt.The upper Paleozoic structural layer is unevenly distributed in the northern South China.In the basement of Beibu Gulf Basin and southwestern Taiwan Basin,the structural layer is composed of the stable epicontinental sea deposit.The distribution areas in the Pearl River Mouth Basin and the southeastern Hainan Basin belong to ancient uplifts in the late Paleozoic,lacking the upper Paleozoic structural layers.The stratigraphic distribution and sedimentary environment in Middle-Late Jurassic to Cretaceous are characteristic of differentiation in the east and the west.The marine,paralic deposit is well developed in the basin basement of southwestern Taiwan but the volcanic activity is not obvious.The marine and paralic facies deposit is distributed in the eastern Pearl River Mouth Basin basement and the volcanic activity is stronger.The continental facies volcano-sediment in the Early Cretaceous is distributed in the basement of the western Pearl River Mouth Basin and Southeastern Hainan Basin.The Upper Cretaceous red continental facies clastic rocks are distributed in the Beibu Gulf Basin and Yinggehai Basin.The NE direction granitic volcanic-intrusive complex,volcano-sedimentary basin,fold and fault in Mesozoic basement have the similar temporal and spatial distribution,geological feature,and tectonic attribute with the coastal land in South China,and they belong to the same magma-deposition-tectonic system,which demonstrates that the late Mesozoic structural layer was formed in the background of active continental margin.Based on the analysis of basement structure and the study on tectonic attribute,the paleogeographic map of the basin basement in different periods in the northern South China Sea is compiled. | SUN XiaoMeng ZHANG XuQing ZHANG GongCheng LU BaoLiang YUE JunPei ZHANG Bin | 2014 | Science China Earth Sciences2014，57，6： | 18 |
| 12 | 下扬子区新生代断陷盆地的构造与形成显示文摘为了揭示下扬子海陆全区新生代断陷盆地的构造特征,进而探讨盆地的形成机理,故对研究区的地震、钻井和地质资料进行系统分析,梳理区内的主要构造地质证据,并在时空上进行对比。垂直盆地走向的区域大剖面构造解析显示,下扬子区由陆至海,盆地范围逐步扩大,断陷充填厚度逐渐增厚,结构趋于复杂,表明盆地的拉伸量和伸展强度自西向东呈增大趋势。受下扬子块体近似楔形几何形状与东部侧向挤压的边界条件约束,块体近南北向侧向扩展,块体内区域伸展,前新生代的基底先存断裂复活,诱发区域张裂作用和盆地沉降,断陷盆地形成受基底-应力两个基本因素制约。下扬子新生代块体的伸展与郯庐断裂的右旋走滑,均为下扬子块体构造形变的地质响应,其动力学机制可用太平洋板块北西向俯冲进行解释。 | 徐曦 高顺莉 | 2015 | 地学前缘2015，22，6： | 13 |
| 13 | 华南板块古生代生物礁及其古地理控制因素显示文摘华南板块在古生代处于中、低纬度,碳酸盐岩类型多样并形成不同时空背景下的多种生物礁建造,生物礁发展序列基本吻合于全球古生代生物礁的宏演化趋势,寒武纪生物群和古生代动物群演化过程中重要造礁生物门类的起源、辐射、灭绝与复苏事件是塑造礁群落基本生态结构的历史因素。寒武纪早期的古杯-藻礁和继之的微生物礁生长区域相当局限;早—中奥陶世的苔藓虫礁、藻礁以及瓶筐石-硬海绵礁群落分异明显;晚奥陶世珊瑚-层孔虫礁以及藻丘建造见于浙赣局限台地及台缘带,而扬子区志留纪兰多维列世生物礁的生长频繁受陆源碎屑岩覆盖;中泥盆世的珊瑚-层孔虫-藻礁群落结构相对稳定,晚泥盆世法门期—密西西比亚纪的微生物礁、苔藓虫-珊瑚礁、宾夕法尼亚亚纪—早二叠世的苔藓虫-海绵-藻礁、中—晚二叠世的珊瑚-苔藓虫-海绵-藻礁可诠释为与生物灭绝事件相关的幕式群落演替。区域构造活动导致的岩相分异和海平面变化显著制约生物礁的时空分布。中—晚奥陶世的偏深水环境、志留纪兰多维列世—早泥盆世早期扬子区整体抬升的古地理格局造成适宜于生物礁生长海域的缩减;泥盆纪较长的温室期促进了生物礁发展,而宾夕法尼亚亚纪—早二叠世偏凉的海洋水体对生物礁的规模影响力度明显。从华南板块古生界整体的视角看,海相碳酸盐岩具有量值优势,海水在时间尺度和空间展布上多维持较高的清澈度,陆源碎屑岩沉积在特定的时间段可视为生物礁生长的主控因素;海平面变化因其幅度有限可在单剖面或区域上控制生物礁群落的纵横迁移,碳酸盐岩沉积区多见基底沉降与沉积补偿速率基本均衡,具备不同规模的浅海相沉积空间,因此水深变化并非起到决定性作用。特定时段碳酸盐岩台地海水的盐度异常可造成大规模白云岩沉积可排除生物礁发育。 | 王建坡 李越 程龙 曾雄伟 王冠 | 2014 | 古生物学报2014，53，1： | 11 |
| 14 | 晚震旦至中奥陶世下扬子被动大陆边缘原型盆地特征显示文摘随着油气二次创业的深入,海相地层已成为油气勘探领域的重点.下扬子沉积了巨厚的海相地层,其原型盆地经历了多期次的构造改造.通过对下扬子边界的讨论,对其进行系统的整体分析.在活动论构造历史观和盆地原型分析TSM工作程式的指导下,通过对下扬子晚震旦至中奥陶世残留地层分布状况以及该时期沉积充填过程的分析,确定了晚震旦至中奥陶世下扬子原型盆地的性质为被动大陆边缘,其特征主要表现在硅质碎屑沉积物、碳酸盐岩沉积物和同生断裂现象等方面.该时期碳酸盐岩台地发育成镶边台地,台地有侧向生长现象和向海盆输入沉积物的舌状凸起,以江南断裂为代表的同生断裂表明盆地沉积物的物源始终是从下扬子内部自西北向东南方向单向搬运,这些均表明晚震旦至中奥陶世为成熟的被动大陆边缘. | 印峰 杨风丽 叶芳 吴哲 吴满 | 2013 | 地球科学(中国地质大学学报)2013，38，5： | 11 |
| 15 | 下扬子地区早古生代晚期前陆盆地沉积特征与盆山过程显示文摘下扬子地区从晚奥陶世开始沉积特征发生了明显转变,从浅海相转变为三角洲相沉积.这一沉积特征转变与早古生代晚期经历的强烈造山事件密切相关.通过下扬子地区晚奥陶世到志留纪沉积序列的沉积学和碎屑锆石年代学研究,揭示沉积盆地的性质及其时空演化过程,探讨沉积盆地发育与造山带隆升剥蚀之间的关系.下扬子地区早古生代晚期沉积学特征从东南向西北岩性由岩屑砂岩变为石英砂岩,粒度由粗粒变为细粒;沉积厚度等值线具有明显的不对称性,靠近东南等值线密,且沉积厚度大;往西北等值线稀疏,且沉积厚度小;沉积中心呈狭长带状分布,并从东南向西北方向迁移;具有前陆盆地的沉积特征.上奥陶统到中志留统的碎屑锆石以900~720Ma的年龄为主,指示物源以下伏新元古代晚期裂谷层序为主;从早志留世高家边组开始,450~420Ma碎屑锆石年龄出现并逐渐增多,表明同造山岩浆岩被剥露地表并开始提供物源;碎屑锆石中没有出现明显的代表华夏地块基底1.9~1.7Ga的特征年龄峰值,表明华夏地块不是下扬子地区早古生代晚期前陆盆地的主要物源区.下扬子地区前陆盆地从晚奥陶世开始沉降,晚奥陶世的构造沉降速率超过了沉积物的供给速率,前渊沉积了巨厚的浅海相泥岩夹粉砂岩和砂岩;晚奥陶世末造山带持续隆升并向西北方向扩展,沉积速率加快,沉积物粒度明显变粗,沉积相也由浅海相转变成三角洲前缘相;早志留世开始埋深较大的同造山岩浆岩开始遭受剥蚀,导致前陆盆地中450~420 Ma的碎屑锆石含量明显增加. | 杨树锋 陈汉林 龚根辉 张耀 孟立丰 | 2019 | 地球科学2019，44，5： | 10 |
| 16 | Multistage Deformation in the Northeastern Segment of the Jiangshao Fault (Suture) Belt: Constraints for the Relationship between the Yangtze Plate and the Cathaysia Old Land显示文摘Multistage deformation events have occurred in the northeastern Jiangshao Fault (Suture) Belt. The earliest two are ductile deformation events. The first is the ca. 820 Ma top-to-the-northwest ductile thrusting, which directly resulted from the collision between the Cathaysia Old Land and the Chencai Arc (?) during the Late Neoproterozoic, and the Jiangnan Orogenic Belt that formed as the ocean closed between the Yangtze Plate and the jointed Cathaysia Old Land and the Chencai Arc due to continuous compression. The second is the ductile left-lateral strike-slipping that occurred in the latest Early Paleozoic. Since the Jinning period, all deformation events represent the reactivation or inversion of intraplate structures due to the collisions between the North China and Yangtze plates during the Triassic and between the Philippine Sea and Eurasian plates during the Cenozoic. In the Triassic, brittle right-lateral strike-slipping and subsequent top-to-the south thrusting occurred along the whole northeastern Jiangshao Fault Zone because of the collision between the North China and Yangtze plates. In the Late Mesozoic, regional extension took place across southeastern China. In the Cenozoic, the collision between the Philippine Sea and Eurasian plates resulted in brittle thrusts along the whole Jiangnan Old land in the Miocene. The Jiangshao Fault Belt is a weak zone in the crust with long history, and its reactivation is one of important characteristics of the deformation in South China; however, late-stage deformation events did not occur beyond the Jiangnan Old Land and most of them are parallel to the strike of the Old Land, which is similar to the Cenozoic deformation in Central Asia. In addition, the Jiangnan old Land is not a collisional boundary between the Yangtze Plate and Cathaysia Old Land in the Triassic. | ZHANG Jin LI Jinyi XIAO Wenxia FENG Qianwen MA Zongjin | 2013 | Acta Geologica Sinica(English Edition)2013，87，4： | 7 |
| 17 | 云开池垌志留纪辉长岩体的年代学、地球化学特征及构造意义显示文摘华南陆块早古生代的构造属性是华南地质研究争论的焦点,主要有洋-陆俯冲/碰撞和陆内构造两种观点之争.而华南陆块早古生代岩浆岩的报道以花岗质岩石为主,对构造指示意义更为明确的同期镁铁质岩浆岩则研究较少,且对已发现的少量早古生代镁铁质岩浆岩的岩石成因也颇具争议.为了更好地限定华南早古生代的构造属性,对云开地区新近识别出的池垌辉长岩体开展了详细的野外地质、年代学和地球化学研究.其SIMS锆石U-Pb年代学测试得到其^(206)Pb/^(238)U加权平均年龄为433.9±1.5Ma,代表其结晶年龄.样品具较低的SiO_2含量(47.81%~48.83%),高的MgO含量(13.02%~14.65%)、Cr含量(278×10^(-6)~356×10^(-6))和Ni含量(120×10^(-6)~184×10^(-6)),富集大离子亲石元素、亏损高场强元素.(^(87)Sr/^(86)Sr)i=0.708 5~0.710 7,ε_(Nd)(t)=-6.0~-8.2,显示EMⅡ型富集地幔的Sr-Nd同位素特征.结合区域Lu-Hf同位素、古生物、古水流等地质资料,云开地区志留纪时期发育一个受古老俯冲交代作用影响的地幔楔,该地幔楔源区在华南广西运动期间才受到热扰动而部分熔融.认为池垌辉长岩是在早古生代华南陆内造山后的伸展背景下由古老俯冲交代地幔楔熔融而成的产物. | 徐畅 王岳军 张玉芝 徐文景 甘成势 | 2019 | 地球科学2019，44，4： | 7 |
| 18 | 巨型花岗岩带与大陆聚合—裂解作用成因联系研究进展显示文摘围绕巨型花岗岩带与大地构造之间的成因联系,回顾了人们对全球超大陆聚合与裂解作用的研究进程,总结了古元古代哥伦比亚超大陆、新元古代罗迪尼亚超大陆、新元古代晚期—早古生代原冈瓦纳大陆以及晚古生代—中生代潘吉亚超大陆形成与演化过程的研究进展,结合收集自中国华南、塔里木、华北、青藏等构造单元的地质资料,分析了四期大陆聚合作用与裂解过程的基本特征和发生时间的不等时性,及其对巨型花岗岩带形成与分布以及矿产资源的制约关系,明确了超大陆演化对巨型花岗岩带及其矿产资源研究的重要意义。同时,提出了已有研究中的若干薄弱环节,对今后可能实现的创新与突破进行了展望。 | 舒良树 王博 | 2019 | 高校地质学报2019，25，2： | 6 |
| 19 | 湘中南中-晚奥陶世硅质岩地球化学特征及其对奥陶纪盆地演化的启示显示文摘湘中南地区奥陶系由“细碎屑岩-硅质岩系-粗碎屑岩”构成,三者厚度变化具有明显的规律性:厚度等值线的展布逐渐趋于北东方向,厚度最大区域向南东方向迁移.区内岭口剖面烟溪组硅质岩SiO2含量(89.08%-94.32%)和Al/(Al+Fe+Mn)值(0.52-0.79)较高,具有轻稀土略富集、无明显铈异常和铕异常的特点;大桥剖面烟溪组硅质岩SiO2含量高(91.74%-95.14%),Al/(Al+Fe+Mn)值为0.34-0.56,具有轻稀土富集、无明显铕异常和间歇性铈负异常、Y/Ho比值低(20.65±1.63)的特点.硅质岩地球化学特征及图解说明其主要为正常海相生物成因,形成于开阔的大陆边缘背景.对比邻近地区相应层位数据发现,湘中南及其邻区中-晚奥陶世硅质岩成因与沉积背景相似,指示其形成于统一盆地中,结合地层等厚度图分析认为,盆地经历了被动大陆边缘-前陆盆地的转换,硅质岩系可能是前陆盆地初始阶段的产物,在其展布范围内无明显热液影响,暗示造成华夏地块抬升的地球动力学来源可能还在该套硅质岩系展布范围的更南部或东南部. | 何垚砚 牛志军 杨文强 宋芳 王晓地 贾小辉 | 2016 | 中国地质2016，43，3： | 6 |
| 20 | Timing of Metamorphism and Provenance of the Metamorphic Basement of the Xiangshan Uranium Orefield, Jiangxi Province, China显示文摘The origin, age and evolution of the Precambrian metamorphic basement of southern China provide useful insights into early crustal development. Here, we present new laser ablation–inductively coupled plasma–mass spectrometry(LA–ICP–MS) U–Pb age data for detrital zircons from five samples of the Precambrian metamorphic basement of the Xiangshan uranium orefield. Two of these samples, from the northern Xiangshan volcanic basin, yielded a total of 140 U–Pb ages that cluster within the Neoproterozoic(773–963 Ma; 79.3% of data points), with the rest being scattered through the Paleoproterozoic and Mesoproterozoic, along with a single Archean age. These ages indicate that this basement material is associated with the Cathaysia Block. In comparison, the 172 concordant ages from the other three samples from the southern part of the Xiangshan volcanic basin cluster within the Neoproterozoic(767–944 Ma; 59.8%) as well as the Proterozoic(37.8%) and the Archean(2502–2712 Ma; 14.5%). These samples are also free of zircons with Grenvillian ages, indicating that these units are associated with the southeastern Yangtze Block. Combining these data with the geochemistry of these units, which suggests that the metamorphosed sedimentary rocks within the northern and southern parts of the Xiangshan basin have a common component from a magmatic island arc that formed during the early Neoproterozoic, we infer that the basin was located along the boundary between the Cathaysian and Yangtze blocks. In addition, the zircons within the samples from the southern and northern parts of the Xiangshan basin show different pre-Neoproterozoic(963 Ma) age populations but similar postNeoproterozoic zircon populations, indicating that the amalgamation of the Cathaysian and Yangtze blocks occurred after the Neoproterozoic(960 Ma), with magmatism peaking at 830 Ma and rifting starting at ~770 Ma, leading to the subsequent deposition(from bottom to top) of the Shenshan, Kuli, and Shangshi formations. | GUO Fusheng SHI Guo YANG Qingkun ZHANG Wanliang XIE Caifu ZHOU Wanpeng ZHANG Jiewei | 2018 | Acta Geologica Sinica(English Edition)2018，92，1： | 6 |
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