Tisza Plate

Tectonic microplate, in present-day Europe
Pelso and Tisza units

The Tisza Plate is a tectonic block, or microplate, in present-day Europe. The two major crustal blocks of the Pannonian Basin, Pelso and Tisza, underwent a complex process of rotation and extension of variable magnitude during the Cenozoic era. The northward push of the Adriatic Block initiated the eastward displacement and rotation of both the Alcapa (or Pelso) and Tisza blocks.[1][2][3] The Zágráb-Hernád line is the former plate margin between the Pelso of African origin and the Tisza Plate of Eurasian origin.

References

  1. ^ Tom McCann (2008). The Geology of Central Europe. Geological Society of London. p. 805. ISBN 978-1-86239-265-6.
  2. ^ Petrology of the metamorphic basement of the Tisza Block at the Jánoshalma High, S Hungary, Acta Geologica Hungarica, p. 349-371, ISSN 0236-5278 (Print) ISSN 1588-2594 (Online)
  3. ^ Luigi Beccaluva; Gianluca Bianchini; B. Marjorie Wilson; Marjorie Wilson (2007). Cenozoic Volcanism in the Mediterranean Area. Geological Society of America. p. 68. ISBN 978-0-8137-2418-8.
  • v
  • t
  • e
Tectonic plates
Major plates
  • African
  • Antarctic
  • Eurasian
  • Indo-Australian
    • Australian
    • Indian
  • North American
  • Pacific
  • South American
World map indicating tectonic plate boundaries
Minor platesMicroplatesAncient platesOceanic ridgesAncient oceanic ridges
  • icon Geology portal
  • List
  • Category
  • Commons
  • v
  • t
  • e
Countries
Geologic regions
Orogens
Mountain ranges
Oceanic basins
Intracontinental
basins and grabens
Tectonic plates and
microcontinents
Terranes
UNESCO World Heritage Sites


Stub icon

This tectonics article is a stub. You can help Wikipedia by expanding it.

  • v
  • t
  • e
Stub icon

This Hungarian geography article is a stub. You can help Wikipedia by expanding it.

  • v
  • t
  • e