Receive exclusive offers and updates from Oxford Academic. WikiProject Albums Album articles v t e. WikiProject Albums Album articles. It furthers the University's objective of excellence in research, scholarship, and education by publishing worldwide. This article has been rated as Stub-Class on the project's quality scale. Dacitoandesites, mostly situated west of the anticline, are considered as of Oligocene age, but older than the plutonic rocks.
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The Miocene granite has visible foliation, the I-type granodiorites and the dacitoandesites occasionally exhibit visibly oriented mineral fabric. In such cases, the fast and inexpensive magnetic susceptibility measurements can provide information about the degree and type of the orientation of the fabric.
The Vardar zone is the suture between colliding Adriatic and Eurasian plates, comprising profoundly different tectonostratigraphic units which came into contact during Early Palaeogene. Email alerts New issue alert. Views Read Edit New section View history. The granitoids, forming the core of the anticline and the satellite bodies intruded during Oligocene at the depth of 10 kmbut were exhumed during a mid-Miocene extensional D4 phase of deformation, simultaneously with the intrusion of S-type granite which crops out NW of the anticline.
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The magnetic fabrics of the dacitoandesites did not reflect deformation. By using this site, you drenim to the Terms of Use and Privacy Policy. I have just modified 2 external links on Brazde. Sign In or Create an Account.
Our aim was to find out if the loosely dated D3 and the well-dated D4 xrenik left imprint met the magnetic fabrics of the above-mentioned rocks by studying the magnetic susceptibility anisotropy of nearly independently oriented samples from 25 localities. A physics-based approach of deep interseismic creep for viscoelastic strike-slip earthquake cycle models.
Abstract The Vardar zone is the suture between colliding Adriatic and Eurasian plates, comprising profoundly different tectonostratigraphic units which came into contact during Early Palaeogene. Related articles in Google Scholar.
We found that the granodiorites often have high or extremely high degree of magnetic ddrenik, suggesting that it was acquired under the influence of stress in the last stage of solidification. In progress issue alert.
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Deep velocity image of the north Zagros collision nrt Iran from regional and teleseismic tomography. This article has not yet received a rating on the project's importance scale. Retrieved from " https: As of February"External links modified" talk page sections are no longer generated or monitored by InternetArchiveBot.
Latest Most Read Most Cited Spatio-temporal seismic velocity variations associated to the central Italy seismic sequence from noise cross-correlation.
The anticline is conceived as having been formed during compression D3 phase deenik deformation of post-Cretaceous ageprior to the intrusion of I-type granitoids or alternatively, the updoming of the regionally metamorphosed rocks was caused by the intrusion of the plutons.
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WikiProject Albums Album articles v t e. In the northern part of the Kopaonik pluton, and in the Drenje massif the pattern of the schistosity planes do not fit to the anticlinorium, neither seem to satisfy an onion-shell model put forward earlier for the Kopaonik pluton.
The reason may be that they cooled completely before the intrusion of the I-type granodiorites. From Wikipedia, the free encyclopedia.
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Citing articles via Google Scholar. Dacitoandesites, mostly situated west of the anticline, are considered as of Oligocene age, but older than the plutonic rocks. Please take a moment to review my edit. The zone was subsequently intruded by igneous rocks, concentrated at certain places, like the Kopaonik area, where plutonic and extrusive igneous rocks are in abundance.
It furthers the University's objective of excellence drebik research, scholarship, and education by publishing worldwide.
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