Uplift of the Transdanubian Range, Pannonian Basin: How fast and why?-Reference-Cited by-同舟云学术

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Uplift of the Transdanubian Range, Pannonian Basin: How fast and why?

Published:2020-09 Issue: Volume:192 Page:103263
ISSN:0921-8181
Container-title:Global and Planetary Change
language:en
Short-container-title:Global and Planetary Change

Author:

Ruszkiczay-Rüdiger Zs,Balázs A.,Csillag G.,Drijkoningen G.,Fodor L.

Funder

National Research, Development and Innovation Office of Hungary

NKFIH-OTKA

Hungarian Academy of Sciences

ETH Zürich

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference123 articles.

1. Pleistocene fluvial terraces from northern France (Seine, Yonne, Somme): synthesis, and new results from interglacial deposits;Antoine;Quat. Sci. Rev.,2007

2. Tertiary brittle faulting and stress field evolution in the Gerecse Mountains, northern Hungary;Bada;Tectonophys,1996

3. Present-day stress field and tectonic inversion in the Pannonian basin;Bada;Glob. Planet. Chang.,2007

4. Symmetry during the syn- and post-rift evolution of extensional back-arc basins: the role of inherited orogenic structures;Balázs;Earth Planet. Sci. Lett.,2017

5. Morphology of a large paleo-lake: Analysis of compaction in the Miocene–Quaternary Pannonian Basin;Balázs;Glob. Planet. Chang.,2018

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