Search Results - "Feng, Shaoying"

SINOPROBE deep reflection profile reveals a Neo-Proterozoic subduction zone beneath Sichuan Basin by Gao, Rui, Chen, Chen, Wang, Haiyan, Lu, Zhanwu, Brown, Larry, Dong, Shuwen, Feng, Shaoying, Li, Qiusheng, Li, Wenhui, Wen, Zhongping, Li, Feng

“…A new multichannel seismic reflection profile collected across the Sichuan Basin in southern China by SINOPROBE images prominent reflectors that originate…”
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Lithospheric structure and faulting characteristics of the Helan Mountains and Yinchuan Basin： Results of deep seismic reflection profiling by Liu, BaoJin, Feng, ShaoYing, Ji, JiFa, Wang, ShuaiJun, Zhang, JianShi, Yuan, HongKe, Yang, GuoJun

“…The Helan Mountains and Yinchuan Basin （HM-YB） are located at the northern end of the North-South tectonic belt, and form an intraplate tectonic deformation…”
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Crustal Structure of the Chuan‐Dian Block Revealed by Deep Seismic Sounding and its Implications for the Outward Expansion of the East Tibetan Plateau by XIONG, Xiaosong, WANG, Guan, LI, Qiusheng, LU, Zhanwu, GAO, Rui, FENG, Shaoying, WU, Guowei

“…The Chuan‐Dian Block (CDB) is located in the southeastern margin of the Tibetan Plateau, with a complex geological structure and active regional faults. The…”
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The crustal structures of the central Longmenshan along and its margins as related to the seismotectonics of the 2008 Wenchuan Earthquake by Jia, ShiXu, Liu, BaoJin, Xu, ZhaoFan, Liu, Zhi, Feng, ShaoYing, Zhang, JianShi, Lin, JieYan, Tian, XiaoFeng, Liu, QiaoXia, Guo, WenBin

“…In 2010, a 500-km-long wide-angle reflection/refraction seismic profile was completed, running northwest from the central Sichuan Basin. This profile…”
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High-resolution crustal structure of the Yinchuan basin revealed by deep seismic reflection profiling： implications for deep processes of basin by Huang, Xingfu, Feng, Shaoying, Gao, Rui, Li, Wenhui

“…The Yinchuan basin, located on the western margin of the Ordos block, has the characteristics of an active continental rift. A NW-striking deep seismic…”
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Structural Characteristics of the Basement beneath Qiangtang Basin in Qinghai-Tibet Plateau： Results of Interaction Interpretation from Seismic Reflection/Refraction Data by Qiusheng, LI, Rui, GAO, Shaoying, FENG, Zhanwu, LU, Hesheng, HOU, Ye, GUAN, Pengwu, LI, Haiyan, WANG, Zhuo, YE, Xiaosong, XIONG, Jinkai, LIU, Rizheng, HE

“…The studies on configuration, character/property of the basement of Qiangtang basin is helpful for evaluating petroleum and nature gas resources as well as…”
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Novel nasolacrimal dacryocystorhinostomy combined with fluticasone propionate for the treatment of chronic dacryocystitis by Qin Mu, Dai Zhenhua, Feng Shaoying, Lei Shiqi, Lei Guanxiong, Yi Jiasheng

“…AIM: To investigate the effect of a new type of rhinodacryocystostomy combined with fluticasone propionate on patients with chronic dacryocystitis.METHODS: A…”
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Sedimentary and tectonic evolution of the Banquan pull-apart basin and implications for late Cenozoic dextral strike-slip movement of the Tanlu Fault Zone by Shu, Peng, Xu, Xiwei, Feng, Shaoying, Liu, Baojin, Li, Kang, Tapponnier, Paul, Deng, Xiaojuan, Chen, Guihua, Xia, Nuan, Xu, Hongtai, Qin, Jingjing, He, Fubing, Ma, Yan, Zheng, Rongzhang

“…The Banquan Basin is a pull-apart basin with the largest scale and the most prominent structure due to dextral slip of the Tanlu Fault Zone (TLFZ) in late…”
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Detailed structure of the lithosphere and deep dynamics beneath the Three River belt and western edge of the Yangtze craton by LI, Qiusheng, FENG, Shaoying, BAI, Zhiming, GAO, Yuan, GAO, Song, XIONG, Xiaosong, WANG, Xiaoran

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Deep crustal deformation of the Longmen Shan, eastern margin of the Tibetan Plateau, from seismic reflection and Finite Element modeling by Feng, Shao‐ying, Zhang, Pei‐zhen, Liu, Bao‐jin, Wang, Ming, Zhu, Shou‐biao, Ran, Yong‐kan, Wang, Wei‐tao, Zhang, Zhu‐qi, Zheng, Wen‐jun, Zheng, De‐wen, Zhang, Hui‐ping, Tian, Xiao‐feng

“…Rivaling the Himalaya in relief, the Longmen Shan is probably one of the most enigmatic mountain ranges in the world: high mountains reach more than 4000 m…”
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