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1)  klippe [klip]
飞来峰
1.
The large-scale gliding-type klippe system in Longmen Mountains and neotectonic activity of the Longmen Orogen;
龙门山巨型滑覆型飞来峰体系与龙门山构造活动性
2.
Structural deformation and genetic mechanism of the Qingping klippe in central Longmen Mountains;
龙门山中段清平飞来峰的构造变形特征及形成机制
2)  klippen
飞来峰
1.
According to the internal structural features and the mechanical origin, this paper devides the klippen in Peng County into two kinds:thruSt nappe and gliding nappe.
彭县地区飞来峰根据其内部构造特征和力学成因可分为两类──推覆体和滑覆体。
2.
Along the low-angle overthrust Early Permian marble and Early Triassic sandy slate were thrust southward over Paleocene-Eocene purplish red conglomerate of the Paleocene-Eocene Fenghuoshan Group and brick-red sandy conglomerate of the Oligocene Yaxicuo Group, forming many klippen of varying scales, and thick fault brecci.
沿低角度逆冲断层,早二叠世大理岩和早三叠世砂板岩自北向南逆冲推覆于古新统—始新统风火山群紫红色砾岩和渐新世砖红色砂砾岩之上,形成大量不同规模的飞来峰;沿主逆冲断层发育厚层断层角砾岩与断层泥,局部形成碳酸盐质糜棱岩。
3)  thrust outlier
飞来峰群
1.
The nappe structures in this area are generally overthrusted and stacked by a number of slices and sheets, with thrust outliers in the front of the nappe structures.
锦屏山地区推覆构造带滑移面均为韧性剪切带 ,而且整个推覆构造带由多个岩片推覆堆叠在一起 ,在其前缘则出现飞来峰群。
4)  Feilɑifeng shike
飞来峰石刻
5)  Feilaifeng Cliffside Sculptures
飞来峰造像
6)  Baishi Goujia Klippe
白石-苟家飞来峰
1.
The Ganxi Formation sections are described in detail in the Baishi Goujia Klippe.
详细描述了白石-苟家飞来峰内甘溪组地层剖面,首次在汶川水磨及崇州九龙沟发现有甘溪组分布,建立了甘溪组的地层层序,讨论了岩性组合特征及基本层序类型,并进行了层序地层初探。
补充资料:飞来峰
【飞来峰】
 (地名)在浙江杭县灵隐山东南。舆地志曰:晋时西僧慧理登此。叹曰:此是中天竺国灵鹫山之小岭,不知何年飞来,因号其峰曰飞来。亦名灵鹫峰。
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