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| 1 | 扬子地块西、北缘中元古代地层的划分与对比显示文摘广泛分布于扬子地块西缘和北缘的中元古代地层经历了强烈的变形和绿片岩相的变质改造。根据形成时代,该区的中元古代可以识别出两个阶段,中元古代早期(1.8~1.4Ga)和中元古代晚期(1.4~1.0Ga)。中元古代早期的地层包括大红山群、东川群、河口群和通安组(1~4段),中元古代晚期的地层主要由分布在扬子地块西南缘的昆阳群、会理群和分布于扬子地块北缘的神农架群和打鼓石群组成。新的锆石原位定年结果表明,通安组的凝灰岩形成于1744±14Ma左右,河口群角斑岩形成于1659±23Ma左右,侵入会理群天宝山组的辉长辉绿岩形成于1026±7Ma左右。根据岩石组合、形成环境以及年代学资料,中元古代早期的大红山群、东川群、河口群和通安组(1~4段)形成时代相近,地层组成基本相同,它们都含有与岩浆热液有关的铁氧化物铜金(IOCG)矿床或层状铜矿床(SSC),都在1.75~1.45Ga期间形成于大陆裂解环境。扬子地块北缘的火地垭群也可能属于中元古代早期地层。中元古代晚期地层在扬子地块西缘北缘均有分布,其中的昆阳群和会理群大体形成于1.2~1.0Ga,神农架群和打鼓石群形成于1.4~1.0Ga,它们的顶界可能延伸到新元古代早期。在中元古代晚期的地层中含有大量叠层石,表明它们形成于温暖潮湿的浅海环境。除上述的中元古代晚期地层之外,云南元谋地区的苴林群、川西的登相营群、通安组五段等也属于中元古代晚期的地层。 | 耿元生 旷红伟 柳永清 杜利林 | 2017 | 地质学报2017，91，10： | 59 |
| 2 | 中国中新元古代重要沉积地质事件及其意义显示文摘地球曾经历了3次超大陆演化过程,其中2次超大陆(哥伦比亚(Columbia)和罗迪尼亚(Rodinia))旋回涉及中新元古代,并与一系列区域性事件相联系,形成了多成因的超大陆演化模型。华北中东部新元古代沉积事件、扬子和塔里木新元古代裂谷事件、雪球事件等都被视为Rodinia超大陆的裂解响应,它们对定时三大陆块相互关系及定位其在全球超大陆的位置具有至关重要的作用,也反映了重要沉积地质事件在超大陆研究中不可或缺的作用和意义。此外,在中新元古代的Columbia和Rodinia超大陆演化过程中,还伴随发育具有广泛区域性甚至全球意义的巨厚白云岩与碳酸盐岩微生物(岩)、红层与黑色页岩、全球性臼齿亮晶碳酸盐岩和埃迪卡拉纪盖帽碳酸盐岩等沉积事件群及元素(同位素)漂移等地球化学异常事件,也包括特殊且重要的磷块岩、锰、铁矿等沉积成矿事件。由于不断显示出来在全球古大陆重建和古地理恢复方面的重要作用,它们越来越得到学术界的广泛关注和研究。文中通过系统分析中国中新元古代超大陆旋回演化中发育的部分重要或关键地质事件(群)时空发育与分布特征,并结合作者团队的实际资料和测试数据,以期揭示超大陆演化过程与重要沉积地质事件的内在联系,为超大陆聚散旋回演化和时空定位及原型沉积盆地的发育和评价提供科学证据。 | 旷红伟 柳永清 耿元生 白华青 彭楠 范正秀 宋换新 夏晓旭 王玉冲 陈骁帅 | 2019 | 古地理学报2019，21，1： | 27 |
| 3 | 区域变质作用与中国大陆地壳的形成与演化显示文摘在编制1∶500万中国变质地质图的基础上,本文总结了中国主要变质带的演化以及各变质带与中国大陆地壳形成演化之间的内在联系。虽然在华北和华南克拉通都有古太古代到中太古代的变质年代记录,但是由于后期改造其变质作用的特点及与区域构造背景的联系已难以追索。新太古代末-古元古代初期的变质作用在华北克拉通表现最明显,这期变质作用紧随大规模的TTG岩浆作用,普遍具有逆时针的P-T演化轨迹,反映了地幔柱主导的岩浆-变质事件特点。古元古代晚期的变质事件在华北、华南、塔里木克拉通都有强烈反映。这期变质作用以形成具有顺时针P-T演化轨迹的高压麻粒岩为特点,与形成Columbia超大陆的一些造山带的特点类似,但是这三个不同克拉通在与Columbia聚合的时间和空间方位上存在差异。华南克拉通是相对年轻的克拉通,是沿新元古代江南造山带扬子和华夏地块拼合的产物。新元古代江南造山带的火山岩形成时代和变质作用程度从北东向南西迁移,反映了造山过程逐渐迁移和剪刀式闭合的特点。形成华南克拉通后,在其东南缘又先后经历了加里东期和印支期的变质改造,并且由北西向南东变质带从加里东期转变为印支期,但是这两期变质作用的构造背景尚不很清楚。中国南北大陆的聚合首先从西昆仑-阿尔金-北祁连-北秦岭-桐柏开始,所反映的变质作用是早古生代的蓝片岩相和榴辉岩相变质岩相伴产出,表明经历了从洋壳俯冲到陆陆碰撞的演化过程。中国东部的南北大陆到印支期才最终汇聚,相应的变质作用以南部出现高压蓝片岩相、北部出现超高压的榴辉岩相变质带为特点,表明南方大陆向北方大陆的俯冲。超高压带内普遍含有柯石英,意味着大规模的陆壳深俯冲。华北克拉通和塔里木克拉通以北的中亚造山带内存在多条从早古生代到晚古生代的变质带和多条蓝片岩相变质带,表明这是一个由多阶段、多条变质带组成的造山区。但是其变质作用的空间和时间演化还有待进一步深入。青藏高原变质带具有北老南新的空间分布特点,最北部的印支期龙木错-双湖-澜沧江变质带反映了原特提斯和古特提斯洋的碰撞拼合过程,北部的燕山期班公湖-怒江变质带和中部的喜马拉雅早期雅鲁藏布江变质带反映了新特提斯洋的两次碰撞拼合过程,南部喜马拉雅晚期的高喜马拉雅变质带反映了印度板块向北俯冲导致的高原快速隆升过程。 | 耿元生 沈其韩 杜利林 宋会侠 | 2016 | 岩石学报2016，32，9： | 21 |
| 4 | 扬子克拉通崆岭杂岩新太古代花岗片麻岩成因及其构造意义显示文摘以崆岭杂岩中新太古代花岗片麻岩为研究对象,系统研究了其锆石U-Pb年代学和全岩地球化学特征,并对其岩石成因和扬子陆核~3.0~2.6Ga构造演化过程进行了初步探讨.锆石LA-ICP-MS U-Pb同位素测年结果表明,花岗片麻岩形成年龄为2 673±39Ma,且遭受了古元古代(2 042±27Ma)的高压麻粒岩相变质作用.地球化学研究表明,该套花岗片麻岩富Si,贫Mg、Cr、Ni,具有Eu、Sr和高场强元素的负异常.花岗片麻岩的εNd(t)值在-1.9~-0.1之间变化,对应两阶段Nd同位素模式年龄为3.15~3.01Ga,锆石饱和温度为789~825℃,显示岩体可能形成于初生长英质地壳物质在后碰撞伸展构造背景高温条件下部分熔融.结合前人已有的研究成果,认为以崆岭杂岩为代表的扬子陆核可能完整记录了~2.9~2.6Ga板块俯冲-碰撞-后碰撞与造山作用相关的完整过程. | 邱啸飞 杨红梅 赵小明 卢山松 江拓 段瑞春 刘重芃 彭练红 魏运许 | 2019 | 地球科学2019，44，2： | 17 |
| 5 | Formation and evolution of the Archean continental crust of China:A review显示文摘The mainland of China is composed of the North China Craton,the South China Craton,the Tarim Craton and other young orogehie belts.Amongst the three cratons,the North China Craton has been studied most and noted for its widely-distributed Archean basement rocks.In this paper,we assess and compare the geology,rock types,formation age and geochemical composition features of the Archean basements of the three cratons.They have some common characteristics,including the fact that the crustal rocks prior to the Paleoarchean and the supracrustal rocks of the Neoarehean were preserved,and Tonalite-Trondhjemtite- Granodiorite (TTG)magmatism and tectono-magmatism occurred at about 2.7 Ga and about 2.5 Ga respectively.The Tarim Craton and the North China Craton show more similarities in their early Precambrian crustal evolution.Significant findings on the Archean basement of the North China Craton are coneluded to be:(1)the tectonic regime in the early stage (>3.1 Ga)is distinct from modem plate tectonics;(2)the continental crust accretion occurred mostly from the late Mesoarchean to the early Neoarehean period;(3)a huge linear tectonic belt already existed in the late Neoarchean period,suggesting the beginning of plate tectonics;and (4)the preliminary cratonization had already been completed by about 2.5 Ga. Hadean detrital zircons were found at a total of nine locations within China.Most of them show clear oscillatory zoning,sharing similar textures with magmatic zircons from interrnediate-felsic magmatic rocks. This indicates that a fair quantity of continental material had already developed on Earth at that time. | Yu-sheng Wan Shou-jie Liu Hang-qiang Xie Chun-yan Dong Yuan Li Wen-qian Bai Dun-yi Liu | 2018 | China Geology2018，1，1： | 12 |
| 6 | Zircon Geochronological Evidence for Participation of the North China Craton in the Protolith of Migmatite of the North Dabie Terrane显示文摘The plate affiliation of the North Dabie terrane(NDT) has been controversial. To address this fundamental question, an integrated study of internal structure, in-situ U-Pb dating and trace element analysis in zircons and field investigation for migmatite in the NDT was carried out, which reveals participation of crustal rocks of the North China craton(NCC) in the protolith in addition to the more common crustal rocks of the Yangtze craton(YC). The evidence of an NCC affinity for protolith of migmatite in the NDT is the ~2.5 Ga(2 486±14 and 2 406±26 Ma) magamtic age and ~1.8 Ga(1 717±79 Ma) metamorphic age in the relict zircon domains because these two age groups are characteristic for the evolution of the NCC. The evidence of a YC affinity for protolith of migmatite in the NDT is the more common 0.7–0.8 Ga(e.g., 787±12 Ma) magamtic zircon age. Mid-Neoproterozoic magmatic age(0.7–0.8 Ga) is a symbol of YC basement rocks. In view of the widely exposed YC crustal components in the NDT, we suggest that the protolith of the NDT is mainly crustal rocks from the YC with minor crustal components from the NCC. The zircon rim domains and new growth grains from all the migmatite samples are characterized by anatectic zircons and have a widely concordant ages ranging from 112.2±2.8 to 159.6±4.3 Ma with several peak values, suggesting a long lasting multistage anatexis. In conclusion, the NDT has a mixed protolith origin of both the YC and the NCC crustal rocks were strongly remoulded by anatexis during orogenic collapse. | Haijin Xu Junfeng Zhang | 2018 | Journal of Earth Science2018，29，1： | 9 |
| 7 | Hydrocarbon Geological Conditions and Exploration Potential of Mesozoic–Paleozoic Marine Strata in the South Yellow Sea Basin显示文摘No substantial breakthroughs have been made in hydrocarbon exploration of the South Yellow Sea Basin.It is believed that the Mesozoic-Paleozoic marine sedimentary formation in the South Yellow Sea Basin is similar to that in the Sichuan Basin.Therefore,outcrop,drilling,and seismic data were determined and compared with the research results on petroleum geological conditions in the Yangtze land area,and the hydrocarbon geological conditions were analyzed comprehensively from multiple aspects,such as basin evolution and main source rocks,reservoir characteristics,preservation conditions,and structural traps.The results show that two main stages in the South Yellow Sea Basin(the stable evolution stage of the Mesozoic-Paleozoic marine basin and the Mesozoic-Cenozoic tectonic reformation and basin formation stage)were important for the development and evolution of four sets of main source rocks.Reservoirs dominated by carbonate rocks,three sets of capping beds with good sealing capability,relatively weak magmatic activity,and multiple types of structural traps jointly constituted relatively good hydrocarbon-reservoir-forming conditions.There were four sets of main source-reservoir-cap assemblages and three possible hydrocarbon reservoir types(primary residual-type hydrocarbon reservoir,shallow reformed-type hydrocarbon reservoir,and composite-type hydrocarbon reservoir)developed in the marine strata.It is concluded that the marine strata in the South Yellow Sea Basin have relatively good hydrocarbon potential.The Laoshan Uplift is characterized by stable structure,complete preserved source reservoir cap assemblage,and large structural traps,and thus it is the preferred prospect zone for marine Paleozoic hydrocarbon exploration in this area. | YUAN Yong CHEN Jianwen LIANG Jie XU Ming LEI Baohua ZHANG Yuxi CHENG Qingsong WANG Jianqiang | 2019 | Journal of Ocean University of China2019，18，6： | 7 |
| 8 | 扬子北缘晚古元古代A型花岗质岩: Columbia超大陆裂解的证据显示文摘为约束扬子陆块晚古元古代构造演化历史,以华山观岩体的钾长花岗岩和二长花岗岩为研究对象,开展地球化学、年代学、全岩Nd同位素及锆石Hf同位素分析。锆石U-Pb定年结果显示钾长花岗岩和二长花岗岩的结晶年龄分别为1860±12 Ma(MSWD=0.69)和1832±14 Ma(MSWD=0.48)。两类岩石都显示铝质A型花岗岩的地球化学特征,一致的ε_(Hf)(t)值(-10.9~-13.8)及其二阶段模式年龄(2962~3183 Ma),揭示其由同一套太古宙的地壳部分熔融形成。综合已有ε_(Hf)(t)值资料,表明扬子陆块广泛存在两套太古宙长英质地壳(3.0~3.5 Ga; 3.5~3.9 Ga),为华山观两类花岗岩的岩浆形成提供了物源。华山观岩体两类花岗岩的锆石饱和温度揭示源岩位于较深的地壳,且二长花岗岩的形成有更多热源的参与。结合扬子陆块同期(~1.85Ga)A型花岗岩的地球化学数据,认为华山观钾长花岗岩具有后碰撞A_2型花岗岩的特征,形成于后碰撞伸展环境,而华山观二长花岗岩具有A_1型花岗岩的地球化学特征,暗示造山后伸展到陆内裂谷过渡的构造背景,可能与Columbia超大陆裂解有关。 | 黄明达 崔晓庄 程爱国 任光明 何虎庄 陈风霖 张恒利 张建强 任飞 | 2019 | 地质学报2019，93，3： | 7 |
| 9 | 扬子克拉通北缘“神农架群底界”的再厘定及其地层学意义显示文摘神农架群的底界问题一直以来悬而未决。神农架群底界能否获取,已成为神农架群能否完美成为待建系候选层型的关键。距神农架东南几十公里的黄陵穹隆东北部地区自下而上发育中-新元古代西汊河组、吴家台组、浇园山组、南沱组和陡山沱组等地层,且胡正祥等(2012)认为该地吴家台组为神农架群中下部地层,那么该地是否存在神农架群的底界自然就引起大家的极大关注。本文基于该地浇园山剖面西汊河组石英片岩样品(0529-1),吴家台组底部砾岩(0228-4)和砂岩(0228-5)3件样品,应用LA-ICP-MS方法进行了碎屑锆石年龄的测试分析,同时结合地层单元间接触关系和岩石学与沉积学特征等标志,最终约束吴家台组形成时代。结果表明,崆岭北部樟村坪以北浇园山剖面西汊河组与上覆吴家台组呈不整合接触;西汊河组碎屑锆石年龄谱仅显示太古宙和2.0Ga两个明显的峰值;但吴家台组碎屑锆石年龄谱不仅包含了与西汉河组相同的太古宙和2.0Ga两个年龄峰值,而且还含有0.8Ga的弱峰值,由此断定西汊河组和吴家台组形成时限是完全不同的。前者应年轻于2.0Ga,但由于其为角闪岩相变质岩,又不同于扬子克拉通最终(1.8Ga)固结前的变质结晶基底岩石组合,因此推测西汊河组大致为中元古代,同理,吴家台组应形成于0.8Ga以后,结合吴家台组之上具有典型的南沱组冰碛杂砾岩,因此其时代应界于青白口纪晚期-南华纪早期之间,进一步结合各岩组砾岩中砾石组分的证据认为,吴家台组应相当于区域上莲沱组。同时研究表明,西汊河组和吴家台组物源主要来自黄陵穹隆核部中太古代TTG片麻岩和新太古代的花岗质片麻岩,古元古代碎屑锆石主要来源于崆岭杂岩中部的火山-岩浆岩以及黄陵穹隆南翼的新元古代岩浆岩。 | 旷红伟 耿元生 柳永清 王玉冲 夏晓旭 彭楠 范正秀 陈骁帅 白华青 | 2019 | 地质学报2019，93，1： | 5 |
| 10 | Metamorphic petrology and geology in China:A review显示文摘The development of metamorphic petrology to metamorphic geology in China has a long history.Ancient basement metamorphic rocks are distributed primarily in the North China Craton,the Yangtze Block and Tarim Craton.They are mainly made up of plutonic gneiss and metamorphosed supercrust rock,transformed to granulite facies through Archean Paleoproterozoic.Many of the Paleoproterozoic metamorphic rocks have undergone high-pressure granulite facies metamorphism with a clockwise metamorphic evolution path.The ultrahigh temperature (UHT)granulites from the Late Paleoproterozoic are found in North China Craton.Many high-precision chronological data have allowed preliminary construction of the formation and evolutionary framework of different metamorphic basements.Primarily there are low-temperature and high-pressure blue schist,high-temperature and high-pressure granulite and ultrahigh-pressure (UHP)eclogite facies metamorphic rocks in the Phanerozoic orogenic belt.The discovery of eclogite in the Sulu orogen and a large quantity of coesite in its country rocks show that there was a deep subduction of voluminous continental materials during the collision process between the Yangtze block and the North China Craton in the Early Mesozoic phase.From the studies of,for instance,organic matter vitrinite reflectance,illite crystallinity,illite (muscovite)polytype and illite (muscovite)b dimension,the Late Paleozoic strata in the eastern region of Inner Mongolia and the north-central region of NE China have only experienced diagenesis to an extremely low-grade metamorphism.The discovery of impact-metamorphosed rocks in Xiuyan area of Liaoning province has enriched the type and category of metamorphic rocks in China.The phase equilibrium method has been widely used in the study of metamorphism of middle and high-grade metamorphic rocks.On the basis of existing geologic surveys and monographic study results, different scholars have respectively compiled 1:1500000 Metamorphic Geological Map and Specifications of Qinghai Tibet Plateau and its Adjacent Areas,1:2500000 Metamorphic Tectonic Map of China, and the 1:5000000 Metamorphic Geological Map and Specifications of China,among others repectively, which have systematically summarized the research results of metamorphic petrology and metamorphic geology in China. | Yuan-sheng Geng Qi-han Shen Hui-xia Song | 2018 | China Geology2018，1，1： | 4 |
| 11 | Zircon U-Pb Ages and Hf Isotopes of Neoproterozoic Meta-Igneous Rocks in the Liansandao Area,Northern Sulu Orogen,Eastern China,and the Tectonic Implications显示文摘The Sulu Orogen preserves the Neoproterozoic tectonic-magmatic events,corresponding to the breaking up of the Rodinia supercontinent.The ages and petrogenesis of meta-igneous rocks in the Liansandao area in the northern Sulu Orogen are not well-constrained.This study reports zircon U-Pb ages and Hf isotopes of these rocks from the Liansandao area.Three meta-igneous rock samples give similar weighted mean 206 Pb/238 U ages of 744±11,767±12,and 762±15 Ma,respectively,indicating the Neoproterozoic crystallization ages.These rocks formed coevally with the Wulian and Yangkou intrusions that located along the Yantai-Qingdao-Wulian fault zone.The Neoproterozoic ages indicate that the meta-igneous rocks from the Liansandao area have affinity to the Yangtze Block.The three samples haveεHf(t)values of-7.2–-10.5,-6.0–-17.5,and-6.8–-12.0,respectively.These negativeεHf(t)values indicate a primarily crustal source.However,the widely variousεHf(t)values that are higher than the continental crust,suggesting magma mixing between mantle-derived materials and the continental crust or source heterogeneity.Combined with the Hf model ages and geochemical characteristics,the monzodiorite(sample LSD-2)is most likely to be mantle-derived magma then interacted with ancient continental crust,and the granitic protolith(samples LSD-1 and LSD-3)in the Liansandao area might derive from the re-melting of a Paleoproterozoic continental crust at^750 Ma,resulting from the upwelling and underplating of mantle-derived magma formed in an extensional setting due to the break-up of the Rodinia supercontinent. | Zhaojun Song Huimin Liu Fanxue Meng Xingyu Yuan Qiao Feng Dingwu Zhou Juan Ramon Vidal Romani Hongbo Yan | 2019 | Journal of Earth Science2019，30，6： | 4 |
| 12 | 黔西赫章2.5 Ga石英二长闪长岩的发现及其地质意义显示文摘黔西位于扬子板块西南缘,有关扬子板块内约2.5 Ga的岩浆事件记录极少。最近,对黔西赫章发现的石英二长闪长岩的研究表明,其成岩年龄为(2542±9)Ma,为该区首次发现的新太古代晚期岩石。该岩石主要由斜长石、碱性长石、石英、角闪石、黑云母等矿物组成,具有较高的SiO2(59.2%~60.6%)、Na2O(4.70%~4.85%)质量分数和Na2O/K2O(3.02%~3.19%)比值,以及较低的Al2O3(17.0%~17.7%)、MgO(2.42%~2.61%)质量分数。样品稀土元素总质量分数为120×10^-6~221×10^-6,(La/Yb)N=8.32~17.98,轻、重稀土元素分异不明显,表现为弱的右倾稀土元素配分模式,并具有弱的Eu负异常。在微量元素蛛网图上,样品富集大离子亲石元素(Ba、Sr)、亏损高场强元素(Nb、Ta、Ti),具有弱负到正的εHf(t)值(-0.51^+6.93)和正的εNd(t)值(+0.22^+0.88),与太古宙低铝型高重稀土元素TTG的地球化学性质基本一致。综合研究显示,该岩石可能是在角闪岩相下,下地壳基性岩部分熔融形成的,源区残留相主要为金红石以及斜长石。黔西约2.5 Ga岩石的发现证实了扬子板块西南缘具有新太古代基底的存在,这为扬子周缘新太古代岩浆成因的碎屑锆石研究提供了依据,为扬子板块新太古代地壳演化提供了新的信息。 | 何良伦 刘雨 杨坤光 蔡京辰 王军 徐扬 | 2020 | 地质科技通报2020，39，6： | 3 |
| 13 | Geochronological and Geochemical Constraints on the Petrogenesis of Early Paleoproterozoic(2.40–2.32 Ga) Nb-Enriched Mafic Rocks in Southwestern Yangtze Block and Its Tectonic Implications显示文摘Recent geological survey has identified the Early Paleoproterozoic meta-mafic intrusions in the southwestern Yangtze Block.We present geochronological,whole-rock geochemical and Nd isotopic data for these meta-mafic rocks to better address the tectonic evolution of the Yangtze Block during the Early Paleoproterozoic Period.Geochronological data show that the meta-mafic rocks have zircon ages of 2 395-2 316 Ma.They have high TiO_2 contents of 1.40 wt.%-3.66 wt.% and Nb concentrations of 13.7 ppm-45.5 ppm,thus aregrouped as Nb-enriched mafic rocks.These mafic rocks are characterized by tholeiitic compositions with enrichment of LREEs and LILEs,and can be divided into two groups.Group 1 samples display E-MORB-like geochemical characteristics.Group 2 samples have positive ENd(t) values of 4.0-5.0.Geochemical data indicate that all meta-mafic rocks were likely derived from a depleted asthenospheric mantle.REE modeling indicates lower degree of partial melting for Group 2 samples(3%-10%) relative to Group 1 samples(15%-20%).Taking into account contemporaneous post-collisional granitoids in southwestern Yangtze Block,we propose that these meta-mafic rocks were formed in a post-collisional extension setting.These meta-mafic rocks can be compared with those in Africa,South America and Europe,and might be linked with the Arrowsmith orogenic belt. | Guichun Liu Xin Qian Jing Li Jian-Wei Zi Tianyu Zhao Qinglai Feng Guangyan Chen Shaobin Hu | 2020 | Journal of Earth Science2020，31，1： | 3 |
| 14 | Nature and Evolution of Pre-Neoproterozoic Continental Crust in South China: A Review and Tectonic Implications显示文摘South China as an amalgamation of the Yangtze and Cathaysia blocks is composed of Archean to Mesoproterozoic basement overlain by Neoproterozoic and younger cover.Both the constituent Yangtze and Cathaysia blocks contain well-preserved Neoproterozoic rocks that have been extensively studied in terms of the age and tectonic nature,but less is known about their earlier crustal history due to the incomplete rock record.Recent efforts in investigating the yet survived crustal nature based on isotopic and elemental signatures preserved in igneous and sedimentary rocks have steadily improved our knowledge about the pre-Neoproterozoic continental crustal evolution in South China.In this paper,we summarize the up-to-date pre-Neoproterozoic records,including petrological,geochronological,geochemical and geophysical data,across South China,and discuss its spatiotemporal patterns of the pre-Neoproterozoic crust and the relevant tectonic events.While the xenocrystic/inherited and detrital zircon records suggest widespread Archean(mainly ca.2.5 Ga)crustal components within both the Yangtze and Cathaysia blocks,exposed Archean rocks are only limited to isolated crustal provinces in the Yangtze Block.These Archean rocks are dominated by TTGs(tonalite-trondhjemitegranodiorite)with varied ages(3.3-2.5 Ga)and zircon Hf isotopes,indicating a compositionally heterogeneous nature of the Archean Yangtze Block and,by inference,the development of multiple ancient terranes.The early Paleoproterozoic(2.4-2.2 Ga)tectonomagmatic events characterize the western Yangtze Block and are supportive of an east-west subdivision of the Yangtze basement,whereas the late Paleoproterozoic(2.1-1.7 Ga)orogeneses may have affected a larger area covering both the western and eastern parts of the Yangtze Block,and also the Cathaysia Block.The eastern Yangtze Block with generally northeastward-younging late Paleoproterozoic magmatism and metamorphism likely experienced a prolonged 2.05-1.75 Ga orogenic process welding the various Archean proto-continents,consistent with the documentation of a buried late Paleoproterozoic orogenic belt imaged by deep seismic profiling from its central part and of a slightly older ophiolitic mélange in the northern part.The Cathaysia Block was probably involved in a short-lived 1.9-1.8 Ga orogenic event.The two orogeneses overlapped in time and may have contributed to the cratonization of a possible unified South China,and are referred to be linked with the assembly of the Nuna Supercontinent.The subsequent late Paleoproterozoic to early Mesoproterozoic rift successions and intrusions(1.7-1.5 Ga)in the southwestern Yangtze Block,and the ca.1.43 Ga rifting in Hainan Island of the Cathaysia Block could be responses to the Nuna break-up.Late Mesoproterozoic(1.2-1.0 Ga)magmatism of varied age and nature in different localities of the Yangtze Block is reflective of a complex tectonic process in the context of the assembly of the Rodinia Supercontinent.Similar-aged metamorphism(1.3-1.0 Ga)is recorded in Hainan Island,reflecting the Grenvillian continental collision during the Rodinia assembly,but further studies are necessar y to better constrain the late Mesoproterozoic tectonic framework of South China. | WANG Kai DONG Shuwen YAO Weihua ZHAO Tianyu | 2020 | Acta Geologica Sinica(English Edition)2020，94，6： | 2 |
| 15 | Ca. 1.7 Ga Magmatism on Southwestern Margin of the Yangtze Block: Response to the Breakup of Columbia显示文摘This paper presents some data of the Jiaopingdu gabbro and Caiyuanzi granite at the southwestern margin of the Yangtze Block,on the geochemical compositions,zircon LA-ICP-MS U-Pb ages and Hf isotopic data.The Jiaopingdu gabbro gives the age of 1721±5 Ma,the Caiyuanzi granite 1732±6 Ma and 1735±4 Ma,and the Wenjiacun porphyry granite 1713±4 Ma,suggesting nearly contemporaneous formation time of the gabbro and granite.The bimodal feature is demonstrated by the gabbro Si O2 content of 44.64-46.87 wt%and granite 73.81-77.03 wt%.In addition,the granite has high content of Si O2 and Na2 O+K2 O,low content of Al2 O3 and Ca O,enriched in REEs(except Eu)and Zr,Nb,Ga and Y,depleted in Sr,implying it belongs to A-type granite geochemistry and origin of within-plate environment.The zirconε(Hf)(t)of the granite and gabbro is at the range of 2-6,which is near the 2.0 Ga evolution line of the crust,implying the parent magma of the gabbro being derived from the depleted mantle and a small amount of crustal material,and the parent magma of the granite from partial melting of the juvenile crust and some ancient crustal material at the same time.Compared with 1.8-1.7 Ga magmatism during breakup of other cratons in the world,we can deduce that the Columbia has initially broken since ca.1.8 Ga,and some continental marginal or intra-continental rifts occurred at ca.1.73 Ga. | GENG Yuansheng DU Lilin KUANG Hongwei LIU Yongqing | 2020 | Acta Geologica Sinica(English Edition)2020，94，6： | 1 |
| 16 | 扬子地块中太古宙地壳增生:来自黄陵背斜南部地区花岗闪长质片麻岩的证据显示文摘扬子地块黄陵背斜南部出露的花岗闪长质片麻岩是太古宙TTG片麻岩的重要组成单元,具有高Al2O3、Na2O、Sr以及低Rb、Nb等特征,属于高铝TTG系列,且具埃达克质岩石属性。结合片麻岩微量元素蛛网图显示的Nb、Ta和Hf等高场强元素富集以及Th、Pb和U等大离子亲石元素亏损的特征,本文认为该岩石形成于俯冲环境下玄武质洋壳的部分熔融作用。黄陵背斜北部出露的2.9~3.0 Ga TTG片麻岩和弧性质角闪岩,反映该时期是扬子地块陆壳生长的一次重要阶段,且以洋壳俯冲产生岛弧或安第斯型岩浆作用的陆壳水平增生为主,通过微陆块拼贴或规模较小的板块构造模式而形成。 | 王庆 蒋幸福 | 2023 | 现代地质2023，37，2： | 0 |
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