New geophysical and geological data on the Moldanubian plutonic complex and the Kaplice Fault, southern Bohemia
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F22%3A00557454" target="_blank" >RIV/67985831:_____/22:00557454 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/61989100:27350/22:10250491
Výsledek na webu
<a href="https://link.springer.com/article/10.1007/s00531-022-02182-5" target="_blank" >https://link.springer.com/article/10.1007/s00531-022-02182-5</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00531-022-02182-5" target="_blank" >10.1007/s00531-022-02182-5</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
New geophysical and geological data on the Moldanubian plutonic complex and the Kaplice Fault, southern Bohemia
Popis výsledku v původním jazyce
The paper presents a new structural model of the granitoid intrusions of the Moldanubian plutonic complex in southern Bohemiaeast of the town of Kaplice. Valuable archival gravity data were supplemented by magnetic survey and precise profile gravity measurements to better define the gravitational effect of the granitoid body and provide an accurate model solution. Our findings, based on geophysical analyses and modelling, bring new information on the shape and deep structure of the Moldanubian plutonic complex in southern Bohemia. These results are complemented by a tectonic investigation of the Freistadt granodiorite body and the Kaplice Fault. New information on the geometry of the Kaplice Fault plane acquired from Linsser indications is discussed in relation to its possible recent seismic activity. The usefulness of the Linsser indications method for active tectonic studies is demonstrated. This is the first regional study in this insufficiently known part of the Bohemian Massif, providing new information on the extent of granites and their relationship to one of the most significant faults in this area.
Název v anglickém jazyce
New geophysical and geological data on the Moldanubian plutonic complex and the Kaplice Fault, southern Bohemia
Popis výsledku anglicky
The paper presents a new structural model of the granitoid intrusions of the Moldanubian plutonic complex in southern Bohemiaeast of the town of Kaplice. Valuable archival gravity data were supplemented by magnetic survey and precise profile gravity measurements to better define the gravitational effect of the granitoid body and provide an accurate model solution. Our findings, based on geophysical analyses and modelling, bring new information on the shape and deep structure of the Moldanubian plutonic complex in southern Bohemia. These results are complemented by a tectonic investigation of the Freistadt granodiorite body and the Kaplice Fault. New information on the geometry of the Kaplice Fault plane acquired from Linsser indications is discussed in relation to its possible recent seismic activity. The usefulness of the Linsser indications method for active tectonic studies is demonstrated. This is the first regional study in this insufficiently known part of the Bohemian Massif, providing new information on the extent of granites and their relationship to one of the most significant faults in this area.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
<a href="/cs/project/GJ19-02177Y" target="_blank" >GJ19-02177Y: Procesy transferu a vmístění magmatu v kolabujících orogenech</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2022
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
International Journal of Earth Sciences
ISSN
1437-3254
e-ISSN
1437-3262
Svazek periodika
111
Číslo periodika v rámci svazku
4
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
17
Strana od-do
1315-1331
Kód UT WoS článku
000773838800002
EID výsledku v databázi Scopus
2-s2.0-85127253308