构造学和引力现象(斯洛文尼亚纳诺斯)

Q3 Earth and Planetary Sciences
L. Placer, A. Mihevc, I. Rižnar
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引用次数: 1

摘要

伊斯特拉推进区是外二元系西北部的一个特殊变形地区。它的形成是由于中新世中期以来,作为亚得里亚海微板块(Adria)一部分的Istra地块向Dinarides运动。Istra地块的运动导致了沿着旧位错的遗传位移,这些位错可以追溯到始新世末形成二元系的早期形成阶段及其变形。这些变形也反映在外Dinaric叠瓦带和外Dinaris逆冲带边界沿线的某些极端重力现象中,中生代碳酸盐岩被推压在新生代复理石上。这两条带之间的边界带连接着特诺沃、赫鲁希察和斯涅日尼克冲断层前缘。这里介绍了在这个边界带发生的四种特殊引力现象,因为它们的大小是显著的:Črna griža(Trnovo Nappe)、Suhi vrh(Hrušica Nappe。这里详细描述了苏海的现象。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tectonics and gravitational phenomena (Nanos, Slovenia)
The Istra Pushed Area is a specifically deformed territory of the northwestern part of the External Dinarides. It formed due to the movement of the Istra block as part of the Adriatic Microplate (Adria) towards the Dinarides since the middle Miocene. The movement of the Istra block caused hereditary shifts along the old dislocations dating back to the early formation stage of the formation of the Dinarides at the end of the Eocene and their deformation. These deformations are reflected also in certain extreme gravitational phenomena along the boundary between the External Dinaric Imbricated Belt and the External Dinaric Thrust Belt, where Mesozoic carbonates are thrusted upon the Cenozoic flysch. The boundary zone between these two belts connects the Trnovo, Hrušica and Snežnik Thrust Fronts. Four specific gravitational phenomena that occurred in this boundary zone are presented here, as they are remarkable in terms of their size: Črna griža (Trnovo Nappe), Suhi vrh (Hrušica Nappe), Petelinje mlake and Ilirska Bistrica (both from the Snežnik Nappe). The phenomena at Suhi vrh is described in detail herein.
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来源期刊
Geologija
Geologija Earth and Planetary Sciences-Geophysics
CiteScore
1.00
自引率
0.00%
发文量
10
审稿时长
10 weeks
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