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An Overview on the Composition and Age of Upper Crust of Proto-Tethyan Lajishan Intra-oceanic Arc,NE Tibet Plateau

Acta Geologica Sinica(English Edition) 2024年第2期98卷 285-302页

作者： FU Changlei HE xiaohu YAN Zhen Jonathan CAITCHISON xiao wenjiao WANG Bingzhang LI Wufu LI Yusen SinoProbe Laboratory Institute of GeologyChinese Academy of Geological SciencesBeijing 100037China Key Laboratory of the Northern Qinghai–Tibet Plateau Geological Processes and Mineral Resources Qinghai Geological Survey InstituteXining 810012China Department of Geology School of Earth SciencesYunnan UniversityKunming 650091China School of Earth and Environmental Sciences University of QueenslandBrisbane 4072Australia Xinjiang Institute of Ecology and Geography Chinese Academy of SciencesUrumqi 830011China State Key Laboratory of Lithospheric Evolution Institute of Geology and GeophysicsChinese Academy of SciencesBeijing 100029China School of Earth Science and Resources China University of GeosciencesBeijing 100083China

Identification and anatomy of oceanic arcs within ancient orogenic belt are significant for better understanding the tectonic framework and closure process of paleo-ocean *** article summarizes the geological,geochemical,and geochronological characteristics of upper crust of Proto-Tethyan Lajishan intra-oceanic arc and provides new data to constrain the subduction evolution of the South Qilian *** intra-oceanic arc volcanic rocks,including intermediate-mafic lava,breccia,tuff,and minor felsic rocks,are distributed along southern part of the Lajishan ophiolite *** and isotopic compositions indicate that the intermediate-mafic lava were originated from depleted mantle contaminated by sediment melts or hydrous fluids,whereas the felsic rocks were likely generated by partial melting of juvenile mafic crust in intra-oceanic arc *** from felsic rocks yield consistent and concordant ages ranging from 506 to 523 Ma,suggesting these volcanic rocks represent the relicts of upper crust of the Cambrian intra-oceanic *** with the Cambrian forearc ophiolite and accretionary complex,we suggest that the Cambrian intra-oceanic arc in the Lajishan ophiolite belt is belonging to the intra-oceanic arc system which was generated by south-directed subduction in the South Qilian Ocean at a relatively short interval between approximately 530 and 480 Ma.

关键词： volcanic rocks intra-oceanic arc U-Pb age Lajishan ophiolite belt South Qilian Ocean Proto-Tethyan realm

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Hot subduction in the southern Paleo-Asian Ocean:Insights from clinopyroxene chemistry and Sr-Nd-Hf-Pb isotopes of Carboniferous volcanics in West Junggar

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Geoscience Frontiers 2024年第1期15卷 155-174页

作者： Yao xiao Xijun Liu wenjiao xiao xiao-Han Gong Hao Wu Yujia Song Zhiguo Zhang Pengde Liu Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration College of Earth SciencesGuilin University of TechnologyGuilin 541004China Collaborative Innovation Center for Exploration of Nonferrous Metal Deposits and Efficient Utilization of Resource Guilin University of Technology Guilin 541004China National Key Laboratory of Ecological Security and Resource Utilization in Arid Areas Xinjiang Institute of Ecology and GeographyChinese Academy of SciencesUrumqi 830011China School of Earth Sciences and Resources China University of GeosciencesBeijing 100083China College of Civil Engineering Hexi UniversityZhangye 734000China

The chemical evolution and pressure-temperature conditions of subduction zone magmatism along ancient suture zones in orogenic belts can provide important information regarding plate convergence processes in *** magmatism in West Junggar is key to understanding the tectonothermal and subduction history of the Junggar Ocean,which was a branch of the Paleo-Asian Ocean,as well as the accretionary processes in the southwestern Central Asian Orogenic Belt(CAOB).We undertook a geochronological,mineralogical,geochemical,and Sr-Nd-Hf-Pb isotopic study of volcanic rocks from the Baikouquan area of West *** used these data to determine the petrogenesis,mantle source,and pressure-temperature conditions of these magmas,and further constrain the subduction and tectonic history of the Junggar *** studied volcanic rocks yielded zircon U-Pb ages of 342-337 Ma and are characterized by enrichments of large-ion lithophile elements(LILEs),and depletions in high-field-strength elements(HFSEs),indicative of an island arc *** volcanic rocks have positiveƐNd(t)(5.83-7.04)andƐHf(t)(13.47-15.74)values,87Sr/86Sr(t)ratios of 0.704023-0.705658,and radiogenic 207Pb/204Pb(t)and 208Pb/204Pb(t)ratios at a given 206Pb/204Pb(t)ratio,indicative of a depleted mantle source contaminated by subduction-related *** modeling calculations indicate that≤1%of a subduction component comprising fluid and sediment melt could have generated the source of the parental melts of the Baikouquan volcanic *** phenocrysts in the volcanic rocks are classified as high-and low-Ti clinopyroxene,and pressure-temperature calculations suggest the host rocks formed at high temperatures(~1300℃)and shallow to moderate depths(<2 GPa).The magma was probably generated by hot and hydrous melting in a mantle wedge in response to subduction of young,hot oceanic *** present results,combined with published data,suggest that the Baikouquan volcanic r

关键词： Hot subduction Sr-Nd-Hf-Pb isotopes Clinopyroxene chemistry West Junggar Central Asian Orogenic Belt

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弧前盆地的沉积和构造特征

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地球科学 2024年第7期49卷 2539-2551页

作者：谭毅滢肖文交宋东方中国科学院地质与地球物理研究所岩石圈演化国家重点实验室北京100029 中国科学院大学地球与行星科学学院北京100049 中国科学院新疆生态与地理研究所新疆矿产资源研究中心新疆乌鲁木齐830011

汇聚板块边缘的沉积盆地是造山带研究的重要对象,其中弧前盆地位于弧前区域靠近岛弧一侧,更易在造山过程中被保留下来,保存造山带结构和演化的信息.本文以研究较为充分的新生代弧前盆地为例,详述了弧前盆地的大地构造位置、形成机制、... 详细信息

汇聚板块边缘的沉积盆地是造山带研究的重要对象,其中弧前盆地位于弧前区域靠近岛弧一侧,更易在造山过程中被保留下来,保存造山带结构和演化的信息.本文以研究较为充分的新生代弧前盆地为例,详述了弧前盆地的大地构造位置、形成机制、沉积、物源和构造特征,为古老造山带研究中弧前盆地的识别提供依据.弧前盆地位于岛弧和海沟外坡之间,可以形成于伸展或挤压环境中,前者由伸展正断层形成地堑式盆地,后者由增生楔逆冲构造形成挤压盆地.弧前盆地发育多种类型的沉积,其中洋内弧以半深海-深海相沉积为主,大陆弧则涵盖陆相-海陆交互相-海相等多种沉积相,总体呈现粒度从边缘向中心变细、从下往上变粗的沉积序列.陆源碎屑主要来源于相邻岛弧和增生楔,通过河流、海底峡谷和海底滑坡等方式进入盆地.洋中脊、海山、洋底高原和大洋破碎带俯冲都能不同程度地影响俯冲带结构,造成弧前盆地的反转、抬升剥蚀、沉积间断、物源区变化以及沉积环境的改变.弧前盆地的沉积过程复杂,难以用单一模型简单概括,在应用弧前盆地对造山带进行分析时,应结合多学科资料对地质记录进行综合分析.

关键词：俯冲带弧前盆地沉积特征构造特征造山带构造地质学

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New paleomagnetic data confirm a dual-collision process in the Himalayas

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National Science Review 2015年第4期2卷 395-396页

作者： wenjiao xiao Institute of Geology and Geophysics Chinese Academy of Sciences

The India–Asia collision and continual plate convergence have created the Himalayan–Tibetan Orogen,which is the youngest and most spectacular continent–continent collision belt on Earth,and thus an ideal place for the study of continent–continent collisions[1,2].Although a large number of geological and geophysical investigations

关键词： data Asia Figure

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Plate divergent-convergent coupling system and dynamic mechanism of continental orogenic belts

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Science China Earth Sciences 2023年第8期66卷 1909-1912页

作者： wenjiao xiao Xinjiang Institute of Ecology and Geography Chinese Academy of SciencesUrumqi 830011China

Since the establishment of the theory of plate tectonics in the1960s and 1970s,the comprehension of global tectonics has shifted from “fixism” to “mobilism”,which is hailed as a revolution in earth science(Vine,1966;Dewey and Bird,1970).According to the basic theoretical framework of plate tectonics,the Earth’s surface can be divided into a number of rigid lithospheric plates,which move relative to one another on the ductile asthenosphere,giving rise to deformation。

关键词： tectonics continental orogenic

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地震反射剖面揭示阿尔泰山陆内逆冲造山机制

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Science Bulletin 2024年第11期69卷 1757-1766页

作者：张蕾赵连锋赵亮谢小碧田小波肖文交姚振兴 Key Laboratory of Earth and Planetary Physics Institute of Geology and GeophysicsChinese Academy of SciencesBeijing 100029China State Key Laboratory of Lithospheric Evolution Institute of Geology and GeophysicsChinese Academy of SciencesBeijing 100029China Institute of Geophysics and Planetary Physics University of California at Santa CruzCA 95064USA Xinjiang Institute of Ecology and Geography Chinese Academy of SciencesUrumqi 830011China

The Altai orogen is a typical intracontinental orogen in Central Asia that experienced far-field deformation associated with Indian-Eurasian plate convergence. This region is characterized by uplift comparable to that of the Tianshan Mountains but has a distinct strain rate. Half of the Indo-Asia strain is accommodated by the Tianshan Mountains, whereas the Altai Mountains accommodates only 10%. To elucidate how the Altai Mountains produced such a large amount of uplift with only one-fifth of the strain rate of the Tianshan Mountains, we constructed a detailed crustal image of the Altai Mountains based on a new 166.8-km deep seismic reflection profile. The prestack migration images reveal an antiform within the Erqis crust, an ~10 km Moho offset between the Altai arc and the East Junggar area, and a major south-dipping(30° dip) thrust in the lower crust beneath the Altai Mountains, which is connected to the Moho offset. The south-dipping thrust not only records the southward subduction of the Ob-Zaisan Ocean in the Paleozoic but also controlled the Altai deformation pattern in the Cenozoic with the Erqis antiform. The Erqis antiform prevented the extension of deformation to the Junggar crust. The southdipping thrust in the lower crust of the Altai area caused extrusion of the lower crust, generating uplift at the surface, thickening of the crust, and steep(~10 km) Moho deepening in the Altai Mountains. This process significantly widened the deformation zone of the Altai Mountains. These findings provide a new geodynamic model for describing how inherited crustal structure controls intraplate deformation without strong horizontal stress.

关键词： Altai mountains Deep seismic reflection profile Subduction-accretion process Intraplate deformation pattern

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Origin of the DUPAL anomaly in the Tethyan mantle domain and its geodynamic significance

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Science China Earth Sciences 2023年第12期66卷 2712-2727页

作者： Xijun LIU Jifeng XU wenjiao xiao Pengde LIU Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration&Collaborative Innovation Center for Exploration of Nonferrous Metal Deposits and Efficient Utilization of Resources in Guangxi College of Earth SciencesGuilin University of TechnologyGuilin 541004China School of Earth Sciences and Resources China University of GeosciencesBejing 100083China National Key Laboratory of Arid Area Ecological Security and Sustainable Development State Key Laboratory of Desert and Oasis Ecology Xinjiang Institute of Ecology and GeographyChinese Academy of SciencesUrumqi 83001lChina

Mantle heterogeneity has revealed systematic differences in Pb isotopic compositions between the Indian OceanSouth Atlantic mantle in the Southern Hemisphere and the Pacific Ocean-North Atlantic mantle in the Northern *** large-scale difference in mantle isotopes in the Southern Hemisphere is known as the DUPAL anomaly,but its origin remains *** on a systematic review of the Nd-Pb isotopic evolution of the Tethyan mantle domain,this study identified the long-term presence of the DUPAL anomaly in this domain since the early Paleozoic,characterized by long-term and high mantle thorium/uranium(Th/U)*** comparing the Nd-Pb isotopic compositions of the Tethyan mantle domain with the Panthalassic-Pacific mantle domain(the Paleo-Asian,Paleo-Pacific,and modern Pacific oceans),it is shown that the mantle initially had low Th/U features due to early Earth crust-mantle differentiation,with the crust having high Th/U *** such,the mantle initially had uniformly low Th/U ratios that were inherited throughout the Panthalassic-Pacific mantle ***,the plate tectonics and continental collisions in the Tethyan domain affected its characteristics,leading to the long-term and large-scale DUPAL *** the opening of and subduction in the Tethys Ocean,Gondwanaland fragmentation and frequent continent-continent collisions led to long-term and extensive crust-mantle interactions and the continuous input of highTh/U mantle sources,which thus modified the *** process formed not only the unique DUPAL anomaly in the Tethyan mantle domain,but also the Tethyan tectonic domain dominated by continental ***,the high DUPAL anomaly in the Proto-and Paleo-Tethyan mantle domains records the effects of mantle plumes,which might have occurred primarily during the formation of the Proto-and Paleo-Tethys oceans during the early evolution of the Tethyan ***,the inherent coupling of mantle domain properties and plat

关键词： Tethyan domain DUPAL anomaly Large low-shear-velocity provinces(LLSVPs) Ophiolite Geodynamics

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Northward subduction-related orogenesis of the southern Altaids:Constraints from structural and metamorphic analysis of the HP/UHP accretionary complex in Chinese southwestern Tianshan,NW China

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Geoscience Frontiers 2015年第2期6卷 191-209页

作者： Mark Scheltens Lifei Zhang wenjiao xiao Jinjiang Zhang School of Earth and Space Sciences Peking University State Key Laboratory of Lithosphere Evolution Institute of Geology and Geophysics Chinese Academy of Sciences

The Chinese Tianshan belt of the southern Altaids has undergone a complicated geological evolution. Different theories have been proposed to explain its evolution and these are still hotly debated. The major subduction polarity and the way of accretion are the main problems. Southward, northward subduction and multiple subduction models have been proposed. This study focuses on the structural geology of two of the main faults in the region, the South Tianshan Fault and the Nikolaev Line. The dip direction in the Muzhaerte valley is southward and lineations all point towards the NW. Two shear sense motions have been observed within both of these fault zones, a sinistral one, and a dextral one, the latter with an age of 236-251 Ma. Structural analyses on the fault zones show that subduction has been northward rather than southward. The two shear sense directions indicate that the Yili block was first dragged along towards the east due to the cloclkwise rotation of the Tarim block. After the Tarim block stopped rotating, the Yili block still kept going eastward, inducing the dextral shear senses within the fault zones.

关键词： Structural geology Tianshan Subduction polarity HP/UHP belt

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A new ophiolitic mélange containing boninitic blocks in Alxa region:Implications for Permian subduction events in southern CAOB

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Geoscience Frontiers 2018年第5期9卷 1355-1367页

作者： Rongguo Zheng Jinyi Li wenjiao xiao Lijia Wang Institute of Geology Chinese Academy of Geological SciencesBeijing 100037China Xinjiang Research Center for Mineral Resources Xinjiang Institute of Ecology and GeographyChinese Academy of SciencesUrumqi 830011China State Key Laboratory of Lithospheric Evolution Institute of Geology and GeophysicsChinese Academy of SciencesBeijing 100029China CAS Center for Excellence in Tibetan Plateau Earth Science Chinese Academy of SciencesBeijing 100101China University of Chinese Academy of Sciences Beijing 100049China

The Alxa region, located in the southernmost part of Central Asian Orogenic Belt, is a key region for understanding the tectonic processes associated with the closure of the Paleo-Asian Ocean. Issues of late Paleozoic tectonic settings and tectonic unit divisions of the Alxa region still remain controversial. In this study, we report a new ophiolitic mélange named the Tepai ophiolitic mélange in the northern Alxa region, northwest of Alxa Youqi. The tectonic blocks in the Tepai ophiolitic mélange are mainly composed of serpentinized peridotites, serpentinites, mylonitized gabbros, gabbros, basalts, and quartzites, with a matrix comprising highly deformed clastic rocks. A gabbro exhibits a zircon LA-ICP-MS Ue Pb age of278.4 ± 3.3 Ma. Gabbros exhibit high Mg O and compatible element contents, but extremely low TiO_2,totally rare earth element and high field strength element contents. These rocks exhibit light rare earth element depleted patterns, and display enriched in large-ion lithophile elements and depleted in high field strength elements. Boninite-like geochemical data show that they were formed in a subductionrelated environment, and derived from an extremely depleted mantle source infiltrated by subduction-derived fluids and/or melts. The Tepai ophiolitic mélange exhibits similar zircon U-Pb-O isotopic compositions and whole-rock geochemical characteristics to those of the Quagan Qulu ***, we propose that the Tepai ophiolitic mélange may have been the western continuation of the Quagan Qulu ophiolite. Our new finding proves the final closure of the Paleo-Asian Ocean might have taken place later than the early Permian.

关键词： Alxa region CAOB Ophiolite LA-ICP MS U-Pb Oxygen isotope

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Magma Replenishment as Revealed by Textural and Geochemical Features of Plagioclase Phenocrysts in Subduction-Related Lavas

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Acta Geologica Sinica(English Edition) 2019年第2期93卷 464-476页

作者： LIU Xiujin LIU Wei xiao wenjiao WAN Bo Key Laboratory of Geochemical Cycling of Carbon and Mercury in the Earth's Critical Zone Institute of Geophysical and Geochemical Exploration Chinese Academy of Geological Sciences Geochemical Research Center of Soil Quality China Geological Survey Key Laboratory of Mineral Resources Institute of Geology and Geophysics Chinese Academy of Sciences Institutions of Earth Science Chinese Academy of Sciences State Key Laboratory of Lithospheric evolution Institute of Geology and Geophysics Chinese Academy of Sciences Xinjiang Research Center fo r Mineral Resources Xinjiang Institute of Geography Chinese Academy of Sciences

Various petrographic features and geochemical characteristics indicative of disequilibrium are preserved in plagioclase phenocrysts from basaltic to andesitic lavas in East Junggar, northwest China. These characteristics indicate that they crystallized in a magma chamber, which was replenished by less differentiated and high-temperature magmas. The petrographic and geochemical features of the plagioclase phenocrysts are interpreted to record responses to changes in temperature, composition and mechanical effect during magma replenishment. Distinct rare earth element(REE) patterns between cores and rims of the same plagioclase crystal suggest derivation from two end-member magmas. From core to rim, plagioclase phenocrysts commonly display sharp fluctuations of anorthite(An) content up to 20, which either correspond to reverse zoning associated with ovoidal cores and resorption surface(PI), or normal zoning with euhedral form and no resorption surface(P2). Plagioclase crystals with diverse textures and remarkably different An content coexist on the scale of a thin-section. Cores of these plagioclases in each sample display a bimodal distribution of An content. From core to rim in PI, concentrations o f FeOT and Sr increase remarkably as An content increases. During magma replenishment, pre-existing plagioclase phenocrysts in the andesitic magma, which were immersed into hotter and less differentiated magmas, were heated and resorbed to form ovoidal cores, and then were overgrown by a thin rim with much higher contents of An, FeO^T and Sr. However, pre-existing plagioclase phenocrysts in the basaltic magma were injected into cooler and more evolved magmas, and were remained as euhedral cores, which were later enclosed by oscillatory zoned rims with much lower contents of An, Sr and Ba.

关键词： magma replenishment resorption REE pattern plagioclase phenocryst East Junggar

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