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| 1 | Late Quaternary normal faulting and its kinematic mechanism of eastern piedmont fault of the Haba-Yulong Snow Mountains in northwestern Yunnan, China显示文摘The regional geologic and geomorphic observations show that an active arcuate normal fault constitutes the main boundary fault of the Haba-Yulong Snow Mountains (HYSM). This fault is called eastern piedmont fault of Haba-Yulong Snow Mountains (HYPF). The fault consists of two segments with differential trend; the northern segment is NW-trending and NE-dipping and the southern section is S-N trending and E-dipping. Three sets of fault scarps cutting late Quaternary landforms and their dating results indicate that the fault is a prominent Holocene active fault and its throw rates are 0.3―1.4 mm/a during late Quaternary. The geometry and kinematics of the fault suggest that the arcuate normal faulting or rifting are typical surface deformation pattern at the two tips of the Z-shaped rift zone of northwestern Yunnan, which is related to regional east-west extension accompanying clockwise rota- tion of micro-block. | WU ZhongHai ZHANG YongShuang HU DaoGong ZHAO XiTao YE PeiSheng | 2009 | Science China Earth Sciences2009，52，10： | 14 |
| 2 | Early Cenozoic Tectonics of the Tibetan Plateau显示文摘Geological mapping at a scale of 1:250000 coupled with related researches in recent years reveal well Early Cenozoic paleo-tectonic evolution of the Tibetan Plateau. Marine deposits and foraminifera assemblages indicate that the Tethys-Himalaya Ocean and the Southwest Tarim Sea existed in the south and north of the Tibetan Plateau, respectively, in Paleocene-Eocene. The paleooceanic plate between the Indian continental plate and the Lhasa block had been as wide as 900km at beginning of the Cenozoic Era. Late Paleocene transgressions of the paleo-sea led to the formation of paleo-bays in the southern Lhasa block. Northward subduction of the Tethys-Himalaya Oceanic Plate caused magma emplacement and volcanic eruptions of the Linzizong Group in 64.5-44.3 Ma, which formed the Paleocene-Eocene Gangdise Magmatic Arc in the north of Yalung-Zangbu Suture (YZS), accompanied by intensive thrust in the Lhasa, Qiangtang, Hoh Xil and Kunlun blocks. The Paleocene-Eocene depression of basins reached to a depth of 3500-4800 m along major thrust faults and 680-850 m along the boundary normal faults in central Tibetan Plateau, and the Paleocene-Eocene depression of the Tarim and Qaidam basins without evident contractions were only as deep as 300-580 m and 600-830 m, respectively, far away from central Tibetan Plateau. Low elevation plains formed in the southern continental margin of the Tethy-Himalaya Ocean, the central Tibet and the Tarim basin in Paleocene-Early Eocene. The Tibetan Plateau and Himalaya Mts. mainly uplifted after the Indian-Eurasian continental collision in Early-Middle Eocene. | WU Zhenhan HU Daogong YE Peisheng WU Zhonghai | 2013 | Acta Geologica Sinica(English Edition)2013，87，2： | 9 |
| 3 | Miocene Tectonic Evolution from Dextral-Slip Thrusting to Extension in the Nyainqentanglha Region of the Tibetan Plateau显示文摘在西藏的 Nyainqentanglha 区域的右滑倒导致了 obliqueunderthrusting 和花岗石产生在对中间早中新世,但是在时代底高举并且紧张的指责统治了的前。东方西方右滑倒 Gangdise 差错系统合并进东北趋势东方,转动东方更远的北方进右滑倒北方 Damxung 剪碎带和 Jiali 的蘸东南的 Nyainqentanglha 戳系统指责。这些差错是形成了由当西方的块不到东方的开车了,早, Miocene,和大 Nyainqentanglha 花岗石的底盘在 18.3-11.0 妈形成了戳系统。Thedextral 滑倒运动在~ 1 结束了 1 个妈和底盘玫瑰,由在 8.6-8.3 妈的重力的砍标记,一个新差错系统发展了。西北趋势右滑倒差错形成了到 raisen 底盘的西北,而有某左首滑倒的东北趋势南方 Damxung 上投断层形成了到东南。后者被 thewest-northwest-trending Lhiinzhub 上投断层被右滑倒远代替到东方。这相对本地高举让存款保存了的 Eocene 和 Miocene 邻近那被区域抬升和一个系统的开始跟随通常纵贯抓住 ens 在在~ 6 .5 晚中新世妈。Theregional 高举南部的西藏的高原因此看起来发生在 8.3 妈和 6.5Ma 之间。Gulu, Damxung-Yangbajain 和 Angan 在 NyainqentanglhaMountains 的通行证东方被更早的东北趋势差错局部地控制的系统抓住。这些抓住 ens 统治随后的构造运动并且山向西北作为西北趋势右滑倒差错仍然很活跃。Miocene 是迎来了现代构造政体的大构造变化的一时间。 | WU Zhenhan Patrick J. BAROSH ZHAO Xun WU Zhonghai HU Daogong LIU Qisheng | 2007 | Acta Geologica Sinica(English Edition)2007，81，3： | 8 |
| 4 | Surface Rupture of the 1515 Yongsheng Earthquake in Northwest Yunnan, and Its Seismogeological Implications显示文摘The 1515 M7? Yongsheng earthquake is the strongest earthquake historically in northwest Yunnan. However, its time, magnitude and the seismogenic fault have long been a topic of dispute. In order to accurately define those problems, a 1:50000 active tectonic mapping was carried out along the northern segment of the Chenghai–Binchuan fault zone. The result shows that there is an at least 25 km–long surface rupture and a series of seismic landslides distributed along the Jinguan fault and the Chenghai fault. Radiocarbon dating of the ^(14) C samples indicates that the surface rupture should be a part of the deformation zone caused by the Yongsheng earthquake in the year 1515. The distribution characteristics of this surface rupture indicate that the macroscopic epicenter of the 1515 Yongsheng earthquake may be located near Hongshiya, and the seismogenic fault of this earthquake is the Jinguan–Chenghai fault, the northern part of the Chenghai–Binchuan fault zone. Striations on the surface rupture show that the latest motion of the fault is normal faulting. The maximum co–seismic vertical displacement can be 3.8 m, according to the empirical formula for the fault displacement and moment magnitude relationship, the moment magnitude of the Yongsheng earthquake was Mw 7.3–7.4. Furthermore, combining published age data with the ^(14) C data in this paper reveals that at least four large earthquakes of similar size to the 1515 Yongsheng earthquake, have taken place across the northern segment of the Chenghai–Binchuan fault zone since 17190±50 yr. BP. The in–situ recurrence interval of Mw 7.3–7.4 characteristic earthquakes in Yongsheng along this fault zone is possibly on the order of 6 ka. | HUANG Xiaolong WU Zhonghai WU Kungang | 2018 | Acta Geologica Sinica(English Edition)2018，92，4： | 8 |
| 5 | 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 |
| 6 | An Application-Oriented Cache Allocation and Prefetching Method for Long-Running Applications in Distributed Storage Systems显示文摘Characteristics of long-running applications in cloud and big data environment are various and significantly influence the performance of cache systems.The gap between existing cache systems and the increasing performance requirements motivates us to propose the Application-oriented cache allocation and prefetching method(ACAP)to improve data access performance.An application-oriented cache allocation approach is designed based on hit count growth rates for a higher overall hit rate.Two application-oriented sequential prefetching approaches are proposed to improve the hit rate and prefetching accuracy by learning average read sizes of long-running applications.Based on correlation of data accesses,a parallelized correlated-directed prefetching approach is proposed to further increase the hit rate.Above approaches are intergrated to obtain the maximized hit rate and prefetching accuracy.Experimental results on12 public real system traces show that ACAP achieves14.03%(up to 33.82%)higher prefetching accuracy and2.01%(up to 7.54%)higher hit rate compared with the best combination of baselines. | GUO Chang LI Ying LIU Hongzhi WU Zhonghai | 2019 | Chinese Journal of Electronics2019，28，4： | 4 |
| 7 | Age and Origin of Paleogene Granitoids from Western Yunnan Province,China:Geochemistry,SHRIMP Zircon Ages,and Hf-in-Zircon Isotopic Compositions显示文摘We report geochemical data, SHRIMP zircon ages and Hf-in-zircon isotopic compositions for Cenozoic granitoids from major fault systems in the Tethyan belt in western Yunnan Province, southwestern China.Four magmatic pulses occurred in the Paleogene, namely at ca.57 Ma, ca.50 Ma, 45–40 Ma, and 38–34 Ma.Early magmatism of this episode(57–50 Ma) produced S-type granites whose zircons yielded εHf(t) values of-5.0 to-0.3.In contrast, late magmatism of this episode reflects heterogeneous sources.Zircons from a granite porphyry along the Ailaoshan-Red River fault system have slightly positive εHf(t) values suggesting derivation from relatively young crust and/or a juvenile source.However, zircons from a granite along the Gaoligong fault system have strongly negative εHf(t) values and suggest derivation from a Paleoproterozoic crustal source.The composition of the granitoids varies with age(from ca.57 Ma to ca.34 Ma) from peraluminous to metaluminous and also suggests a change from syn-collisional to late-orogenic tectonic setting.A new tectonic model, impacting lithospheric wedge(ILW) is shown for the origin of Paleogene granitoids in this paper. | SHI Yuruo WU Zhonghai Alfred KRoNER FAN Taoyuan YANG Zhenyu | 2015 | Acta Geologica Sinica(English Edition)2015，89，5： | 3 |
| 8 | Late Cenozoic Geomorphology, Geochronology and Physiography of Yuntaishan in Southern Taihang Mountain, North China显示文摘在 Yuntaishan 世界 Geopark 的 Zhingfang 河集水的迟了的新生代似地球形状的特征和 geochronologic 数据被学习。几个 quarternary geochronologic 方法,包括的电子旋转回声(ESR ) ,光学地刺激的光(OSL ) ,热照明(TL ) 和 U 系列在这份报纸被介绍。结果建议有二均夷作用表面,作为是在渐新世或渐新世期间形成到早中间的中新世的时期的 Taihang 舞台的一个近似平原的 Taihang 表面说出,并且是 Tang-hien 舞台的一条成熟宽山谷的 Tang-hien 表面在晚中新世上新世或上新世早的更新世时期期间形成了并且可能基于 ESR 在 2.22.6 妈以前结束了标明日期。在 Tang-hien 阶段以后,河的切口和沉积分别地在河底部上面与 35 m, 812 m, 2224 m, 2838 m, 5062 m 和 8085 m 的高度形成了六个溪流平台。冲积层沉积的标明日期的结果建议这些平台在 Holocene, 2023 ka B.P, 110120 ka B.P, 200240 ka B.P, 8401200 ka B.P 或 450 ka 期间被形成 B.P 或 1100 ka B.P 分别地。这些结果显示河的阵发性的切口,在 Yuntaishan 世界 Geopark 控制风景的形成,被周期的干燥湿的气候变化主要在迟了的新生代山期间影响高举。 | WU Zhonghai ZHAO Xitao MA Yinsheng ZHAO Xun ZHAO Ting YANG Shouzheng GAO Linzhi | 2010 | Acta Geologica Sinica(English Edition)2010，84，1： | 3 |
| 9 | Late Cenozoic Sedimentary Evolution of Pagri-Duoqing Co graben, Southern End of Yadong-Gulu Rift, Southern Tibet显示文摘The north trending rifts in southern Tibet represent the E-W extension of the plateau and confirming the initial rifting age is key to the study of mechanics of these rifts. Pagri-Duoqing Co graben is located at southern end of Yadong-Gulu rift, where the late Cenozoic sediments is predominately composed of fluvio-lacustrine and moraine. Based on the sedimentary composition and structures, the fluviolacustrine could be divided into three facies, namely, lacustrine, lacustrine fan delta and alluvial fan. The presence of paleo-currents and conglomerate components and the provenance of the strata around the graben indicate that it was Tethys Himalaya and High Himalaya. Electron spin resonance(ESR) dating and paleo-magnetic dating suggest that the age of the strata ranges from ca. 1.2 Ma to ca. 8 Ma. Optically stimulated luminescence(OSL) dating showed that moraine in the graben mainly developed from around181-109 ka(late Middle Pleistocene). Combining previous data about the Late Cenozoic strata in other basins, it is suggested that 8-15 Ma may be the initial rifting time. Together with sediment distribution and drainage system, the sedimentary evolution of Pagri could be divided into four stages. The graben rifted at around 15-8 Ma due to the eastern graben-boundary fault resulting in the appearance of a paleolake.Following by a geologically quiet period about 8-2.5 Ma, the paleolake expanded from east to west at around 8-6 Ma reaching its maximum at ca. 6 Ma. Then, the graben was broken at about 2.5 Ma. At last,the development of the glacier separated the graben into two parts that were Pagri and Duoqing Co since the later stages of the Middle Pleistocene. The evolution process suggested that the former three stages were related to the tectonic movement, which determined the basement of the graben, while the last stage may have been influenced by glacial activity caused by climate change. | HA Guanghao WU Zhonghai HE Lin WANG Shubing | 2018 | Acta Geologica Sinica(English Edition)2018，92，3： | 3 |
| 10 | Tectonics and Topography of the Tibetan Plateau in Early Miocene显示文摘Early Miocene stratigraphy, major structural systems, magmatic emplacement, volcanic eruption, vegetation change and paleo-elevation were analyzed for the Tibetan Plateau after regional geological mapping at a scale of 1:250,000 and related researches, revealing much more information for tectonic evolution and topographic change of the high plateau caused by Indian-Asian continental collision. Lacustrine deposits of dolostone, dolomite limestone, limestone, marl, sandstone and conglomerate of weak deformation formed extensively in the central Tibetan Plateau, indicating that vast lake complexes as large as 100,000–120,000 km2 existed in the central plateau during Early Miocene. Sporopollen assemblages contained in the lacustrine strata indicate the disappearance of most tropical-subtropical broad-leaved trees since Early Miocene and the flourishing of dark needleleaved trees during Early Miocene. Such vegetation changes adjusted for latitude and global climate variations demonstrate that the central Tibetan Plateau rose to ca. 4,000–4,500 m and the northeastern plateau uplifted to ca. 3,500–4,000 m before the Early Miocene. Intensive thrust and crustal thickening occurred in the areas surrounding central Tibetan Plateau in Early Miocene, formed Gangdise Thrust System(GTS) in the southern Lhasa block, Zedong-Renbu Thrust(ZRT) in the northern Himalaya block, Main Central Thrust(MCT) and Main Boundary Thrust(MBT) in the southern Himalaya block, and regional thrust systems in the Qaidam, Qilian, West Kunlun and Songpan-Ganzi blocks. Foreland basins formed in Early Miocene along major thrust systems, e.g. the Siwalik basin along MCT, Yalung-Zangbu Basin along GTS and ZRT, southwestern Tarim depression along West Kunlun Thrust, and large foreland basins along major thrust systems in the northeastern margin of the plateau. Intensive volcanic eruptions formed in the Qiangtang, Hoh-Xil and Kunlun blocks, porphyry granites and volcanic eruptions formed in the Nainqentanglha and Gangdise Mts., and leucogranites and granites formed in the Himalaya and Longmenshan Mts. in Early Miocene. The K2O weight percentages of Early Miocene magmatic rocks in the Gangdise and Himlayan Mts. are found to increase with distance from the MBT, indicating the genetic relationship between regional magmatism and subduction of Indian continental plate in Early Miocene. | WU Zhenhan YANG Yan Patrick J. BAROSH WU Zhonghai ZHANG Yaoling | 2014 | Acta Geologica Sinica(English Edition)2014，88，2： | 2 |
| 11 | Nikethamide affects inspiratory neuron discharge in the nucleus retrofacialis medial region in brain slices from neonatal rats显示文摘BACKGROUND:Nikethamide,a respiratory center stimulant,is widely used in China.However,its effects on the central nervous system and medullary respiratory center remain poorly understood.OBJECTIVE:To investigate the influence of nikethamide on inspiratory neuron discharge in the medial region of the nucleus retrofacialis in neonatal rats,based on the observations addressing rhythmic respiratory discharge generated by the basic medullary respiratory center and various respiration neuron discharges in brain slices.DESIGN,TIME AND SETTING:A controlled,observational study utilizing in vitro neuroelectrophysiology was performed at the Department of Physiology in Southern Medical University between September and December in 2007.MATERIALS:Nikethamide was purchased from Sigma,USA;BL-420E biological signal collection and management system was provided by Chengdu TME Technology,China.METHODS:Isolated medulla-spinal cord preparations were collected from neonatal Sprague Dawley rats,aged 1-3 days.Tissues were divided to include the medial region of the nucleus retrofacialis,ventral respiratory,and dorsal respiratory groups.Subsequently,modified Kreb's solution and 5 μg/mL nikethamide-containing modified Kreb's solution were consecutively perfused into the medial region of the nucleus retrofacialis in neonatal rat brain slices.MAIN OUTCOME MEASURES:Hypoglossal nerve root respiratory-related rhythmic discharge activities and inspiratory neuron discharges were recorded with an adsorption electrode and microelectrode.RESULTS:Nikethamide resulted in prolonged inspiratory neuron discharge time,shortened respiratory cycle and expiratory time.Nikethamide intervention resulted in enhanced integral amplitude of some inspiratory neurons with no changes in discharge frequency or increased discharge frequency in remaining inspiratory neurons with no changes in integral amplitude.CONCLUSION:Nikethamide excites inspiratory neurons in the basic rhythmic respiration and medullary respiratory center,in addition to increased inspiratory neuron and neural network excitability. | Zhibin Qian Mingli Ji Zhonghai Wu | 2010 | Neural Regeneration Research2010，5，4： | 2 |
| 12 | Initial Rifting Age of the Nearly N–S Rifts in Southern Tibetan Plateau:New Evidence from the Age limit of the Early Sediments显示文摘Objective The nearly parallel N–S-trending rifts in southern Tibet represent the E–W extension of the Tibet Plateau.Most data which constrained the age of the extensional deformation come from isotopic dating of the dikes probably related to the activity of the nearly N–S faulting and micas from hydrothermal activity and the lowtemperature thermochronology of plateau uplift. | HA Guanghao WU Zhonghai HE Lin WANG Shubing | 2017 | Acta Geologica Sinica(English Edition)2017，91，2： | 2 |
| 13 | Effect of Low-Level Prenatal Mercury Exposure on Neonate Neurobehavioral Development in China 显示文摘 | Jinhua Wu Tinger Ying Zhonghai Shen | 2014 | Pediatric Neurology2014，51，1： | 1 |
| 14 | High photoelectrochemical water splitting performance on nitrogen doped double-wall TiO 2 nanotube array electrodes显示文摘 | Hongjun Wu Zhonghai Zhang | 2011 | International Journal of Hydrogen Energy2011，，21： | 1 |
| 15 | Photoelectrochemical water splitting and simultaneous photoelectrocatalytic degradation of organic pollutant on highly smooth and ordered TiO 2 nanotube arrays显示文摘 | Hongjun Wu Zhonghai Zhang | 2011 | Journal of Solid State Chemistry2011，，12： | 1 |
| 16 | Photoelectrochemical water splitting and simultaneous photoelectrocatalytic degradation of organic pollutant on highly smooth and ordered TiO2 nanotube arrays显示文摘 | Hongjun Wu Zhonghai Zhang | | 0，，12： | 1 |
| 17 | Identification and characterization of a novel peptide ligand of epidermal growth factor receptor for targeted delivery of therapeutics显示文摘 | LI Zhonghai ZHAO Ruijiao WU Xianghua | 2005 | Faseb J2005，19，14： | 1 |
| 18 | Photoelectrochemical water splitting and simultaneous photoelectrocatalytic degradation of organic pollutant on highly smooth and ordered TiO2 nano?tube arrays显示文摘 | WU Hongjun ZHANG Zhonghai | 2011 | Journal of Solid State Chemistry2011，184，2： | 1 |
| 19 | On the generation and pruning of skeletons using generalized Voronoi diagrams显示文摘 | Liu Hongzhi Wu Zhonghai Frank H | 2012 | Pattern Recognition Letters2012，33，16： | 1 |
| 20 | Optimization of total fla- vonoids extraction from mulberry leaf using an ethanol - based solvent system 显示文摘 | KAI NIE ZHONGHAI TANG XU WU | 2012 | Journal of Medicinal Plants Research2012，6，12： | 1 |
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