Orogenic Movements during the Paleozoic Period: Development of the Granitoid Formations in the Northwestern Region of Spain's Iberian Peninsula

Juan Ramon Vidal Romaní; Zhaojun Song; Huimin Liu; Yifang Sun; Haonan Li

doi:10.1007/s12583-019-1268-z

Volume 31 Issue 3

Jul 2020

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Journal of Earth Science > 2020 > 31(3): 611-620.

Juan Ramon Vidal Romaní, Zhaojun Song, Huimin Liu, Yifang Sun, Haonan Li. Orogenic Movements during the Paleozoic Period: Development of the Granitoid Formations in the Northwestern Region of Spain's Iberian Peninsula. Journal of Earth Science, 2020, 31(3): 611-620. doi: 10.1007/s12583-019-1268-z

Citation:

Juan Ramon Vidal Romaní, Zhaojun Song, Huimin Liu, Yifang Sun, Haonan Li. Orogenic Movements during the Paleozoic Period: Development of the Granitoid Formations in the Northwestern Region of Spain's Iberian Peninsula. Journal of Earth Science, 2020, 31(3): 611-620. doi: 10.1007/s12583-019-1268-z

Citation:

Juan Ramon Vidal Romaní, Zhaojun Song, Huimin Liu, Yifang Sun, Haonan Li. Orogenic Movements during the Paleozoic Period: Development of the Granitoid Formations in the Northwestern Region of Spain's Iberian Peninsula. Journal of Earth Science, 2020, 31(3): 611-620. doi: 10.1007/s12583-019-1268-z

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Orogenic Movements during the Paleozoic Period: Development of the Granitoid Formations in the Northwestern Region of Spain's Iberian Peninsula

doi: 10.1007/s12583-019-1268-z

Juan Ramon Vidal Romaní^{1, 2
,
,
,},
Zhaojun Song^{1, 3
,
,
,},
Huimin Liu¹,
Yifang Sun¹,
Haonan Li¹

1.
College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
2.
University Institute of Geology, University of Corunna, Galicia 15071, Spain
3.
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China

More Information

Corresponding author: Juan Ramon Vidal Romaní, ORCID:0000-0001-7158-4945, juan.vidal.romani@udc.es; Zhaojun Song, ORCID:0000-0001-6516-2818, songzhaojun76@163.com
Received Date: 25 Sep 2019
Accepted Date: 06 Nov 2019
Publish Date: 01 Mar 2020

Abstract

Abstract

In the present study, Paleozoic Variscan orogenesis was a model of the oroclinal flexion accompanied by extensive magmatism, which could be divided into the following two types:post-tectonic and syn-tectonic tonalite granite, and leuco-granite which were controlled by the tectonic characteristics of the intrusions. It was observed that a very high majority of the samples had displayed discontinuities in their structures, that were later utilized to define the granitoid morphology and development characteristics of the rock during the intrusion phases. Furthermore, it was determined that the tectonics associated with the Alpine orogeny results in the new generation of faults and fractures during the Paleogene Period had produced the development of the Sierras. Due to different weathering processes, the depressions which had resulted in the present granitoid reliefs were found to be exclusively related to the structural development processes during the geological history (either tectonic or magmatic) of the granite, and not as normally interpreted.
- granitoid,
- geomorphology,
- endogenous forms,
- exogenous forms,
- intrusive structures

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References(62)

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