Pre-Variscan palaeogeographical structures in the Cantabrian Zone, Spain: some critical considerations regarding their origin, location and significance

IF 0.9 Q3 GEOLOGY
G. V. van Loevezijn
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引用次数: 0

Abstract

Abstract An update of the main Devonian pre-Variscan palaeogeographical features of the southern Cantabrian Zone is presented. The approximal locations of these features are recorded in sections studied, with thin, incomplete developments for the highs and thick successions for the troughs. Generally, pre-Variscan palaeogeographical features were affected by Variscan and Alpine orogenic deformations, but with a different impact. Oroclinal bending, tectonic shortening by thrusts, movements along strike-slip faults and bending by folds all affected the Devonian palaeogeographical features, and only an approximation of their location and shape can be given. Nevertheless, the palaeogeography recorded in pre-Variscan sedimentary successions and their relative positions, provide specific, clear and objective evidence of the pre-Variscan elements.
西班牙坎塔布连地区前瓦里斯坎古地理构造:关于其起源、位置和意义的一些关键考虑
摘要对坎塔布里安带南部泥盆纪-华力西期前的主要古地理特征进行了更新。这些特征的近似位置记录在所研究的剖面中,高点的发育很薄,不完整,波谷的发育很厚。一般来说,前华力西期古地理特征受到华力西和阿尔卑斯造山变形的影响,但影响不同。造山带弯曲、逆冲构造缩短、走滑断层运动和褶皱弯曲都影响了泥盆纪的古地理特征,只能给出其位置和形状的近似值。然而,华力西前沉积序列中记录的古地理及其相对位置,为华力西期前元素提供了具体、清晰和客观的证据。
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来源期刊
Geologos
Geologos GEOLOGY-
CiteScore
1.70
自引率
0.00%
发文量
7
审稿时长
12 weeks
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