Crustal Thinning From Orogen to Back‐Arc Basin: The Structure of the Pannonian Basin Region Revealed by P ‐to‐ S Converted Seismic Waves-Reference-Cited by-同舟云学术

Crustal Thinning From Orogen to Back‐Arc Basin: The Structure of the Pannonian Basin Region Revealed by P ‐to‐ S Converted Seismic Waves

Author:

Kalmár Dániel¹²^ORCID,Hetényi György³²^ORCID,Balázs Attila⁴^ORCID,Bondár István⁵^ORCID,

Affiliation:

1. Department of Geophysics and Space Science Eötvös Loránd University Budapest Hungary

2. Kövesligethy Radó Seismological Observatory Institute of Earth Physics and Space Science Sopron Hungary

3. University of Lausanne Institute of Earth Sciences Lausanne Switzerland

4. Department of Earth Sciences ETH Zürich Zürich Switzerland

5. Institute for Geological and Geochemical Research Research Center for Astronomy and Earth Sciences Budapest Hungary

Funder

National Research, Development and Innovation Office

Swiss National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

Reference81 articles.

Cited by 20 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献