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1)  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。
2)  Feilɑifeng shike
飞来峰石刻
3)  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
4)  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。
5)  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。
6)  Feilaifeng Cliffside Sculptures
飞来峰造像
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