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| 1 | Structures of the Bohai Petroliferous Area,Bohai Bay Basin显示文摘This paper, for the first time, deals with a more systematic study of the structures in the Bohaipetroliferous area that covers nearly one third of the Bohai Bay basin. The study mainly involves the effects of preexisting basement faults on the basin formation, the characteristics of basin geometry and kinetics, the modelling of the tectonic-thermal history, the polycyclicity and heterogeneity in the structural evolution and the natural seismic tomographic images of the crust and upper mantle. The authors analyze the features of the dynamic evolution of the basin in the paper and point out that the basin in the Bohai petroliferous area is an extensional pull-apart basin. | CAI Dongsheng LUO Yuhui YAO Changhua HE Jiankun HU Shengbiao LU Huafu WANG Liangshu | 2000 | Acta Geologica Sinica(English Edition)2000，74，3： | 8 |
| 2 | Altered relationship between thickness and intrinsic activity amplitude in generalized tonic–clonic seizures显示文摘A thinner cortex has higher potential for binding GABA receptor A which is associated with larger amplitudes of intrinsic brain activity(i BA). However, the relationship between cortical thickness and i BA is unknown in intact and epileptic brains. To this end, we investigated the relationship between cortical thickness measured by highresolution MRI and surface-based i BA derived from resting-state functional MRI in normal controls(n = 82) andpatients with generalized tonic–clonic seizures(GTCS)only(n = 82). We demonstrated that the spatial distribution of cortical thickness negatively correlated with surface-based i BA amplitude at both whole-brain and within independent brain functional networks. In GTCS patients,spatial coupling between thickness and i BA amplitude decreased in the default mode, dorsal attention, and somatomotor networks. In addition, the vertex-wise acrosssubject thickness–i BA amplitude correspondence altered in the frontal and temporal lobes as well as in the precuneus in GTCS patients. The relationship between these two modalities can serve as a brain-based marker for detecting epileptogenic changes. | Wei Liao Jue Wang Ting Xu Zhiqiang Zhang Gong-Jun Ji Qiang Xu Zhengge Wang Fang Yang Xi-Nian Zuo Anqi Qiu Yu-Feng Zang Guangming Lu Huafu Chen | 2016 | Science Bulletin2016，61，24： | 3 |
| 3 | Operation of the CSNS Penning surface H^- ion source显示文摘The accelerator complex of the China Spallation Neutron Source (CSNS) consists of a H- linear accelerator (linac) and a rapid cycling synchrotron (RCS). The linac contains a Penning surface H- ion source. The designed energy and the beam current of the source are 50 keV and 20 mA respectively, with a normalized root mean square (norm. rms.) emittance of 0.2π mm mrad. The manufactures and tests of the discharge chamber are in great progress. The construction of H- ion source test stand has been completed, and the operation of the source is also in progress. Stable H- ion beams with energy of 50 keV and current up to 50 mA are attained. Emittance measurement for the H- beam is being prepared. | WU XiaoBing OUYANG HuaFu CHI YunLong HE Wei HUANG Tao LI Gang LIU YingMan LU YanHua XU TaoGuang ZHANG JunSong ZHANG HuaShun ZHAO FuXiang | 2011 | Science China(Physics,Mechanics & Astronomy)2011，54，S2： | 2 |
| 4 | The synchronization of spontaneous BOLD activity predicts extraversion and neuroticism显示文摘 | Luqing Wei Xujun Duan Yang Yang Wei Liao Qing Gao Ju-rong Ding Zhiqiang Zhang Weixi Zeng Yuan Li Guangming Lu Huafu Chen | 2011 | Brain Research2011，，： | 2 |
| 5 | Closing history of the southern Tianshan oceanic basin, western China: an oblique collisional orogen显示文摘 | Chen Chuming Lu Huafu Jia Dong | 1999 | Tectonophysics1999，302，： | 1 |
| 6 | Structural Features of Northem Tarim Basin:Implications for regional Tectonics and Petroleum Traps显示文摘 | Jia Dong Lu Huafu Cai Dongsheng | 1998 | AAPG Bulletin1998，，： | 1 |
| 7 | Growth of the Huoerguosi anticline (north Tianshan Mountains) by limb rotation since the late Miocene显示文摘Huoerguosi 背斜,在北方 Tianshan 山山麓 fold-and-thrust 带定位了,是 trending 东方西方差错相关的褶层。在沿着 Jingou 河的生气的节,它的南方手足由 Anjihaihe 的生长前阶层组成( E ( 2-3 )一), Shawan (( E-3-N-1 ) s ), Taxihe ( N ( 1 ) t )和 Dushanzi ( N ( 2 ) d )的更低的部分形成, trending 东方西方并且蘸到南方 55 学位,并且 Dushanzi ( N ( 2 ) d )和 Xiyu 的上面的部分的生长阶层(( N-2-Q ( 1 )) x )形成,哪个在 Xiyu 的底部在生长阶层的底从 55 个学位减少到 47 个学位的剧降(( N-2-Q ( 1 )) x )形成到类似于在 Xiyu 的顶的 0 个学位(( N-2-Q ( 1 )) x )形成。在背斜的北方手足的阶层垂直或打翻,并且被突破戳切导致 drag 褶层。深入地,背斜是对称的,并且它的核心包括白垩纪和侏罗记忍受煤的床。在地震侧面,在背斜的南方手足的生长前阶层的地震反射镜常常蘸到南方,并且生长阶层之一扇向南方,谁的向上蘸减少。沿着 Jingou 河山谷和在地震侧面显示出的背斜的深结构的南方手足生长阶层 outcropped 的几何学显示 Huoerguosi 背斜是由手足旋转成长的分开褶层背斜。基于生长模型和 magnetostratigraphic 年龄,在 Huoerguosi 背斜的成长过程期间,南方手足吸收的平均弄短率类似于 0.46 mm/a ,和背斜的平均高举率类似于超过平均免职率的 0.86 mm/a ,它根据背斜的顶强烈地被侵蚀的事实。考虑 Huoerguosi 背斜的对称的几何学并且忽略突破推进,整个背斜弄短应该非常类似于 0.92 mm/a,加倍在南方手足从生长决定的弄短的率。 | WANG ShengLi CHEN Yan LU HuaFu | 2008 | Chinese Science Bulletin2008，53，19： | 1 |
| 8 | Structural development of the Lower Paleozoic belt of South China: Genesis of an intracontinental orogen显示文摘 | Jacques Charvet Liangshu Shu Michel Faure Flavien Choulet Bo Wang Huafu Lu Nicole Le Breton | 2010 | Journal of Asian Earth Sciences2010，，4： | 1 |
| 9 | Closing history of the southern 7ianshan oceanic basin, western China: an oblique collisional orogeny显示文摘 | Chen Chuming Lu Huafu Dong Jia | 1999 | Tectonophysics1999，302，： | 1 |
| 10 | Structural Features of Northern Tarim Basin:Implications for Regional Tectonics and PetroleumTraps显示文摘 | Dong Jia Huafu Lu Dongsheng Cai | 1998 | AAPG Bulletin1998，82，1： | 1 |
| 11 | Structural Features of Northern Tarim Basin: Implications for Regional Tectonics and Petroleum Traps: Reply显示文摘 | Dong Jia Huafu Lu Chengzao Jia | 1999 | AAPG Bulletin1999，83，8： | 1 |
| 12 | Structural features of northern Tarim Basin: implications for regional tectonics and petroleum traps显示文摘 | Jia Dong Lu Huafu Cai Dongsheng | 1998 | AAPG Bulletin1998，82，1： | 1 |
| 13 | Structure Features of Northern Tarim Basin: Implications for Regional Tectonics and PetroleumTraps显示文摘 | Dong Jia Huafu Lu Dongsheng Cai | 1998 | AAPG Bulletin1998，82，1： | 1 |
| 14 | Rejuvenation of the Kuqa foreland basin, north flank of the Tarim Basin, Northwest China显示文摘 | Lu Huafu David G Howell Jia Dong | 1994 | International Geology Review1994，36，： | 1 |
| 15 | Closing history of the southern Tianshan oceanic basin, western China: An oblique collisional orogeny显示文摘 | Chen Chunming Lu Huafu Jia Dong | 1999 | Tectonophysics1999，302，12： | 1 |
| 16 | Tectonic character and deformation time in Cenozoic Kuqa Basin显示文摘 | LU Huafu JIA Dong CHEN Chuming | 1999 | Earth Science Frontiers1999，6，4： | 1 |
| 17 | Rejuvenation of the Kuqa foreland basin,north flank of the Tarim Basin,Northwest China显示文摘 | Lu Huafu Howell D G Jia Dong | 1994 | International Geology Review1994，36，12： | 1 |
| 18 | Changing stress field in the middle segment of the Tan--Lu fault zone, Eastern China 显示文摘 | Lu Huafu Yu Hongnian Ding Youwen | 1983 | Tectonophysics1983，98，： | 1 |
| 19 | Evidence and dynamics for the change of the strike-slip direction of the Changle-Nan'ao ductile shear zone,Southeastern China显示文摘 | Wang Zhihong Lu Huafu | 1997 | Journal of Asian Earth Sciences1997，15，6： | 1 |
| 20 | Paleozoic accretionary terranes in Northern Tianshan,NW China显示文摘 | Shu Liangshu Chen Yuntang Lu Huafu | 2000 | Chinese Geochemistry2000，19，3： | 1 |
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