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| 1 | Surface Rupture and Co-seismic Displacement Produced by the Ms 8.0 Wenchuan Earthquake of May ^(12)th,2008,Sichuan,China:Eastwards Growth of the Qinghai-Tibet Plateau显示文摘女士 8 的地震给 Wenchuan 以县,西方的四川,中国,在 2008 年 5 月 12 日并且导致了长表面破裂(> 300 km ) 。关于表面破裂的第一手的观察在 Yingxiu, Beichuan 和 Qingchuan 的最糟点击的区域由地震生产了,查明地震的原因的结构在 Longmenshan 构造的带的中央差错地区。沿着 Yingxiu-Beichuan 破裂地区活动范围 2.5-4 m 的单个差错的平均 co 地震的垂直排水量和越过中央、正面的 Longmenshan 差错的累积垂直排水量系上带子是大约 56 m。表面破裂力量从 Beichuan 的北方被归结为 Qingchuan 县和表演 23 m 右罢工滑倒部件。Wenchuan 指责戳的地震是在印度、欧亚的大陆的连续集中的行动下面的西藏的高原的东方生长的表明。 | DONG Shuwen ZHANG Yueqiao WU Zhenhan YANG Non MA Yinsheng SHI Wei CHEN Zhengle LONG Changxin AN Meijian | 2008 | Acta Geologica Sinica(English Edition)2008，82，5： | 59 |
| 2 | Jurassic Tectonic Revolution in China and New Interpretation of the “Yanshan Movement”显示文摘摘要:与结构的地质的调查的新数据和高分辨率的同位素的标明日期数据的获得和累积,我们极大地改进了我们从迟了的侏罗记在时期期间发生在东方中国到早白垩纪的构造事件的理解并且可以给性质的新解释,预定并且 Yanshan 运动的 geodynamic 背景。在中间迟了的侏罗记期间(165 挠慬獳漠 ?? | DONG Shuwen ZHANG Yueqiao LONG Changxing YANG Zhenyu JI Qiang WANG Tao HU Jianmin CHEN Xuanhua | 2008 | Acta Geologica Sinica(English Edition)2008，82，2： | 41 |
| 3 | Active Faulting Pattern,Present-day Tectonic Stress Field and Block Kinematics in the East Tibetan Plateau显示文摘这篇论文由从出版文学集成可得到的数据在东方西藏的高原检验主要活跃差错和今日的构造压力地并且建议这个区域的一个块 kinematics 模型。它证明东方西藏的高原被罢工滑倒和反向的指责压力政体统治并且最大的水平压力与当代的速度地粗略地一致,除了在哪儿的西方 Qinling 范围它罢工主要罢工滑倒指责的平行。在东方西藏的高原的活跃 tectonics 被三描绘指责系统。指责系统的离开滑倒 Kunlun-Qinling 联合东方 Kunlun 差错地区,沿着 Minshan 范围的左首的倾斜的反向的差错和切西方 Qinling 范围的二个主要旧姓惹人注目的差错,它提供东方运动,在 10 14 mm/a, Chuan-Qing 块。指责系统的离开滑倒 Xianshuihe 顺时针方向提供了 Chuan-Dian 块的旋转。指责系统的 Longmenshan 戳形成东方西藏的高原的东方边缘并且被宣传了到四川盆的 SW。越过 Longmenshan 范围的外壳的弄短似乎低(2 4 mm/a ) 并且吸收了仅仅 Chuan-Qing 块的东方运动的小部分。大多数这个东方运动被传给华南,它是在 7 9 mm/a 的动人的看见病房。东方西藏的高原的外壳和岩石圈更加被变厚,这从地球物理的数据解释被建议并且变阻器逻辑地分层。上面的外壳似乎是从通过在 15 20 km 的深度的一个 d é collement 地区的更低的外壳的 decoupled,它包含了 Longmenshan 差错带并且宣传对四川盆的 SW 东方。Wenchuan 地震就在这个 d é collement 系统的区分的点被形成。一个变阻器逻辑边界应该在在哪儿的 Longmenshan 差错带下面存在东方西藏的高原和石版印刷的更低的外壳 Yangze 块的球的披风被并列。 | ZHANG Yueqiao DONG Shuwen YANG Nong | 2009 | Acta Geologica Sinica(English Edition)2009，83，4： | 34 |
| 4 | Changes of Late Mesozoic Tectonic Regimes around the Ordos Basin(North China)and their Geodynamic Implications显示文摘合成基于岩石层位学、结构的分析在 Ordos 盆附近在地区在迟了的中生代变丑模式上在这份报纸被给。迟了的中生代构造压力进化的一张相对年表从差错 kinematics 的域分析被建立并且由 stratigraphic 接触关系抑制了。结果表演引申构造有压缩性并且 extensional 政体。Ordos 盆和它的环境在到 NNE-SSW 扩展的弱 N-S 在期间对中间的侏罗记早,它重新激活 E-W-trending 地下室破裂。构造政体在迟了的侏罗记期间改变了到多方向性的有压缩性的,它沿着 Ordos 盆的边缘的地区导致了外壳的弄短的变丑。然后,它在早白垩纪期间改变了到 extensional,哪个 rifted Ordos 盆的西方、西北、东南的边缘。NW-SE 压缩在迟了的白垩纪期间发生了并且引起了沉积的结束并且 Ordos 盆高举。在 Ordos 盆最好附近的迟了的中生代构造压力政体和联系变丑模式的这分阶段执行的进化在东亚在地区性的 geodynamic 设置记录变化,从对跟随在诺思和华南块之间的三叠纪的碰撞的中间的侏罗记 post-orogenic 扩展早,由三个盘子的同步集中生产了到迟了的侏罗记多方向性的压缩(西伯利亚的板到北方,Paleo和平的板到东方和 Lha 早白垩纪扩展可能是对倒塌并且 lithospheric 北方中国 Craton 变瘦的反应。 | ZHANG Yueqiao SHI Wei DONG Shuwen | 2011 | Acta Geologica Sinica(English Edition)2011，85，6： | 28 |
| 5 | Geohazards Induced by the Lushan Ms7.0 Earthquake in Sichuan Province, Southwest China:Typical Examples, Types and Distributional Characteristics显示文摘Geohazards induced by the Lushan Ms 7.0 earthquake on April 20, 2013 mainly have four types: collapse, landslide, slope debris flow, and sand-soil liquefaction. These geohazards mainly occurred near the epicenter, on steep slopes or below cliffs in high mountain and deep valley areas, and at or near fault ends. They have no obvious relationships to active faults, but their relationships to the weathering degree and structures of rock and rock mass are obvious. Compared with the Wenchuan Ms 8.0 earthquake on May 12, 2008, the Lushan earthquake is relatively little in the impact force and the throwing amount. All of these should be related to the magnitude of this earthquake, not very large but not very little. This character of the Lushan earthquake would make some processes uncompleted so as to bring about some concealed geohazards. Finally, in order to deal with challenges presented by such conceal geohazards, some brief recommendations are put forward. | ZHANG Yongshuang DONG Shuwen HOU Chuntang GUO Changbao YAO Xin LI Bin DU Jianjun ZHANG Jiagui | 2013 | Acta Geologica Sinica(English Edition)2013，87，3： | 24 |
| 6 | Jurassic Tectonics of North China:A Synthetic View显示文摘摘要:这份报纸在诺思中国的侏罗记 tectonics 上给一个合成看法,随建议为逐步的构造进化历史的一个框架的一次尝试。在诺思中国的侏罗记沉积,变丑和 magmatism 被划分了成三个阶段。最早的侏罗记被 magmatism 静止的一个时期标记(在 205190 妈) 并且地区性高举,它被认为是在北方和华南块之间的大陆大陆碰撞描绘的 Indosinian 运动的继续。对中间的侏罗记早(在 190170 妈)被导出披风的火成论和火山作用沿着 Yanshan 带并且在表示的弱 lithospheric 扩展支配 Tan-Lu 差错地区,沿着 Yinshan-Yanshan 构造的带的正常指责和 graben 形成,消沉并且在北方中国块(网络控制块)的广阔区域忍受煤的沉积恢复。到迟了的侏罗记舞台的中间在 165 牡敳 s 开始了 ????? | ZHANG Yueqiao DONG Shuwen ZHAO Yue ZHANG Tian | 2008 | Acta Geologica Sinica(English Edition)2008，82，2： | 23 |
| 7 | The Yanshan orogeny and late Mesozoic multi-plate convergence in East Asia—Commemorating 90th years of the “Yanshan Orogeny”显示文摘The Yanshan movement/orogeny has been proposed for 90 years, which is of special significance in the history of geological research in China. This study conducted a review by synthesizing major achievements regarding episodic deformation features, sedimentary and magmatic records of the Yanshan orogeny in China, and clarified the episodic tectono-magmatism and its geodynamic origins. The tectonic implications of the Yanshan orogeny are discussed in the context of global plate tectonics and supercontinent reconstruction. Lines of evidence from structural, sedimentary and magmatic data suggest that the Yanshan orogeny represents a regional-scale tectonic event that affected the entire China continent in late Mesozoic period. Numerous age and structural constraints consistently indicate that the Yanshan orogeny was initiated in the Jurassic(at ~170±5 Ma). and was characterized by alternating stages of crustal shortening at ~170–136 Ma, crustal extension at ~135–90 Ma, and weak shortening at ~80 Ma. The 170–136 Ma crustal shortening was reflected in the generation of two regional stratigraphic unconformities(the Tiaojishan and Zhangjiakou unconformities), which were initially named the A and B episodes of 'the Yanshan Orogeny' by Mr.Wong Wenhao in 1928. Geodynamically, the Yanshan orogeny in East Asia was associated with nearly coeval oceanic subduction and continental convergence in the Paleo-Pacific, Neo-Tethys, and Mongol-Okhotsk tectonic domains. As a consequence, three giant accretionary-collisional tectonic systems were formed along the continental margins of East Asia, i.e., the Mongol-Okhotsk, Bangonghu-Nujiang, and SE China subduction-and collision-related accretionary systems. The Yanshan orogeny induced widespread crustal-scale folding and thrusting, tectonic reactivation of long-lived zones of crustal weakness,and extensive magmatism and mineralization in intraplate regions. Based on the time principle of supercontinent assembly and break-up, we propose that the mid-Late Jurassic multi-plate convergence in East Asia might represent the initiation of the assembly of the Amasia supercontinent, and the Yanshan orogeny might be the first 'stirrings' that is a prerequisite for the birth of the Amasia supercontinent. | Shuwen DONG Yueqiao ZHANG Hailong LI Wei SHI Huaimin XUE Jianhua LI Shiqi HUANG Yongchao WANG | 2018 | Science China Earth Sciences2018，61，12： | 21 |
| 8 | Cropland redistribution to marginal lands undermines environmental sustainability显示文摘Cropland redistribution to marginal land has been reported worldwide;however,the resulting impacts on environmental sustainability have not been investigated sufficiently.Here we investigated the environmental impacts of cropland redistribution in China.As a result of urbanization-induced loss of high-quality croplands in south China(~8.5 t ha^(-1)),croplands expanded to marginal lands in northeast(~4.5 t ha^(-1)) and northwest China(~2.9 t ha^(-1)) during 1990-2015 to pursue food security.However,the reclamation in these low-yield and ecologically vulnerable zones considerably undermined local environmental sustainability,for example increasing wind erosion(+3.47%),irrigation water consumption(+34.42%),fertilizer use(+20.02%) and decreasing natural habitats(-3.11%).Forecasts show that further reclamation in marginal lands per current policies would exacerbate environmental costs by 2050.The future cropland security risk will be remarkably intensified because of the conflict between food production and environmental sustainability.Our research suggests that globally emerging reclamation of marginal lands should be restricted and crop yield boost should be encouraged for both food security and environmental benefits. | Wenhui Kuang Jiyuan Liu Hanqin Tian Hao Shi Jinwei Dong Changqing Song Xiaoyong Li Guoming Du Yali Hou Dengsheng Lu Wenfeng Chi Tao Pan Shuwen Zhang Rafiq Hamdi Zherui Yin Huimin Yan Changzhen Yan Shixin Wu Rendong Li Jiuchun Yang Yinyin Dou Wenbin Wu Liqiao Liang Bao Xiang Shiqi Yang | 2022 | National Science Review2022，9，1： | 13 |
| 9 | Mineral chemistry, geochemistry and U-Pb SHRIMP zircon data of the Yangxin monzonitic intrusive in the foreland of the Dabie orogen显示文摘The Yangxin composite intrusive consists of three generations of plutons, among which 90% are the second generation intrusions. The second generation intrusion has U-Pb SHRIMP zircon age of 134±2 Ma, substantially younger than the early stage of the Yanshanian. Amphibole and biotite, major mafic minerals in the Yangxin plutons, are rich in magnesium, suggesting a deep source of their parental magma, possibly derived from the upper mantle. Whole rock geochemical data on these rocks show that they have high Al2O3 (15.92%―16.38%), relatively high alkali (Na2O+K2O = 6.95%―7.37%) and higher Na2O contents than K2O (Na2O/K2O = 1.47―1.94). They also have high Sr con-tents (816―897 μg/g) are enriched in strong incompatible elements such as Rb, U, Th, K and LREE, but depleted in HREE and Y. Strong fractionation of LREE from HREE as indicated by high (La/Yb)N ratios ranging from 17.83 to 20.86. Although with little difference, the whole characteristics of the Yangxin intrusive body are greatly similar to the adakite, referring that the formation of the parental magma may relate with the partial melting of the basalt underplating from the mantle after delamina-tion of the mountain root of the Dabie orogen. The body has been uplifted about 5 km since cooling concretion, the average rate was only about 0.04 mm/a,much slower than that of the Dabie orogen in late Mesozoic, but the rates of denudation in two area are similar in Cenozoic. | XUE Huaimin DONG Shuwen JIAN Ping | 2006 | Science China Earth Sciences2006，49，7： | 12 |
| 10 | Discovery of low grade metamorphic volcanic rock sheets within UHP in Dabie Mts. and its implications显示文摘THE ultrahigh-pressure metamorphic zone (UHP), outcropping in the central and southernDabie Mts. with an area of about 1000 km^2, may be the largest one in the world. The forma-tion and exhumation mechanism of the UHP rocks become a hot point in the study of continen-tal orogen. The first finding of the Shiqiao structural window, which is composed of low | DONG Shuwen, WANG Xiaofeng and HUANG Dezhi1. Chinese Academy of Geological Sciences (CAGS), Beijing 100037, China 2. Institute of Geomechanics of CAGS, Beijing 100081 China 3. Anhui Institute of Geological Sciences, Hefei 230001 | 1997 | Chinese Science Bulletin1997，42，14： | 10 |
| 11 | Formation of the Moping Dome in the Xuefengshan Orocline, Central China and its Tectonic Significance显示文摘Many equiaxial dome-like structures developed in the north segment of the Xuefengshan orocline, Central China are obviously inconcordant with the NE-trending linear structures in this area, which contain important records for understanding the structural framework and evolution of this belt. In this paper, taking one of the typical dome-like structures in the Xuefengshan orcline (e.g. Moping dome-like structure) as an example, based on its structural framework interpratatoin, superposed deformation analysis and paleo-stress fields reconstruction, we propose the Moping dome-like structure is composed of two populations of different-striking thrust-fold structures, ~E-trending and NE-striking structures, indicative of two-stages shortening, ~N- and NW-striking, respectively. Together with the geochronological analysis, we suggest the first stage of shortening occurred in Late Triassic to Early Jurassic, due to the Indosinian intercollisional orogeny of the Yangtze Block and the North China Block. The second occurred during Late Jurassic Early Cretaceous owing to Yanshanian intracontinental orogeny, leading to the intensive superposition of the NE-trending structures onto the ~E-trending structures, and the final ocurrence of the Moping dome. Thus, our study indicates the Xuefengshan arc-shape belt also experienced two-phase deformation, and resulted from the superposition of NE SW structures onto ~E-W structures in Late Jurassic Early Cretaceous, which could provide new structural evidence for probing the Mesozoic tectonic framework and evolution of the Xuefengshan orocline. | SHI Wei DONG Shuwen LI Jianhua TIAN Mi WU Guoli | 2013 | Acta Geologica Sinica(English Edition)2013，87，3： | 9 |
| 12 | Dextral-Slip Thrust Faulting and Seismic Events of the Ms 8.0 Wenchuan Earthquake,Longmenshan Mountains,Eastern Margin of the Tibetan Plateau显示文摘Dextral-slip thrust movement of the Songpan-Garzê terrain over the Sichuan block caused the M_s 8.0 Wenchuan earthquake of May 12,2008 and offset the Central Longmenshan Fault(CLF) along a distance of~250 km.Displacement along the CLF changes from Yingxiu to Qingchuan.The total oblique slip of up to 7.6 m in Yingxiu near the epicenter of the earthquake,decreases northeastward to 5.3 m,6.6 m,4.4 m,2.5 m and 1.1 m in Hongkou,Beichuan,Pingtong,Nanba and Qingchuan,respectively.This offset apparently occurred during a sequence of four reported seismic events,EQ1-EQ4,which were identified by seismic inversion of the source mechanism.These events occurred in rapid succession as the fault break propagated northeastward during the earthquake. Variations in the plunge of slickensides along the CLF appear to match these events.The Mw 7.5 EQ1 event occurred during the first 0-10 s along the Yingxiu-Hongkou section of the CLF and is characterized by 1.7 m vertical slip and vertical slickensides.The Mw 8.0 EQ2 event,which occurred during the next 10-42 s along the Yingxiu-Yanziyan section of the CLF,is marked by major dextralslip with minor thrust and slickensides plunging 25°-35°southwestward.The Mw 7.5 EQ3 event occurred during the following 42-60 s and resulted in dextral-slip and slickensides plunging 10°southwestward in Beichuan and plunging 73°southwestward in Hongkou.The Mw 7.7 EQ4 event, which occurred during the final 60-95 s along the Beichuan-Qingchuan section of the CLF,is characterized by nearly equal values of dextral and vertical slips with slickensides plunging 45°-50°southwestward.These seismic events match and evidently controlled the concentrations of landslide dams caused by the Wenchuan earthquake in Longmenshan Mountains. | WU Zhenhan DONG Shuwen Patrick J. BAROSH ZHANG Zuoheng LIAO Huaijun | 2009 | Acta Geologica Sinica(English Edition)2009，83，4： | 8 |
| 13 | Seismogenic Structure around the Epicenter of the May 12,2008 Wenchuan Earthquake from Micro-seismic Tomography显示文摘一个三维的本地规模的 P 速度模型在下面到 25 km,在主要吃惊震中区域附近的深度用从 5856 余震的地震光线由一个最新部署的暂时的地震网络记录了的 83821 event-to-receiver 被构造。棋盘测试证明我们的 tomographic 模型有 ∼2 km 的侧面、垂直的分辨率。高分辨率的 P 速度模型在 seismogenic 层揭示了有趣的结构:(1 ) Guanxian-Anxian 差错, Yingxiu-Beichuan 差错和 Longmen 掸人差错地区的 Wenchuan-Maoxian 差错好由突然地上面的外壳的速度变化描出;(2 ) Pengguan 山岳比它的包围区域有通常更高的速度,并且可以延长在下面到从表面的至少 ∼10 km;(3 ) 在 Wenchuan-Maoxian 差错下面的一个突然地侧面的速度变化可以显示 Pengguan 山岳的西方的边界或 Wenchuan-Maoxian 差错是垂直的,并且 Wenchuan 地震的低亚硫酸钠中心可能在蘸 Yingxiu-Beichuan 和 Guanxian-Anxian 差错,和垂直 Wenchuan-Maoxian 差错的 NW 的连词点定位;(4 ) 沿着 Yingxiu-Beichuan 差错的附近被很低的速度和低 seismicity 在浅深度描绘,可能由于孔和破裂的高内容;(5 ) 二块低速度的异例分别地与 ∼5 km 与 ∼7 km 偏移量在挂的墙和 Guanxian-Anxian 差错的脚墙中被想象垂直部件。 | AN Meijian FENG Mei DONG Shuwen LONG Changxing ZHAO Yue YANG Nong ZHAO Wenjin ZHANG Jizhong | 2009 | Acta Geologica Sinica(English Edition)2009，83，4： | 7 |
| 14 | Formation of Natural Bitumen and its Implication for Oil/gas Prospect in Dabashan Foreland显示文摘Natural bitumen is the evolutionary residue of hydrocarbon of sedimentary organic matter.Several kinds of bitumen with different occurrences,including bitumen in source rock,migration bitumen filled in fault,oil-bed bitumen and paleo-reservoir bitumen,are distributed widely in the Dabashan foreland.These kinds of bitumen represent the process of oil/gas formation,migration and accumulation in the region.Bitumen in source rock filled in fractures and stylolite and experienced deformation simultaneously together with source rock themselves.It indicated that oil/gas generation and expelling from source rock occurred under normal buried thermal conditions during prototype basin evolution stages prior to orogeny.Occurrences of bitumen in source rock indicated that paleo-reservoir formation conditions existed in the Dabashan foreland.Migration bitumen being widespread in the fault revealed that the fault was the main channel for oil/gas migration,which occurred synchronously with Jurassic foreland deformation.Oil-bed bitumen was the kind of pyrolysis bitumen that distributed in solution pores of reservoir rock in the Dabashan foreland depression,the northeastern Sichuan Basin.Geochemistry of oil-bed bitumen indicated that natural gas that accumulated in the Dabashan foreland depression formed from liquid hydrocarbon by pyrolysis process.However,paleo-reservior bitumen in the Dabashan forleland was the kind of degradation bitumen that formed from liquid hydrocarbon within the paleo-reservior by oxidation,alteration and other secondary changes due to paleo-reservior damage during tectonics in the Dabashan foreland.In combination with the tectonic evolution of the Dabashan foreland,it is proposed that the oil/gas generated,migrated and accumulated to form the paleo-reservoir during the Triassic Indosinian tectonic movement.Jurassic collision orogeny,the Yanshan tectonic movement,led to intracontinental orogeny of the Dabashan area accompanied by geofluid expelling and paleo-reservoir damage in the Dabashan foreland.The present work proposed that there is liquid hydrocarbon exploration potential in the Dabashan foreland,while there are prospects for the existence of natural gas in the Dabashan foreland depression. | LI Rongxi DONG Shuwen ZHANG Xue ZHU Ruijing | 2012 | Acta Geologica Sinica(English Edition)2012，86，2： | 7 |
| 15 | Seismogenic Structure of the April 20, 2013, Lushan Ms7 Earthquake in Sichuan显示文摘At 08:02 on April 20, 2013, a Ms7.0 earthquake occurred in Lushan, Ya'an, in the Longmenshan fault zone, Sichuan. The epicenter was located between Taiping Town and Shuangshi Town, Lushan County and the maximum earthquake intensity at the epicenter reached class IX. Field investigations in the epicenter area found that, although buildings were seriously damaged, no obvious surface rupture structure was produced, only some ground fissures and sand blows and water ejection phenomena being seen. An integrated analysis of high-resolution remote sensing image interpretation, mainshock and aftershock distribution, and focal mechanism solutions indicated that this earthquake was an independent rupturing event in the southwestern segment of the Longmenshan fault zone, belonging to the thrust-type earthquake. Ruptures occurred along the south-central segment of the Shuangshi-Dachuan fault and the principal rupture plane dipped SW at 33-43°. It is inferred that the Lushan earthquake might be related to the ramp activity of the basal detachment zone (13-19 km) of the Longmenshan fault zone. Historically, there occurred at least two Ms6-6.5 earthquakes along the Shuangshi-Dachuan fault zone; thus it is thought that the Lushan earthquake, different from the Wenchuan earthquake, was a characteristic one in the southwestern segment of the Longmenshan fault zone. In-situ stress measurements indicated the Lushan earthquake was the result of stress release of the southwestern segment of the Longmenshan fault zone after the Wenchuan earthquake. This paper analyzes the tectonic setting of the seismogenic structure of this earthquake. | ZHANG Yueqiao DONG Shuwen HOU Chuntang SHI Jusong WU Zhonghai LI Hailong SUN Ping LIU Gang LI Jian | 2013 | Acta Geologica Sinica(English Edition)2013，87，3： | 7 |
| 16 | Geochronology and Hf Isotopes of Granite Gravel from Fanjingshan, South China: Implication for the Precambrian Tectonic Evolution of Western Jiangnan Orogen显示文摘The debate of assembly time between the Yangtze and Cathaysia blocks has aroused the disputation on the formation mechanism of Jiangnan orogen, South China. Therefore widespread magmatism of 830–750 Ma in South China is interpreted as the product of either plume or arc magmatism, which results in distinctive depositional background in the Neoproterozoic. Granite gravel located at the unconformity between the Banxi Group and Fanjingshan Group of the western Jiangnan orogen was collected, which gave a new age limit to the deposition of the Banxi Group and Nanhu rift. Zircons from the granite gravel crystallized yield a weighted mean 206Pb/238U age of 789±11 Ma, which probably represents the end of the Jiangnan orogeny and marks the onset of Nanhua rift. These zircons have negative εHf(t) of-2.1 to-6.0, with TDM of 1.38–1.52 Ga and Tcrust of 1.81–1.98 Ga indicating an old continental crust origin for the granite. | Jinbao Su Yueqiao Zhang Shuwen Dong Xuanhua Chen Yong Li Jianjun Cui | 2014 | Journal of Earth Science2014，25，4： | 6 |
| 17 | Characteristics of Hydrocarbon Fluid Inclusions and Their Significance for Evolution of Petroleum Systems in the Dabashan Foreland,Central China显示文摘Field investigation combined with detailed petrographic observation indicate that abundant oil,gas,and solid bitumen inclusions were entrapped in veins and cements of sedimentary rocks in the Dabashan foreland,which were used to reconstruct the oil and gas migration history in the context of tectonic evolution.Three stages of veins were recognized and related to the collision between the North China block and the Yangtze block during the Indosinian orogeny from Late Triassic to Early Jurassic(Dl),the southwest thrusting of the Qinling orogenic belt towards the Sichuan basin during the Yanshanian orogeny from Late Jurassic to Early Cretaceous(D2),and extensional tectonics during Late Cretaceous to Paleogene(D3),respectively.The occurrences of hydrocarbon inclusions in these veins and their homogenization temperatures suggest that oil was generated in the early stage of tectonic evolution,and gas was generated later,whereas solid bitumen was the result of pyrolysis of previously accumulated hydrocarbons.Three stages of hydrocarbon fluid inclusions were also identified in cements of carbonates and sandstones of gas beds in the Dabashan foreland belt and the Dabashan foreland depression(northeastern Sichuan basin),which recorded oil/gas formation,migration,accumulation and destruction of paleo-reservoirs during the D2.Isotopic analysis of hydrocarbon fluid inclusions contained in vein minerals shows that δ^(13)C_1 of gas in fluid inclusions ranges from-17.0‰ to-30.4‰(PDB) and δD from-107.7‰ to-156.7‰(SMOW),which indicates that the gas captured in the veins was migrated natural gas which may be correlated with gas from the gas-fields in northern Sichuan basin.Organic geochemical comparison between bitumen and potential source rocks indicates that the Lower Cambrian black shale and the Lower Permian black limestone were the most possible source rocks of the bitumen.Combined with tectonic evolution history of the Dabashan foreland,the results of this study suggest that oil was generated from the Paleozoic source rocks in the Dabashan area under normal burial thermal conditions before Indosinian tectonics and accumulated to form paleo-reservoirs during Indosinian collision between the North China block and the Yangtz block.The paleo-reservoirs were destroyed during the Yanshanian tectonic movement when the Dabashan foreland was formed.At the same time,oil in the paleo-reservoirs in the Dabashan foreland depression was pyrolyzed to transform to dry gas and the residues became solid bitumen. | LI Rongxi QIN Xiaoli DONG Shuwen LIU Shuwen | 2015 | Acta Geologica Sinica(English Edition)2015，89，3： | 4 |
| 18 | Chokeberry(Aronia melanocarpa)as a new functional food relationship with health:an overview显示文摘As a consumer product,black chokeberry(Aronia melanocarpa)is diffi cult to consume due to its pungent taste.It is mainly used in various food industries to produce a variety of juices,preserves,extracts,fruit teas and nutritional supplements.Traditionally,Potawatomi Native Americans used black chokeberry to treat colds,coughs and fever.It has been found to contain numerous active ingredients.Currently,there are many health and medical products that contain black chokeberry.The purpose of this review is to understand the nutritional benefi ts of black chokeberry and to explore its benefi cial effects on biological systems in vitro,thereby emphasizing its therapeutic prospects. | Yiwen Zhang Yingchun Zhao Xinglong Liu Xueyan Chen Chuanbo Ding Ling Dong Jinping Zhang Shuwen Sun Qiteng Ding Sadia Khatoom Zhiqiang Cheng Wencong Liu Liqian Shen Fengyan Xiao | 2021 | Journal of Future Foods2021，1，2： | 3 |
| 19 | Soil Erodibility and Physicochemical Properties of Collapsing Gully Alluvial Fans in Southern China显示文摘In southern China, collapsing gully erosion produces massive deposits of sediment on the plough layer of alluvial fan farmland,leading to reduced nutrients, increased erodibility, and even desertification. The aim of this study was to investigate soil erodibility(the factor K in the Universal Soil Loss Equation, USLE) and physicochemical properties of the alluvial fans of the most severe collapsing gully erosion areas(Hubei, Jiangxi, Fujian, and Guangdong provinces) in southern China. The soils of the collapsing gully alluvial fans had a higher bulk density, but a lower total porosity, saturated water content, and silt and clay fractions than the control(CK) soils from the farmland without desertification. Soil quality gradually decreased from fan edge to fanhead. Significant decreases were found in soil p H, organic matter, cation exchange capacity, and total potassium, nitrogen, and phosphorus, as well as available nitrogen, phosphorus, and potassium, resulting in a gradual decrease in soil nutrients from the fanedge to the fanhead. Soil erodibility was greatest in the fanhead, and soil erodibility K values of the alluvial fans were 53.71%, 66.28%, 67.53%, and 71.68% greater than that in those of the CK soils of Hubei, Jiangxi, Fujian, and Guangdong, respectively, indicating a significant correlation between the soil erodibility K values and physicochemical properties, particularly sand fraction and organic matter content. The results provide new insights into the relationship between soil physicochemical properties and erodibility of alluvial fans, and suggest that improving soil structure might increase soil fertility in the collapsing gully alluvial fan farmland. | DENG Yusong SHEN Xue XIA Dong CAI Chongfa DING Shuwen WANG Tianwei | 2019 | Pedosphere2019，29，1： | 3 |
| 20 | Construction of the Continental Asia in Phanerozoic:A Review显示文摘This is a review of the formation and tectonic evolution of the continental Asia in Phanerozoic.The continental Asia has formed on the bases of some pre-Cambrian cratons,such as the Siberia,India,Arabia,North China,Tarim,South China,and Indochina,through multi-stage plate convergence and collisional collages in Phanerozoic.The north-central Asia had experienced the expansion and subduction of the Paleo-Asian Ocean(PAO)in the early Paleozoic and the closure of the PAO in the late Paleozoic and early Mesozoic,forming the PAO regime and Central Asian orogenic belt(CAOB).In the core of the CAOB,the Mongol-Okhotsk Ocean(MOO)opened with limited expansion in the Early Permian and finally closed in the Late Jurassic–Early Cretaceous.The south-central Asia had experienced mainly multi-stage oceanic opening,subduction and collision evolution in the Tethys Ocean,forming the Tethys regime and Himalaya-Tibetan orogenic belt.In eastern Asia,the plate subduction and continental margin orogeny on western margin of the Pacific Ocean,forms the West Pacific regime and West Pacific orogenic belt.The PAO,Tethys,and West Pacific regimes,together with Precambrian cratons among or surrounding them,made up the major tectonic and dynamic systems of the continental Asia in Phanerozoic.Major tectonic events,such as the Early Paleozoic Qilian,Uralian,and Dunhuang orogeneses,the late Paleozoic East Junggar,Tianshan and West Junggar orogeneses,the Middle to Late Permian Ailaoshan orogeny and NorthSouth Lhasa collision,the early Mesozoic Indochina-South China and North-South China collisions,the late Mesozoic Mongolia-Okhotsk orogeny,Lhasa-Qiangtang collision,and intra-continental Yanshanian orogeny,and the Cenozoic IndoAsian,Arab-Asian,and West Pacific margin collisions,constrained the formation and evolution of the continental Asia.The complex dynamic systems have left large number of deformation features,such as large-scale strike-slip faults,thrustfold systems and extensional detachments on the continental Asia.Based on past tectonics,a future supercontinent,the Ameurasia,is prospected for the development of the Asia in ca.250 Myr. | CHEN Xuanhua DONG Shuwen SHI Wei DING Weicui ZHANG Yiping LI Bing SHAO Zhaogang WANG Ye | 2022 | Acta Geologica Sinica(English Edition)2022，96，1： | 3 |
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