标题:Orogenic Movements during the Paleozoic Period: Development of the Granitoid Formations in the Northwestern Region of Spain’s Iberian Peninsula
作者:Romaní J.R.V.; Song Z.; Liu H.; Sun Y.; Li H.
作者机构:[Romaní, J.R.V] College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, 266590, China, University Institute 更多
通讯作者:Romaní, JRV(juan.vidal.romani@udc.es)
通讯作者地址:[Romaní, J.R.V] College of Earth Science and Engineering, Shandong University of Science and TechnologyChina;
来源:Journal of Earth Science
出版年:2020
DOI:10.1007/s12583-019-1268-z
关键词:endogenous forms; exogenous forms; geomorphology; granitoid; intrusive structures
摘要: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. © 2020, China University of Geosciences and Springer-Verlag GmbH Germany, Part of Springer Nature.
收录类别:SCOPUS
资源类型:期刊论文
原文链接:https://www.scopus.com/inward/record.uri?eid=2-s2.0-85077711314&doi=10.1007%2fs12583-019-1268-z&partnerID=40&md5=e8d38eae7fb0ef25d71fd60402d29a37
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