Geochemistry,geochronology and Hf isotope of granitoids in the Chinese Altai: Implications for Paleozoic tectonic evolution of the Central Asian Orogenic Belt     

Dengfeng He  Yunpeng Dong  Xueyi Xu  Junlu Chen  Xiaoming Liu  Wei Li  Xiangmin Li 《地学前缘(英文版)》2018,9(5):1399-1415

The Chinese Altai in northwestern Xinjiang has numerous outcrops of granitoids which provide critical information on accretionary orogenic processes and crustal growth of the Central Asian Orogenic Belt.Zircon U-Pb ages, Hf-isotopic compositions and whole-rock geochemistry of monzogranite and granodiorites in the Qinghe County are employed to elucidate Paleozoic tectonics of the Chinese Altai. Granodiorites have crystallization ages of 424.6 ± 3.1 Ma(MSWD = 0.23) and 404.0 ± 3.4 Ma(MSWD = 0.18);monzogranite was emplaced in the early Permian with a crystallization age of 293.7 ± 4.6 Ma(MSWD = 1.06). Both granodiorites and monzogranite are I-type granites with A/CNK ratios of 0.92 -0.97 and 1.03 -1.06, respectively. They also show similar geochemical features of high HREE and Y contents, low Sr contents and Sr/Y ratios, as well as enrichment of Cs, Rb, Th and U, and depletion of Nb, Ta, P and Ti.These geochemical features indicate that the monzogranite and granodiorites were formed in an arc setting related to subduction. The gneissic monzogranites display high SiO_2 and K_2 O contents, and belong to the high-K calc-alkaline series. In the chondrite normalized REE distribution pattern, the monzogranite samples exhibit enrichment of LREE with strong negative Eu anomalies(σE u =0.44 -0.53), zircon εHf(t) values from +7.24 to +12.63 and two-stage Hf model ages of 463 -740 Ma. This suggests that the monzogranite was generated from the mixing of pelitic and mantle material. The granodiorite samples are calc-alkaline granites with lower contents of Si O_2 and Na_2 O + K_2 O, higher contents of TiO_2, Fe_2O_3~t, MgO and CaO compared to the monzogranite samples. They also show enrichment of LREE and moderate negative Eu anomalies(σE u= 0.54 =0.81), as well as slightly higher differentiation of LREE than that of HREE. The425 Ma granodiorite has zircon εHf(t) values from -0.51 to +1.98 and two-stage Hf model ages of 1133 -1240 Ma, whereas the 404 Ma granodiorite displays those of +2.52 to +7.50 and 816 -1071 Ma.Geochemistry and zircon Hf isotopic compositions indicate that granodiorites were formed by partial melting of juvenile lower crust. Together with regional geology and previous data, the geochemical and geochronological data of the monzogranite and granodiorites from this study suggest long-lived subduction and accretion along the Altai Orogen during ca. 425 -294 Ma.  相似文献   

Geochronology and geochemistry of mafic dykes in the Helanshan complex: Implications for Mesozoic tectonics in the North China Craton     

《地学前缘(英文版)》2018,9(6):1711-1724

The Helanshan tectonic belt(HTB) is a major tectonic divide between the Alxa and Ordos blocks in the North China Craton. The geochronology and petrogenesis of the mafic dykes in the northern HTB are keys to understanding the tectonic evolution of this belt. The mafic dykes, intruded into the Neoarchean-Paleoproterozoic metamorphic basement, are mainly composed of diabase with a mineral assemblage of plagioclase(45%-60%), pyroxene(25%-35%), minor quartz and Fe-Ti oxides. The LA-ICPMS U-Pb analysis of zircon grains from representative dykes yield a weighted mean age of 206 ± 1.9 Ma, which represents the crystallization age of the dyke. The diabases show high contents of Fe_2 O_3~T(11.88-17.55 wt.%), low contents of SiO_2(45.65-50.95 wt.%) and MgO(3.31-5.50 wt.%) with low Mg#(=100×MgO/(MgO + FeO) atomic ration) of 33-44. They are characterized by enrichment of light rare earth elements(LREEs) and large ion lithophile elements(LILEs)(e.g., Rb, Ba and Pb), and slight depletion of high field strength elements(HFSEs). These features suggest that the magma has undergone extensive fractionation of olivine and pyroxene but only minor crustal contamination during its evolution. Their high Sm contents and La/Sm ratios, and low Sm/Yb ratios indicate that magma from which the dykes formed was derived from low degree(about 5%) partial melting of an enriched garnet + spinel lherzolite mantle source. Together with regional geology, these geochemical and geochronological data suggest that the mafic dykes in the HTB were formed in an intracontinental extensional setting during the late Triassic.  相似文献   

中亚造山带北山下—中二叠统物源分析及古地理意义     

张东东  王建强  牛亚卓  张宇轩  史冀忠  刘兆龙 《地质学报》2023,97(2):307-324

甘蒙北山地区位于中亚造山带中段南端,该区广泛出露的海相二叠系是中亚造山带最年轻的海相沉积之一,是解析古亚洲洋晚期演化的理想载体。然而,北山地区的物源学数据分布不均衡、缺少统计对比,直接限制了学界对古亚洲洋古地理结构的探讨。本文在贯穿北山地区中部至南部的8条剖面中获得了681个碎屑锆石U-Pb年龄和192个Hf同位素数据;在等时地层对比的基础上,统计计算了北山地区已发表的下—中二叠统碎屑锆石数据,重建了区域古地理面貌。早—中二叠世,红石山洋向南俯冲至旱山地块之下,形成了黑鹰山弧和弧后裂谷盆地。该盆地北侧的物源分别来自于旱山地块的前寒武纪基底(926～775 Ma)和奥陶纪—志留纪岩体(485～421 Ma),而南侧的物源主要来自于马鬃山隆起。马鬃山隆起是早古生代红柳河—洗肠井洋闭合的产物,主要由奥陶纪—泥盆纪岩体(470～367 Ma)组成,包括早古生代马鬃山岛弧和双鹰山地块的大部分地区。北山南部发育柳园裂谷盆地,盆地南北两侧的碎屑物质分别主要来自于石炭纪—二叠纪火山岩(322～270 Ma)和马鬃山隆起的早古生代岩体,这两种碎屑物质在盆地中心交汇。本文古地理重建结果表明：红石山洋可代表...  相似文献   

http://www.sciencedirect.com/science/article/pii/S1674987114001091   总被引：2，自引：0，他引：2  

Jieyun Tang  Dengfa He  Di Li  Delong Ma 《地学前缘(英文版)》2015,6(2):227-246

The Wulungu Depression is the northernmost first-order tectonic unit in the Junggar Basin.It can be divided into three sub-units:the Hongyan step-fault zone,the Suosuoquan sag and the Wulungu south slope.The Cenozoic strata in the basin are intact and Mesozoic—Cenozoic deformation can be observed in the Wulungu step-fault zone,so this is an ideal place to study the Mesozoic—Cenozoic deformation.By integration of fault-related folding theories,regional geology and drilling data,the strata of the Cretaceous—Paleogene systems are divided into small layers which are selected as the subjects of this research.The combination of the developing unconformity with existing growth strata makes it conceivable that faults on the step-fault zone have experienced different degrees of reactivation of movement since the Cretaceous.Evolutionary analyses of the small layers using 2D-Move software showed certain differences in the reactivation of different segments of the Wulungu Depression such as the timing of reactivation of thrusting,for which the reactivity time of the eastern segment was late compared with those of the western and middle segments.In addition the resurrection strength was similarly slightly different,with the shortening rate being higher in the western segment than in the other segments.Moreover,the thrust fault mechanism is basement-involved combined with triangle shear fold,for which a forward evolution model was proposed.  相似文献   

The final collision of the CAOB: Constraint from the zircon U–Pb dating of the Linxi Formation, Inner Mongolia     

Jie Han  Jian-Bo Zhou  Bin Wang  Jia-Lin Cao 《地学前缘(英文版)》2015,6(2):211-225

The Linxi Formation occupies an extensive area in the eastern Inner Mongolia in the Central Asian Orogenic Belt(CAOB).The Linxi Formation is composed of slate,siltstone,sandstone and plant,lamellibranch microfossils in the associated strata.Major and trace element data(including REE) for sandstones from the formation indicate that these rocks have a greywacke protolith and have been deposited during a strong tectonic activity.LA-ICPMS U—Pb dating of detrital zircons yield ages of 1801 to 238 Ma for four samples from the Linxi Formation.425—585 Ma,together with the ~500 Ma age for the metamorphism event previously determined for Northeast China,indicates that their provenance is the metamorphic rocks of Pan-African age that have a tectonic affinity to NE China.A few older zircons with U-Pb ages at 1689-1801 Ma,1307-1414 Ma,593-978 Ma are also present,revealing the Neoproterozoic history of NE China.The youngest population shows a peak at ca.252 Ma,suggesting that the main deposition of the Linxi Formation was at late Permain.Moreover,the ca.250 Ma zircon grains of all four samples yield weighted mean ~(206)Pb/~(238)U ages of 250 ± 3 Ma,248 ± 3 Ma,249 ± 3 Ma,and 250 ± 2 Ma,respectively.These ages,together with the youngest zircon age in the sample ZJB-28(ca.238 Ma),suggest that the deposition of the Linxi Formation extended to the early Triassic.Combining with previous results,we suggest that the final collision of the Central Asian Orogenic Belt(CAOB) in the southern of Linxi Formation,which located in the Solonker-Xra Moron-Changchun suture,and the timing for final collision should be at early Triassic.  相似文献   

Geochronology and Tectonic Evolution of the West Section of the Jiangnan Orogenic Belt   总被引：1，自引：1，他引：0  

ZHANG Heng  LI Tingdong  XIE Ying  ZHANG Chuanheng  GAO Linzhi  GENG Shufang  CHEN Tingyu  YOU Guoqing 《《地质学报》英文版》2015,89(5):1497-1515

As an important part of South China Old Land, the Jiangnan Orogenic Belt plays a significant role in explaining the assembly and the evolution of the Upper Yangtze Block and Cathaysia, as well as the structure and growth mechanism of continental lithosphere in South China.The Lengjiaxi and the Banxi groups are the base strata of the west section of the Jiangnan Orogenic Belt.Thus, the research of geochronology and tectonic evolution of the Lengjiaxi and the Banxi groups is significant.The maximum sedimentary age of the Lengjiaxi Group is ca.862 Ma, and the minimum is ca.822 Ma.The Zhangjiawan Formation, which is situated in the upper part of the Banxi Group is ca.802 Ma.The Lengjiaxi Group and equivalent strata should thus belong to the Neoproterozoic in age.The Jiangnan Orogenic Belt consisting of the Lengjiaxi and the Banxi groups as important constituents is not a Greenville Orogen Belt(1.3 Ga–1.0 Ga).The Jiangnan Orogenic Belt is a recyclic orogenic belt, and the prototype basin is a foreland basin with materials derived from the southwest and the sediments belong to the active continental sedimentation.By combining large amounts of dating data of the Lengjiaxi and the Banxi groups as well as equivalent strata, the evolutionary model of the western section of the Jiangnan Orogenic Belt is established as follows: Before 862 Ma, the South China Ocean was subducted beneath the Upper Yangtze Block, while a continental island arc was formed on the side near the Upper Yangtze Block.The South China Ocean was not closed in this period.From 862 Ma to 822 Ma, the Upper Yangtze Block was collided with Cathaysia; and sediments began to be deposited in the foreland basin between the two blocks.The Lengjiaxi Group and equivalent strata were thus formed and the materials might be derived from the recyclic orogenic belt.From 822 Ma to 802 Ma, Cathaysia continued pushing to the Upper Yangtze Block, experienced the Jinning-Sibao Movement(Wuling Movement); as result, the folded basement of the Jiangnan Orogenic Belt was formed.After 802 Ma, Cathaysia and the Upper Yangtze Block were separated from each other, the Nanhua rift basin was formed and began to receive the sediments of the Banxi Group and equivalent strata.These large amounts of dating data and research results also indicate that before the collision of the Upper Yangtze Block with Cathaysia, materials of the continental crust became less and less from the southwest to the east in the Jiangnan Orogeneic Belt; only island arc and neomagmatic arc were developed in the eastern section.Ocean-continent subduction or continent-continent subduction took place in the western and southern sections, while intra-oceanic subduction occurred in the eastern section.Comprehensive analyses on U-Pb ages and Hf model ages of zircons, the main provenance of the Lengjiaxi Group is Cathaysia.  相似文献   

丝绸之路经济带的地理空间认知框架研究     

马照亭  李成名  印洁 《测绘科学》2015,(10):48-53

针对现有的丝绸之路经济带研究主要集中在人文角度的描述、统计和分析,缺少形象的空间思维手段和对经济带战略全局的整体把控的现状,该文在分析丝绸之路经济带地理特点的基础上,提出了丝绸之路经济带地理空间认知框架,认为丝绸之路经济带的地理空间认知是从概念空间、数据空间到信息空间、知识空间,最后形成智慧空间的认知深化过程,并重点研究了专家认知和用户认知两个关键环节。在此框架下,该文结合丝绸之路经济带的地理特点和测绘地理信息行业的技术现状从地理概念、地理数据、专家认知和用户认知四个方面分析了丝绸之路经济带的主要认知内容。研究表明,用户地理空间认知的深化程度依赖于前期的专家认知成果,专家在认知过程中必须时刻围绕用户的地理空间认知需求,专家认知和用户认知是地理空间认知有机统一的两个核心环节,不可割裂或偏废;直观的地理概念、准确的地理数据、丰富的专家经验和便捷的分析工具是科学认知丝绸之路经济带的技术保障,可以为区域经济合作战略的实施提供更多的地理智慧。  相似文献   

基于陆路交通的丝绸之路经济带可达性与城市空间联系   总被引：9，自引：1，他引：8  

曹小曙  李涛  杨文越  黄晓燕  殷江滨  刘永伟  梁斐雯  王武林  王妙妙 《地理科学进展》2015,34(6)

对丝绸之路经济带交通网络及城市空间联系进行分析是实施丝绸之路经济带战略和推进沿线区域合作共赢的基础工作。本文基于GIS空间分析技术,研究了丝绸之路经济带栅格可达性空间格局,并依托陆路交通网络进行了城市空间联系状态模拟。结果显示:丝绸之路经济带内城市可达性空间分布呈现出集聚分布的特点,具有明显的"走廊"空间特征。城市节点平均可达性时间为16.25 h,可达性在2 h以内的区域仅占全区总面积的10.60%,可达性最差的区域大都为荒漠地区,最差可达性高达171 h;西安作为门户城市,承担了中国西北五省与丝绸之路经济带有关国家、地区和城市之间的联系。中亚国家内部及其与外部国家城市之间的空间联系较为薄弱;丝绸之路经济带正在发育形成4条轴线,在未来丝绸之路经济带战略推进过程中,应实施"点—轴"带动,协同推进重点发展走廊和中心城市培育工作。  相似文献   

“一带一路”战略的科学内涵与科学问题   总被引：51，自引：12，他引：39  

刘卫东 《地理科学进展》2015,34(5)

"一带一路"指"丝绸之路经济带"和"21世纪海上丝绸之路",是中国为推动经济全球化深入发展而提出的国际区域经济合作新模式。其核心目标是促进经济要素有序自由流动、资源高效配置和市场深度融合,推动开展更大范围、更高水平、更深层次的区域合作,共同打造开放、包容、均衡、普惠的区域经济合作架构。"一带一路"框架包含了与以往经济全球化完全不同的理念,即"和平合作、开放包容、互学互鉴、互利共赢",这正是丝绸之路文化内涵的体现。本文分析了"一带一路"战略与经济全球化及世界格局变化的关系;剖析了其空间内涵,认为"一带一路"具有多重空间内涵和跨尺度特征,是统筹中国全面对外开放的国家战略。最后,提出了推进"一带一路"建设为地理学提出的几个重要议题,包括地缘政治、国别地理、对外直接外资理论、交通运输优化组织等。  相似文献   

中国对“一带一路”沿线直接投资空间格局   总被引：8，自引：3，他引：5  

郑蕾  刘志高 《地理科学进展》2015,34(5)

2015年3月28日,中国政府正式发布了《推动共建丝绸之路经济带和21世纪海上丝绸之路的愿景与行动》。如何通过对"一带一路"国家和地区直接投资,提升主要产业的国际竞争力,促进中国产业转型升级,实现与沿线国家共同繁荣,已成为当前迫切需要解决的重大课题。现有对外投资理论多基于发达国家的经验,不完全适用于中国;目前的研究侧重从自然资源、市场要素等方面分析中国企业的海外投资动因及影响机制,缺少面向国家战略需求的宏观投资格局研究。本文通过集成统计数据、实地调研和高层访谈等,在回顾国内外对外直接投资研究基础上,提出中国对"一带一路"沿线直接投资空间战略的分析框架,进一步分析中国对沿线国家和地区直接投资的空间分布和产业选择;尔后,剖析投资面临的困境和挑战,并提出中国对沿线地区的空间差异化投资引导战略。  相似文献