气候变化领域集成服务门户(CCPortal): Relationship between magnetic fabrics and deformation of the Miocene Pohorje intrusions and surrounding sediments (Eastern Alps)

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DOI	10.1007/s00531-020-01846-4
	Relationship between magnetic fabrics and deformation of the Miocene Pohorje intrusions and surrounding sediments (Eastern Alps)
	Fodor L.I.; Márton E.; Vrabec M.; Koroknai B.; Trajanova M.; Vrabec M.
发表日期	2020
ISSN	14373254
起始页码	1377
结束页码	1401
卷号	109 期号:4
英文摘要	The Miocene deformation history of magmatic and host metamorphic rocks and surrounding sediments was reconstructed by measuring meso- and microscale structures and anisotropy of magnetic susceptibility (AMS) data in order to constrain the structural evolution of the Pohorje pluton during the onset of lithospheric extension at the Eastern Alps–Pannonian Basin transition. Principal AMS axes, lineation and foliation are very similar to mesoscopic lineation and foliation data from the main intrusive body and from some dykes. Although contribution from syn-magmatic texture is possible, these structures were formed during the cooling of the pluton and associated subvolcanic dykes just shortly after the 18.64 Ma pluton intrusion. Dykes emplaced during progressively younger episodes reflect decreasing amount of ductile strain, while firstly mesoscopic foliation and lineation, and then the tectonic AMS signal gradually disappears. In the structurally highest N–S trending dacite dykes, the AMS fabric only reflects the magmatic flow. The Miocene sediments underwent the same, NE–SW to E–W extension as the magmatic and host metamorphic rocks as indicated by both AMS and fault-slip data. All these events occurred prior to ~ 15 Ma, i.e., during the main syn-rift extension of the Pannonian Basin and during the fastest exhumation of the Tauern and Rechnitz windows, both demonstrating considerable extension of diverse crustal segments of the Alpine nappe pile. After a counterclockwise rotation around ~ 15 Ma, the maximum stress axis changed to a SE–NW orientation, but it was only registered by brittle faulting. During this time, the overprinting of a syn-rift extensional AMS texture was not possible in the cooled or cemented magmatic, metamorphic and sedimentary rocks. © 2020, The Author(s).
英文关键词	Anisotropy of magnetic susceptibility; Dyke; Fault; Foliation; Lineation; Pluton
语种	英语
scopus关键词	deformation; dike; emplacement; igneous intrusion; magnetic anisotropy; magnetic fabric; Miocene; terrestrial deposit; Alps; Eastern Alps; Pohorje Mountains; Slovenia
来源期刊	International Journal of Earth Sciences
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/147673
作者单位	MTA-ELTE Geological, Geophysical and Space Science Research Group at Eötvös University, Pázmány P. sétány 1/C, Budapest, 1117, Hungary; Department of Physical and Applied Geology, Eötvös University, Pázmány P. sétány 1/C, Budapest, 1117, Hungary; Paleomagnetic Laboratory, Mining and Geological Survey of Hungary, Columbus 13 u. 17-23, Budapest, 1145, Hungary; FNSE, Department of Geology, University of Ljubljana, Aškerčeva 12, Ljubljana, 1000, Slovenia; Geomega Ltd., Zsil u. 1, Budapest, 1093, Hungary; Geological Survey of Slovenia, Dimičeva ulica 14, Ljubljana, 1000, Slovenia
推荐引用方式 GB/T 7714	Fodor L.I.,Márton E.,Vrabec M.,et al. Relationship between magnetic fabrics and deformation of the Miocene Pohorje intrusions and surrounding sediments (Eastern Alps)[J],2020,109(4).
APA	Fodor L.I.,Márton E.,Vrabec M.,Koroknai B.,Trajanova M.,&Vrabec M..(2020).Relationship between magnetic fabrics and deformation of the Miocene Pohorje intrusions and surrounding sediments (Eastern Alps).International Journal of Earth Sciences,109(4).
MLA	Fodor L.I.,et al."Relationship between magnetic fabrics and deformation of the Miocene Pohorje intrusions and surrounding sediments (Eastern Alps)".International Journal of Earth Sciences 109.4(2020).