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本文讨论了韦特尔茄尔斯地区海克拉霍克岩系褶皱构造的特征:早期是一系列不同级别的平卧褶皱,并伴生有轴面片理S_1;晚期褶皱表现为不同时代、不同方向、不同类型的叠加褶皱,轴面近直立,有时伴有轴面劈理。叠加褶皱的类型有共轴和横轴重褶构造、两类不同横跨构造和被限制构造。该区经历了六个构造形变期,以相当于主加里东期的第二期(D_2)与喜马拉雅期的第五期(D_5)形变期最为重要。所有的构造形变均与基底断裂,尤其是与西侧滨外的斯匹茨卑尔根断裂带的活动有关。
This paper discusses the characteristics of the fold-forming structure of the Heklahooke series in the Wertel region: the early stage is a series of supine folds with different levels and associated with axial S 1; the late folds are characterized by different ages, different directions and different Type of superimposed folds, nearly vertical shaft surface, sometimes accompanied by axial cleavage. Types of overlying folds include coaxial and horizontal axis fold structures, two types of different span structures and restricted structures. The area underwent six tectonic deformation periods, most importantly equivalent to the second phase of the main Caledonian period (D_2) and the fifth (D_5) phase of the Himalayan period. All tectonic deformation is related to the rupture of the basement, especially to the Spitzer Bergen fault zone on the west side.