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| 1 | Active tectonic blocks and strong earthquakes in the continent of China显示文摘The primary pattern of the late Cenozoic to the present tectonic deformation of China is characterized by relative movements and interactions of tectonic blocks. Active tectonic blocks are geological units that have been separated from each other by active tectonic zones. Boundaries between blocks are the highest gradient of differential movement. Most of tectonic activity occurs on boundaries of the blocks. Earthquakes are results of abrupt releases of accumulated strain energy that reaches the threshold of strength of the earth's crust. Boundaries of tectonic blocks are the locations of most discontinuous deformation and highest gradient of stress accumulation, thus are the most likely places for strain energy accumulation and releases, and in turn, devastating earthquakes. Almost all earthquakes of magnitude greater than 8 and 80%-90% of earthquakes of magnitude over 7 occur along boundaries of active tectonic blocks. This fact indicates that differential movements and interactions of active tectonic blocks are the primary mechanism for the occurrences of devastating earthquakes. | ZHANG Peizhen (张培震) DENG Qidong (邓起东) ZHANG Guomin (张国民) MA Jin (马 瑾) GAN Weijun (甘卫军) MIN Wei (闵 伟) MAO Fengying (毛凤英) WANG Qi (王 琪) | 2003 | Science China Earth Sciences2003，46，z2： | 239 |
| 2 | Paleoearthquake rupture behavior and recurrence of great earthquakes along the Haiyuan fault, northwestern China显示文摘The Haiyuan fault is a major seismogenic fault in north-central China where the 1920 Haiyuan earthquake of magnitude 8.5 occurred, resulting in more than 220000 deaths. The fault zone can be divided into three segments based on their geometric patterns and associated geomorphology. To study paleoseismology and recurrent history of devastating earthquakes along the fault, we dug 17 trenches along different segments of the fault zone. Although only 10 of them allow the paleoearthquake event to be dated, together with the 8 trenches dug previously they still provide adequate information that enables us to capture major paleoearthquakes oc- curring along the fault during the past geological time. We discovered 3 events along the eastern segment during the past 14000 a, 7 events along the middle segment during the past 9000 a, and 6 events along the western segment during the past 10000 a. These events clearly depict two temporal clusters. The first cluster occurs from 4600 to 6400 a, and the second occurs from 1000 to 2800 a, approximately. Each cluster lasts about 2000 a. Time period between these two clus- ters is also about 2000 a. Based on fault geometry, segmentation pattern, and paleoearthquake events along the Haiyuan fault we can identify three scales of earthquake rupture: rupture of one segment, cascade rupture of two segments, and cascade rupture of entire fault (three segments). Interactions of slip patches on the surface of the fault may cause rupture on one patch or ruptures of more than two to three patchs to form the complex patterns of cascade rupture events. | ZHANG Peizhen MIN Wei DENG Qidong MAO Fengying | 2005 | Science China Earth Sciences2005，48，3： | 31 |
| 3 | Colluvial wedges associated with pre-historical reverse faulting paleoearthquakes显示文摘Colluvial wedges collapsed from fault scarp can also be used to study reverse faulting paleoearthquakes. Generating processes of reverse faulting colluvial wedges are much more complex than those associated with normal faulting earthquakes. Reverse faulting colluvial wedge is also in triangle shape, and dies away from the fault. Contact between the fault and the colluvial wedge may be a simple straight reverse fault or a combination of an erosive surface in the upper part and a reverse fault in the lower part. Contents and grain sizes increase near the fault and along the base of a colluvial wedge. Based on examples from the piedmont reverse fault and fold along the northern Tainshan, we studied characteristics of reverse faulting colluvial wedges, and discussed the generating processes of reverse faulting colluvial wedges. Reverse faulting generates an unstable scarp hanging in the air immediately after an earthquake. Fallen material deposits along the base of newly formed fault scarp. Erosive | Qidong Deng Peizhen Zhang | 2000 | Chinese Science Bulletin2000，45，17： | 6 |
| 4 | γ-LiA1O2 Single Crystal: a Novel Substrate for GaN Epitaxy 显示文摘 | Xu Ke XuJun Deng Peizhen | 1998 | Journal of Crystal Growth1998，193，： | 1 |
| 5 | γ-LiAlO2 Single Crystal: a Novel Substrate for GaN Epitaxy 显示文摘 | Xu Ke Xu Jun Deng Peizhen Zhou Yongzong Zhou Guoqing Qiu Rongsheng Fang Zujie | 1998 | Journal of Crystal Growth1998，193，： | 1 |
| 6 | Temperature dependent emission cross-section and fluorescence lifetime of Cr,Yb:YAG crystals显示文摘 | Jun Dong Peizhen Deng | 2003 | Journal of Physics and Chemistry of Solids2003，，7： | 1 |
| 7 | Growth of Large-sized Sapphire Boules by Temperature Gradient Technique (TGT)显示文摘 | Xu Jianwei Zhou Yongzong Zhou Guoqing Xu Ke Deng Peizhen Xu Jun | 1998 | Journal of Crystal Growth1998，193，： | 1 |
| 8 | 显示文摘 | Jiang Chun Deng Peizhen Zhang Junzhou | 1999 | Journal of Luminescence1999，82，4： | 1 |
| 9 | High Efficient Laer Operation of the High-Doped Nd:YAG Crystal Grawn by Temperature Gradient Technology显示文摘 | Mao Yanli Deng Peizhen Zhang Yinghua | | 0，，： | 1 |
| 10 | Perfection and Laser Performances of Nd:YAG Crystals Grown by TGT显示文摘 | Deng Peizhen Qiao Jingwen Hu Bing | 1988 | Journal of Crystal Growth1988，92，： | 1 |
| 11 | Crystal growth and spectral properties of Yb 3 Al 5 O 12显示文摘 | Xiaodong Xu Zhiwei Zhao Jun Xu Peizhen Deng | 2003 | Journal of Crystal Growth2003，，3： | 1 |
| 12 | γ-LiAlO2 Single Crystal: a Novel Substrate for GaN Epitaxy 显示文摘 | Xu Ke Xu Jun Deng Peizhen Zhou Yongzong Zhou Guoqing Qiu Rongsheng Fang Zujie | 1998 | Journal of Crystal Growth1998，193，： | 1 |
| 13 | Active reverse fault-fold zones and earthquakes along northern Tianshan, Xinjiang, China显示文摘 | DENG Qidong FENG Xianyue ZHANG Peizhen | 1996 | Seismology and Geology1996，，： | 1 |
| 14 | Structure and deformational character of strike-slip fault zones显示文摘 | Qidong Deng Daning Wu Peizhen Zhang Shefa Chen | 1986 | Pure and Applied Geophysics PAGEOPH (-)1986，，1： | 1 |
| 15 | Concentration quenching in Yb: YAG显示文摘 | YANG Peizhi DENG Peizhen | 2002 | Journal of Luminescence2002，97，： | 1 |
| 16 | Active reverse fault-fold zones and earthquakes along northem Tianshan, Xinjiang, China显示文摘 | DENG Qidong FANG Xianyue ZHANG Peizhen | 1996 | Seismology and Geology1996，，： | 1 |
| 17 | Basic characteristics of active tectonics in China 显示文摘 | Deng Qidong Zhang Peizhen | 2002 | Science in China ( Series D)2002，32，12： | 1 |
| 18 | γ-LiAlO2 Single Crystal: A Novel Substrate for GaN Epitaxy 显示文摘 | Xu Ke Xu Jun Deng Peizhen | 1998 | Journal of Crystal Growth1998，193，： | 1 |
| 19 | Laser-diode-pumped Cr4+,Nd3+∶YAG with self-Q-swithced laser output of 14 W显示文摘 | Jun Dong Peizhen Deng Yutian Lu | | 0，，： | 1 |
| 20 | Study of the effects of Cr ions on Yb in Cr,Yb:YAG crystal 显示文摘 | Dong Jun Deng Peizhen Xu Zhen | 1999 | Optics Communications1999，170，： | 1 |
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