Anisotropy of magnetic susceptibility as an indicator for palaeocurrent analysis in folded turbidites (Outer Western Carpathians, Poland)-Reference-Cited by-同舟云学术

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Anisotropy of magnetic susceptibility as an indicator for palaeocurrent analysis in folded turbidites (Outer Western Carpathians, Poland)

Published:2020-07-19 Issue:7 Volume:67 Page:3783-3808
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Stachowska Aleksandra¹^ORCID,Łoziński Maciej²^ORCID,Śmigielski Michał²,Wysocka Anna²^ORCID,Jankowski Leszek³^ORCID,Ziółkowski Piotr²

Affiliation:

1. Institute of Geological Sciences Polish Academy of Sciences 51/55 Twarda Street 00‐818 Warsaw Poland

2. Faculty of Geology University of Warsaw 93 Żwirki & Wigury Street 02‐089 Warsaw Poland

3. Polish Geological Institute – National Research Institute Carpathian Branch 1 Skrzatów Street 31‐560 Cracow Poland

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12770

Reference113 articles.

1. Burial and exhumation history of the Polish Outer Carpathians: Discriminating the role of thrusting and post-thrusting extension

2. Post-Miocene shortening pictured by magnetic fabric across the Zagros-Makran syntaxis (Iran)

3. EZ-ROSE: a computer program for equal-area circular histograms and statistical analysis of two-dimensional vectorial data

4. Directional petrological characterisation of deep-marine sandstones using grain fabric and permeability anisotropy: Methodologies, theory, application and suggestions for integration

5. A magnetic fabric study of Late Whitcliffian (U. Silurian) siltstones from the Welsh Borderland

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