Origin of block accumulations based on the near-surface geophysics

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F23%3A00572178" target="_blank" >RIV/67985891:_____/23:00572178 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216208:11310/23:10475520 RIV/49777513:23420/23:43968406

Výsledek na webu

<a href="https://doi.org/10.1515/geo-2022-0468" target="_blank" >https://doi.org/10.1515/geo-2022-0468</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1515/geo-2022-0468" target="_blank" >10.1515/geo-2022-0468</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Origin of block accumulations based on the near-surface geophysics

Popis výsledku v původním jazyce

Understanding the internal structure of specific landforms is a crucial prerequisite for determining their origin and evolution. Near-surface geophysics represents a non-invasive way of subsurface investigation, and it can be used to describe subsurface conditions, especially in protected areas. We tested possible hypotheses of block accumulations origin and evolution by four different geophysical methods (electrical resistivity tomography [ERT], shallow seismic refraction [SSR], ground penetrating radar [GPR], and electromagnetic induction [EMI]) in the Central European Uplands. At the same time, we evaluated the applicability of geophysical methods to determine the internal structure and thickness of block accumulations. Based on the application of two suitable methods (ERT and SSR), we (1) estimated the thicknesses of block accumulations, (2) partially described their internal structure, and (3) presented the most probable hypotheses of block accumulation origin and evolution in two investigated sites.

Název v anglickém jazyce

Origin of block accumulations based on the near-surface geophysics

Popis výsledku anglicky

Understanding the internal structure of specific landforms is a crucial prerequisite for determining their origin and evolution. Near-surface geophysics represents a non-invasive way of subsurface investigation, and it can be used to describe subsurface conditions, especially in protected areas. We tested possible hypotheses of block accumulations origin and evolution by four different geophysical methods (electrical resistivity tomography [ERT], shallow seismic refraction [SSR], ground penetrating radar [GPR], and electromagnetic induction [EMI]) in the Central European Uplands. At the same time, we evaluated the applicability of geophysical methods to determine the internal structure and thickness of block accumulations. Based on the application of two suitable methods (ERT and SSR), we (1) estimated the thicknesses of block accumulations, (2) partially described their internal structure, and (3) presented the most probable hypotheses of block accumulation origin and evolution in two investigated sites.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10508 - Physical geography

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2023

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Open Geosciences

ISSN

2391-5447

e-ISSN

2391-5447

Svazek periodika

15

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

PL - Polská republika

Počet stran výsledku

18

Strana od-do

20220468

Kód UT WoS článku

000965105500001

EID výsledku v databázi Scopus

2-s2.0-85152474145