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昏途修远走西口,苦行求索信天游——乔建中老师中国艺术研究院音乐研究所主政岁月散纪
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作者 韩锺恩 《交响(西安音乐学院学报)》 2015年第1期13-18,共6页
乔建中总是眼光向下:屈家营、内蒙古大草原、苗瑶侗壮、中华乐舞……走西口、信天游,苦行在昏途,再修远亦求索,终于在田野里把土地的歌一首一首地采集回来整整齐齐地码放在永久的《四库全书》集部中间……看样子,这就是老乔的幸福——... 乔建中总是眼光向下:屈家营、内蒙古大草原、苗瑶侗壮、中华乐舞……走西口、信天游,苦行在昏途,再修远亦求索,终于在田野里把土地的歌一首一首地采集回来整整齐齐地码放在永久的《四库全书》集部中间……看样子,这就是老乔的幸福——托命学术,田野为本。因为他折返回来又回到了仅属于他存在自身并通过他自足成就的那个本体:无缘无故地有赖于土地,不由自主地唱着那动人的歌…… 展开更多
关键词 乔建中 中国艺术研究院音乐研究所 主政岁月 散纪
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Geometric Structure and Tectonic Activities of Wanquan Fault,Hebei Province
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作者 Zhou Jianglin You Huichuan +4 位作者 Zhou Yueling Shao Cuiru Yang Qiyan Li Jinjin Zhang Zhengyu 《Earthquake Research in China》 2013年第2期223-232,共10页
Based on detailed investigations and prospecting,this paper describes the geometrical characteristics and tectonic activities of Wanquan fault in northwest of Beijing. This fault strikes mainly northeast or northeast ... Based on detailed investigations and prospecting,this paper describes the geometrical characteristics and tectonic activities of Wanquan fault in northwest of Beijing. This fault strikes mainly northeast or northeast to north,dipping southeast,and extends over a length of 15km. It is a major geological and geomorphological margin,controlling the neotectonic movement in this region. On the southeast side of Wanquan fault are the Late Quaternary unconsolidated deposits,forming a basin or deposition; but on the other side is Mesozoic volcano debris,forming lower-mountains and hills. Wanquan fault is a mid- to-high-angle normal fault dipping southeast. This fault was more active in the Quaternary. Since the middle-late part of the alate Pleistocene,the average rate with vertical slip of a single fault is over 0. 03 ~ 0. 3mm /a,but the fault has multiple slipping surfaces,and a total rate with vertical slip will be estimated. 展开更多
关键词 Wanquan fault Geometric structure Tectonic activities
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Geological Evidence and Characteristics of Activity of the Wuhe-Mingguang Section of Tancheng-Lujiang Fault Zone in Late Pleistocene 被引量:2
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作者 Shu Peng Fang Lianghao +4 位作者 Zheng Yingping Lu Shuo Pan Haobo Song Fangmin Li Shengqiang 《Earthquake Research in China》 CSCD 2016年第4期485-499,共15页
As the most influential strike-slip fault in East China,the Tancheng-Lujiang fault zone draws scholars attention for its strong seismic activity. Nevertheless,most research has been conducted along segments in Shandon... As the most influential strike-slip fault in East China,the Tancheng-Lujiang fault zone draws scholars attention for its strong seismic activity. Nevertheless,most research has been conducted along segments in Shandong Province and Bohai Bay where huge earthquakes occur frequently. Meanwhile,it is generally believed that segments lying to the south of Huaihe River have been inactive since the late Quaternary and thus it is incapable of generating moderate or strong earthquakes. However,these understandings about the Tancheng-Lujiang fault have been questioned by our recent work for part of the fault south to the Huaihe River. Based on interpretation of high-resolution satellite images,detailed field investigations near Wuhe county and Mingguang City in northern Anhui Province and elaborate microstructure analysis, we come to the conclusion that the Tancheng-Lujiang fault zone mainly consists of four branches and at least one should be active since the late Pleistocene for the Wuhe-Mingguang section. This segment is monopolized by dextral strike-slip motion in late Quaternary. Different from obvious faults in bed rocks or consolidated sediments,the latest activity trace in Quaternary loose sediment revealed by trench excavation is not obvious or even invisible to visual observation. According to our recent work and previous studies, we call for more attention to be paid to invisible faults in young sediment and also suggest that more research be conducted along this seemingly placid segment. 展开更多
关键词 Tancheng-Lujiang fault zone South of Huaihe River Wuhe-Mingguang segment Microstructure Late Pleistocene
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